{"pageNumber":"3344","pageRowStart":"83575","pageSize":"25","recordCount":184904,"records":[{"id":70128321,"text":"70128321 - 1999 - 210Pb and 210Po, manganese and iron cycling across the O2/H2S interface of a permanently anoxic fjord: Framvaren, Norway","interactions":[],"lastModifiedDate":"2021-05-10T20:04:21.163789","indexId":"70128321","displayToPublicDate":"1999-10-07T13:24:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2662,"text":"Marine Chemistry","active":true,"publicationSubtype":{"id":10}},"displayTitle":"210Pb and 210Po, manganese and iron cycling across the O2/H2S interface of a permanently anoxic fjord: Framvaren, Norway","title":"210Pb and 210Po, manganese and iron cycling across the O2/H2S interface of a permanently anoxic fjord: Framvaren, Norway","docAbstract":"Vertical profiles of dissolved and particulate 201Po and 210Pb were measured across the redox transition zone at Station F1 in Framvaren Fjord, Norway. In this fjord, a sharp decrease in pH above the O2/H2S interface facilitates the aerobic dissolution of MnO2. In contrast, Fe(II) concentrations begin to increase only at the O2/H2S interface depth. Activity profiles reveal that dissolved 210Po and 210Pb are sequestered efficiently by particulates in surface waters. As polonium-210 and lead-210 activities descend down into the aerobic manganese reduction (AMR) zone, they are remobilized during the reductive dissolution of the carrier phase oxyhydroxides. Both 210Po and 210Pb are highly enriched at the O2/H2S interface where an active community of microbes, such as anoxygenic phototrophs (e.g., Chromatium, Chlorobium sp.), thrives. The coincident peaks in 210Po and 210Pb and microbial biomass suggest a strong biological influence on the behavior of these radionuclides. There is a strong covariance between the vertical distribution of Mn and Pb, indicating that their redox cycling is closely coupled and is likely microbially mediated.","language":"English","publisher":"Elsevier","doi":"10.1016/S0304-4203(99)00059-6","usgsCitation":"Swarzenski, P.W., McKee, B.A., Sorenson, K., and Todd, J.F., 1999, 210Pb and 210Po, manganese and iron cycling across the O2/H2S interface of a permanently anoxic fjord: Framvaren, Norway: Marine Chemistry, v. 67, no. 3-4, p. 199-217, https://doi.org/10.1016/S0304-4203(99)00059-6.","productDescription":"19 p.","startPage":"199","endPage":"217","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":295028,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Norway","otherGeospatial":"Framveran Fjord","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 6.727924346923828,\n 58.116976151635924\n ],\n [\n 6.766204833984375,\n 58.116976151635924\n ],\n [\n 6.766204833984375,\n 58.19486646023086\n ],\n [\n 6.727924346923828,\n 58.19486646023086\n ],\n [\n 6.727924346923828,\n 58.116976151635924\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"67","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54350098e4b0a4f4b46a2368","contributors":{"authors":[{"text":"Swarzenski, Peter W. 0000-0003-0116-0578 pswarzen@usgs.gov","orcid":"https://orcid.org/0000-0003-0116-0578","contributorId":1070,"corporation":false,"usgs":true,"family":"Swarzenski","given":"Peter","email":"pswarzen@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":502868,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKee, Brent A.","contributorId":70711,"corporation":false,"usgs":true,"family":"McKee","given":"Brent","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":502870,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sorenson, Kai","contributorId":11973,"corporation":false,"usgs":true,"family":"Sorenson","given":"Kai","email":"","affiliations":[],"preferred":false,"id":502869,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Todd, James F.","contributorId":84291,"corporation":false,"usgs":true,"family":"Todd","given":"James","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":502871,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70128313,"text":"70128313 - 1999 - 7Be as a tracer of flood sedimentation on the northern California continental margin","interactions":[],"lastModifiedDate":"2017-12-14T16:42:31","indexId":"70128313","displayToPublicDate":"1999-10-07T13:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1333,"text":"Continental Shelf Research","active":true,"publicationSubtype":{"id":10}},"displayTitle":"7Be as a tracer of flood sedimentation on the northern California continental margin","title":"7Be as a tracer of flood sedimentation on the northern California continental margin","docAbstract":"Sediment inventories of the cosmogenic radionuclide 7Be (t1/2=53 d) were measured on the Eel River shelf and slope (northern California continental margin) to investigate sedimentation processes associated with coastal river flooding. Seabed coring shortly after major riverflow events in 1995 and 1997 documented a shelf-wide flood deposit, and subsequent radionuclide studies determined 7Be to be a powerful tracer of fine-grained river sediment. In addition, distinctive signatures of 234Th and 210Pb were observed in oceanic flood deposits and provided additional information regarding depositional processes. During the 1995–1997 monitoring period, 7Be was present (2–35 dpm cm-2) in shelf and slope sediments only after periods of high rainfall and river runoff during the winter months. It is suggested that fluvial input was the primary source of 7Be in shelf sediments after the floods. 7Be sediment inventories and sediment-trap fluxes determined after the 1997 flood revealed that fine-grained fluvial sediments were rapidly (within one month) broadcast over the continental margin, to the 500 m isobath. Dispersal was apparently facilitated by energetic storm waves, which resuspended and redistributed some fraction of the suspended load residing on the shelf prior to accretion as flood deposits. These observations illustrate that floods are an important sedimentary process for modern environments of the Eel shelf and slope, and perhaps for other fluviomarine sedimentary systems of the northern California continental margin. Ratios of the 210Pb sediment-accumulation rate (100 yr average) to the 7Be deposition rate (1–2 month average) for shelf sites illustrate the episodic nature of shelf sedimentation, and suggest that a minimum of 3–30 depositional events complete the most recent stratigraphic record. This observation is consistent with the magnetude and frequency of fluvial sediment input, as Eel River floods with return periods of 3–33 yr (3% of the time of record) have supplied >80% of the total 85 yr suspended load. Based on radionuclide and hydrologic data, it can be concluded that a small number of flood depositional events have had a disproportionate impact on the sedimentary record of the Eel shelf.","language":"English","publisher":"Elsevier","doi":"10.1016/S0278-4343(98)00090-9","usgsCitation":"Sommerfield, C.K., Nittrouer, C.A., and Alexander, C.R., 1999, 7Be as a tracer of flood sedimentation on the northern California continental margin: Continental Shelf Research, v. 19, no. 3, p. 335-361, https://doi.org/10.1016/S0278-4343(98)00090-9.","productDescription":"27 p.","startPage":"335","endPage":"361","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":295019,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295018,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0278-4343(98)00090-9"}],"country":"United States","state":"California","otherGeospatial":"Eel River","volume":"19","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54350098e4b0a4f4b46a236a","contributors":{"authors":[{"text":"Sommerfield, C. K.","contributorId":87472,"corporation":false,"usgs":true,"family":"Sommerfield","given":"C.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":502862,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nittrouer, C. A.","contributorId":73521,"corporation":false,"usgs":true,"family":"Nittrouer","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":502861,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alexander, C. R.","contributorId":72729,"corporation":false,"usgs":true,"family":"Alexander","given":"C.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":502860,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70128302,"text":"70128302 - 1999 - Airborne laser study quantifies El Niño-induced coastal change","interactions":[],"lastModifiedDate":"2014-10-07T12:02:01","indexId":"70128302","displayToPublicDate":"1999-10-07T11:58:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Airborne laser study quantifies El Niño-induced coastal change","docAbstract":"Winter storms during the 1997–1998 El Niño caused extensive changes to the beaches and cliffs of the west coast of the United States, a NASA-NOAA-USGS investigation using a scanning airborne laser has found. For example, near Pacifica in central California, the cliff eroded locally as much as 10–13 m landward during the El Niño winter, at least 40 times the long term average erosion rate. However, only several hundred meters away the cliff was stable. This variability in cliff response may be related to differences in local beach changes where an accreting beach protected part of the cliff and an eroding beach exposed another part to attack by waves.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Eos, Transactions American Geophysical Union","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Geophysical Union","doi":"10.1029/99EO00056","usgsCitation":"Sallenger, A.H., Krabill, W., Brock, J., Swift, R., Jansen, M., Manizade, S., Richmond, B., Hampton, M., and Eslinger, D., 1999, Airborne laser study quantifies El Niño-induced coastal change: Eos, Transactions, American Geophysical Union, v. 80, no. 8, p. 89-92, https://doi.org/10.1029/99EO00056.","productDescription":"4 p.","startPage":"89","endPage":"92","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":295004,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295003,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/99EO00056"}],"country":"United States","otherGeospatial":"Pacific Coast","volume":"80","issue":"8","noUsgsAuthors":false,"publicationDate":"2011-06-03","publicationStatus":"PW","scienceBaseUri":"5435009de4b0a4f4b46a2371","contributors":{"authors":[{"text":"Sallenger, Asbury H. Jr.","contributorId":30562,"corporation":false,"usgs":true,"family":"Sallenger","given":"Asbury","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":502847,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krabill, William","contributorId":33646,"corporation":false,"usgs":true,"family":"Krabill","given":"William","affiliations":[],"preferred":false,"id":502848,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brock, John H.","contributorId":14320,"corporation":false,"usgs":false,"family":"Brock","given":"John H.","affiliations":[],"preferred":false,"id":502846,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Swift, Robert","contributorId":67817,"corporation":false,"usgs":true,"family":"Swift","given":"Robert","affiliations":[],"preferred":false,"id":502851,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jansen, Mark","contributorId":52906,"corporation":false,"usgs":true,"family":"Jansen","given":"Mark","email":"","affiliations":[],"preferred":false,"id":502849,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Manizade, Serdar","contributorId":93412,"corporation":false,"usgs":true,"family":"Manizade","given":"Serdar","email":"","affiliations":[],"preferred":false,"id":502852,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Richmond, Bruce","contributorId":6778,"corporation":false,"usgs":true,"family":"Richmond","given":"Bruce","affiliations":[],"preferred":false,"id":502845,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Hampton, Monty","contributorId":102011,"corporation":false,"usgs":true,"family":"Hampton","given":"Monty","affiliations":[],"preferred":false,"id":502853,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Eslinger, David","contributorId":65020,"corporation":false,"usgs":true,"family":"Eslinger","given":"David","email":"","affiliations":[],"preferred":false,"id":502850,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":70128300,"text":"70128300 - 1999 - Scaling winter storm impacts on Assateague Island, Maryland, Virginia","interactions":[],"lastModifiedDate":"2017-12-15T15:06:57","indexId":"70128300","displayToPublicDate":"1999-10-07T11:42:00","publicationYear":"1999","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Scaling winter storm impacts on Assateague Island, Maryland, Virginia","docAbstract":"No abstract available.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Coastal sediments '99: proceedings of the 4th International Symposium on Coastal Engineering and Science of Coastal Sediment Processes: conference theme: scales of coastal sediment motion and geomorphic change, Hauppauge, Long Island, New York, June 21-23, 1999","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"American Society of Civil Engineers","usgsCitation":"Sallenger, A.H., Howd, P., Brock, J., Krabill, W.B., Swift, R.N., Manizade, S., and Duffy, M., 1999, Scaling winter storm impacts on Assateague Island, Maryland, Virginia, in Coastal sediments '99: proceedings of the 4th International Symposium on Coastal Engineering and Science of Coastal Sediment Processes: conference theme: scales of coastal sediment motion and geomorphic change, Hauppauge, Long Island, New York, June 21-23, 1999, p. 1814-1825.","productDescription":"12 p.","startPage":"1814","endPage":"1825","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":294999,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"543500b9e4b0a4f4b46a23cd","contributors":{"authors":[{"text":"Sallenger, Asbury H. Jr.","contributorId":30562,"corporation":false,"usgs":true,"family":"Sallenger","given":"Asbury","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":502840,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howd, Peter","contributorId":47310,"corporation":false,"usgs":true,"family":"Howd","given":"Peter","affiliations":[],"preferred":false,"id":502842,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brock, John H.","contributorId":14320,"corporation":false,"usgs":false,"family":"Brock","given":"John H.","affiliations":[],"preferred":false,"id":502838,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Krabill, W. B.","contributorId":102819,"corporation":false,"usgs":true,"family":"Krabill","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":502844,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Swift, R. N.","contributorId":69907,"corporation":false,"usgs":true,"family":"Swift","given":"R.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":502843,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Manizade, S.","contributorId":17551,"corporation":false,"usgs":true,"family":"Manizade","given":"S.","email":"","affiliations":[],"preferred":false,"id":502839,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Duffy, M.","contributorId":44483,"corporation":false,"usgs":true,"family":"Duffy","given":"M.","email":"","affiliations":[],"preferred":false,"id":502841,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":70128083,"text":"70128083 - 1999 - Great earthquakes, abundant sand, and high wave energy in the Columbia Cell, USA","interactions":[],"lastModifiedDate":"2017-08-31T13:25:37","indexId":"70128083","displayToPublicDate":"1999-10-03T11:34:00","publicationYear":"1999","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Great earthquakes, abundant sand, and high wave energy in the Columbia Cell, USA","docAbstract":"No abstract available.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Coastal sediments '99: proceedings of the 4th International Symposium on Coastal Engineering and Science of Coastal Sediment Processes: conference theme: scales of coastal sediment motion and geomorphic change, Hauppauge, Long Island, New York, June 21-23, 1999","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"American Society of Civil Engineers","usgsCitation":"Peterson, C.D., Gelfenbaum, G.R., Jol, H.M., Phipps, J.B., Reckendorf, F., Twichell, D.C., Vanderberg, S., and Woxell, L., 1999, Great earthquakes, abundant sand, and high wave energy in the Columbia Cell, USA, in Coastal sediments '99: proceedings of the 4th International Symposium on Coastal Engineering and Science of Coastal Sediment Processes: conference theme: scales of coastal sediment motion and geomorphic change, Hauppauge, Long Island, New York, June 21-23, 1999, v. 2.","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":294908,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"542fba9fe4b092f17df61d11","contributors":{"authors":[{"text":"Peterson, Curt D.","contributorId":83039,"corporation":false,"usgs":true,"family":"Peterson","given":"Curt","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":502767,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gelfenbaum, Guy R. 0000-0003-1291-6107 ggelfenbaum@usgs.gov","orcid":"https://orcid.org/0000-0003-1291-6107","contributorId":742,"corporation":false,"usgs":true,"family":"Gelfenbaum","given":"Guy","email":"ggelfenbaum@usgs.gov","middleInitial":"R.","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":502761,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jol, Harry M.","contributorId":78259,"corporation":false,"usgs":true,"family":"Jol","given":"Harry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":502766,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Phipps, Jim B.","contributorId":53713,"corporation":false,"usgs":true,"family":"Phipps","given":"Jim","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":502764,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Reckendorf, Frank","contributorId":74692,"corporation":false,"usgs":true,"family":"Reckendorf","given":"Frank","email":"","affiliations":[],"preferred":false,"id":502765,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Twichell, Dave C.","contributorId":48495,"corporation":false,"usgs":true,"family":"Twichell","given":"Dave","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":502763,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Vanderberg, Sandy","contributorId":100767,"corporation":false,"usgs":true,"family":"Vanderberg","given":"Sandy","email":"","affiliations":[],"preferred":false,"id":502768,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Woxell, Lorraine","contributorId":10348,"corporation":false,"usgs":true,"family":"Woxell","given":"Lorraine","email":"","affiliations":[],"preferred":false,"id":502762,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":70128068,"text":"70128068 - 1999 - Climatic-eustatic control of Holocene nearshore parasequence development, southeastern Texas coast","interactions":[],"lastModifiedDate":"2014-10-03T10:27:16","indexId":"70128068","displayToPublicDate":"1999-10-03T10:22:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1871,"text":"Gulf Coast Association of Geological Societies Transactions","active":true,"publicationSubtype":{"id":10}},"title":"Climatic-eustatic control of Holocene nearshore parasequence development, southeastern Texas coast","docAbstract":"

Sediment cores, seismic profiles, radiocarbon dates, and faunal assemblages were used to interpret the depositional setting and geological evolution of the southeastern Texas coast during the last glacio-eustatic cycle. Discrete lithofacies and biofacies zones in the ebb-dominated Sabine Lake estuary and adjacent chenier plain record alternating periods of rapid marine flooding and gradual shoaling related to linked climatic/eustatic fluctuations. Monospecific zones of the mollusks Rangia cuneata and Crassostrea virginica, respectively, indicate high fresh water outflow followed by invasion of marine water, whereas intervening organic-rich zones record bayhead delta deposition.

\n
\n

High-frequency parasequence stacking patterns within the valley fill and across the adjacent interfluve reflect an initial rapid rise in sea level about 9 ka that flooded abandoned alluvial terraces and caused onlap of Holocene marsh in the incised valley. The rapid rise was followed by slowly rising and oscillating sea level that filled the deepest portions of the incised valleys with fluvially dominated estuarine deposits, and then a maximum highstand (+1 m msl) about 5 ka that flooded the former subaerial coastal plain between the incised valleys and constructed the highest beach ridges. Between 3.5 and 1.5 ka, sea level oscillated and gradually fell, causing a forced regression and rapid progradation of both the chenier plain and accretionary barrier islands. The only significant sands in the valley fill are (1) falling-stage and lowstand-fluvial sediments between the basal sequence boundary and transgressive surface unconformity, and (2) highstand beach-ridge sediments of the chenier plain.

","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Gulf Coast Association of Geological Societies Transactions","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Gulf Coast Association of Geological Societies","usgsCitation":"Morton, R.A., Kindinger, J.L., Flocks, J.G., and Stewart, L.B., 1999, Climatic-eustatic control of Holocene nearshore parasequence development, southeastern Texas coast: Gulf Coast Association of Geological Societies Transactions, v. 49, p. 384-395.","productDescription":"12 p.","startPage":"384","endPage":"395","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":294901,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":294900,"type":{"id":15,"text":"Index Page"},"url":"https://archives.datapages.com/data/gcags/data/049/049001/0384.HTM"}],"country":"United States","state":"Texas","volume":"49","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"542fba9ae4b092f17df61cf1","contributors":{"authors":[{"text":"Morton, Robert A.","contributorId":28184,"corporation":false,"usgs":true,"family":"Morton","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":502740,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kindinger, Jack L. jkindinger@usgs.gov","contributorId":815,"corporation":false,"usgs":true,"family":"Kindinger","given":"Jack","email":"jkindinger@usgs.gov","middleInitial":"L.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":502738,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Flocks, James G. 0000-0002-6177-7433 jflocks@usgs.gov","orcid":"https://orcid.org/0000-0002-6177-7433","contributorId":816,"corporation":false,"usgs":true,"family":"Flocks","given":"James","email":"jflocks@usgs.gov","middleInitial":"G.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":502739,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stewart, Laura B.","contributorId":38913,"corporation":false,"usgs":true,"family":"Stewart","given":"Laura","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":502741,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70169448,"text":"70169448 - 1999 - Effects of sample size and sampling frequency on studies of brown bear home ranges and habitat use","interactions":[],"lastModifiedDate":"2016-03-25T16:16:31","indexId":"70169448","displayToPublicDate":"1999-10-01T17:15:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3671,"text":"Ursus","active":true,"publicationSubtype":{"id":10}},"title":"Effects of sample size and sampling frequency on studies of brown bear home ranges and habitat use","docAbstract":"

We equipped 9 brown bears (Ursus arctos) on the Kenai Peninsula, Alaska, with collars containing both conventional very-high-frequency (VHF) transmitters and global positioning system (GPS) receivers programmed to determine an animal's position at 5.75-hr intervals. We calculated minimum convex polygon (MCP) and fixed and adaptive kernel home ranges for randomly-selected subsets of the GPS data to examine the effects of sample size on accuracy and precision of home range estimates. We also compared results obtained by weekly aerial radiotracking versus more frequent GPS locations to test for biases in conventional radiotracking data. Home ranges based on the MCP were 20-606 km2 (x = 201) for aerial radiotracking data (n = 12-16 locations/bear) and 116-1,505 km2 (x = 522) for the complete GPS data sets (n = 245-466 locations/bear). Fixed kernel home ranges were 34-955 km2 (x = 224) for radiotracking data and 16-130 km2 (x = 60) for the GPS data. Differences between means for radiotracking and GPS data were due primarily to the larger samples provided by the GPS data. Means did not differ between radiotracking data and equivalent-sized subsets of GPS data (P > 0.10). For the MCP, home range area increased and variability decreased asymptotically with number of locations. For the kernel models, both area and variability decreased with increasing sample size. Simulations suggested that the MCP and kernel models required >60 and >80 locations, respectively, for estimates to be both accurate (change in area <1%/additional location) and precise (CV < 50%). Although the radiotracking data appeared unbiased, except for the relationship between area and sample size, these data failed to indicate some areas that likely were important to bears. Our results suggest that the usefulness of conventional radiotracking data may be limited by potential biases and variability due to small samples. Investigators that use home range estimates in statistical tests should consider the effects of variability of those estimates. Use of GPS-equipped collars can facilitate obtaining larger samples of unbiased data and improve accuracy and precision of home range estimates.

","language":"English","publisher":"International Association for Bear Research and Management","publisherLocation":"New York, NY","usgsCitation":"Arthur, S.M., and Schwartz, C.C., 1999, Effects of sample size and sampling frequency on studies of brown bear home ranges and habitat use: Ursus, v. 11, p. 139-148.","productDescription":"10 p.","startPage":"139","endPage":"148","numberOfPages":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":319432,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":319431,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.bearbiology.com/fileadmin/tpl/Downloads/URSUS/Vol_11/Arthur_Schwartz_Vol_11.pdf","linkFileType":{"id":1,"text":"pdf"}}],"volume":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f66155e4b07d796bf77045","contributors":{"authors":[{"text":"Arthur, Steve M.","contributorId":66169,"corporation":false,"usgs":true,"family":"Arthur","given":"Steve","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":624154,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schwartz, Charles C.","contributorId":124574,"corporation":false,"usgs":false,"family":"Schwartz","given":"Charles","email":"","middleInitial":"C.","affiliations":[{"id":5119,"text":"Retired from U.S. Geological Survey, Interagency Grizzly Bear Study Team, Northern Rocky Mountain Science Center, 2327 University Way, suite 2, Bozeman, MT 59715","active":true,"usgs":false}],"preferred":false,"id":624155,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70168699,"text":"70168699 - 1999 - Groundwater geochemistry in the Seminole Well Field, Cedar Rapids, Iowa","interactions":[],"lastModifiedDate":"2019-12-14T06:19:34","indexId":"70168699","displayToPublicDate":"1999-10-01T16:45:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2529,"text":"Journal of the American Water Resources Association","active":true,"publicationSubtype":{"id":10}},"title":"Groundwater geochemistry in the Seminole Well Field, Cedar Rapids, Iowa","docAbstract":"

The City of Cedar Rapids obtains its municipal water supply from four well fields in an alluvial aquifer along the Cedar River in east-central Iowa. Since 1992, the City and the U.S. Geological Survey have cooperatively studied the groundwater-flow system and water chemistry near the well fields. The geochemistry in the alluvial aquifer near the Seminole Well Field was assessed to identify potentially reactive minerals and possible chemical reactions that produce observed changes in water chemistry. Calcite, dolomite, ferrihydrite, quartz, rhodochrosite, and siderite were identified as potentially reactive minerals by calculating saturation indexes. Aluminosiicate minerals including albite, Ca-montmorillonite, gibbsite, illite, K-feldspar, and kaolinite were identified as potentially reactive minerals using hypothetical saturation indexes calculated with an assumed dissolved aluminum concentration of 1 microgram per liter. Balanced chemical equations derived from inverse-modeling techniques were used to assess chemical reactions as precipitation percolates to the water table. Calcite dissolution was predominate, but aluminosilicate weathering, cation exchange, and redox reactions also likely occurred. Microbial-catalyzed redox reactions altered the chemical composition of water infiltrating from the Cedar River into the alluvial aquifer by consuming dissolved oxygen, reducing nitrate, and increasing dissolved iron and manganese concentrations. Nitrate reduction only occurred in relatively shallow (3 to 7 meters below land surface) groundwater near the Cedar River and did not occur in water infiltrating to deeper zones of the alluvial aquifer.

","language":"English","publisher":"American Water Resources Association","doi":"10.1111/j.1752-1688.1999.tb04212.x","usgsCitation":"Boyd, R., 1999, Groundwater geochemistry in the Seminole Well Field, Cedar Rapids, Iowa: Journal of the American Water Resources Association, v. 35, no. 5, p. 1257-1268, https://doi.org/10.1111/j.1752-1688.1999.tb04212.x.","productDescription":"12 p.","startPage":"1257","endPage":"1268","numberOfPages":"12","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":318371,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Iowa","city":"Cedar Rapids","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.8017578125,\n 41.90432124806034\n ],\n [\n -91.55731201171875,\n 41.90432124806034\n ],\n [\n -91.55731201171875,\n 42.049292638686836\n ],\n [\n -91.8017578125,\n 42.049292638686836\n ],\n [\n -91.8017578125,\n 41.90432124806034\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"35","issue":"5","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"56cee265e4b015c306ec5ed4","contributors":{"authors":[{"text":"Boyd, Robert A.","contributorId":16491,"corporation":false,"usgs":true,"family":"Boyd","given":"Robert A.","affiliations":[],"preferred":false,"id":621324,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70073360,"text":"70073360 - 1999 - Manganese and associated ore deposits of China","interactions":[],"lastModifiedDate":"2014-01-16T13:22:41","indexId":"70073360","displayToPublicDate":"1999-10-01T13:16:27","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2954,"text":"Ore Geology Reviews","active":true,"publicationSubtype":{"id":10}},"title":"Manganese and associated ore deposits of China","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ore Geology Reviews","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam","usgsCitation":"Hein, J.R., and Fan, D., 1999, Manganese and associated ore deposits of China: Ore Geology Reviews, v. 15, no. 1-3, p. 1-176.","productDescription":"176 p.","startPage":"1","endPage":"176","numberOfPages":"176","costCenters":[],"links":[{"id":281187,"type":{"id":15,"text":"Index Page"},"url":"https://www.sciencedirect.com/science/journal/01691368/15/1"},{"id":281188,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"China","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 73.5,15.1 ], [ 73.5,53.56 ], [ 134.78,53.56 ], [ 134.78,15.1 ], [ 73.5,15.1 ] ] ] } } ] }","volume":"15","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd657ae4b0b290851001d6","contributors":{"editors":[{"text":"Hein, James R. 0000-0002-5321-899X jhein@usgs.gov","orcid":"https://orcid.org/0000-0002-5321-899X","contributorId":2828,"corporation":false,"usgs":true,"family":"Hein","given":"James","email":"jhein@usgs.gov","middleInitial":"R.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":509707,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Fan, Delian","contributorId":88515,"corporation":false,"usgs":true,"family":"Fan","given":"Delian","email":"","affiliations":[],"preferred":false,"id":509708,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Hein, James R. 0000-0002-5321-899X jhein@usgs.gov","orcid":"https://orcid.org/0000-0002-5321-899X","contributorId":2828,"corporation":false,"usgs":true,"family":"Hein","given":"James","email":"jhein@usgs.gov","middleInitial":"R.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":488634,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fan, Delian","contributorId":88515,"corporation":false,"usgs":true,"family":"Fan","given":"Delian","email":"","affiliations":[],"preferred":false,"id":488635,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70170276,"text":"70170276 - 1999 - Ground-water quality along a flowpath in a surficial outwash aquifer in the Upper Mississippi River Basin: The influence of land use","interactions":[],"lastModifiedDate":"2016-04-15T11:45:33","indexId":"70170276","displayToPublicDate":"1999-10-01T12:45:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1925,"text":"Hydrological Science and Technology","active":true,"publicationSubtype":{"id":10}},"title":"Ground-water quality along a flowpath in a surficial outwash aquifer in the Upper Mississippi River Basin: The influence of land use","docAbstract":"

No abstract available.

","language":"English","usgsCitation":"Andrews, W., Stark, J., Fong, A.L., and Hanson, P.E., 1999, Ground-water quality along a flowpath in a surficial outwash aquifer in the Upper Mississippi River Basin: The influence of land use: Hydrological Science and Technology, v. 15, no. 1-4, p. 66-75.","productDescription":"10 p.","startPage":"66","endPage":"75","numberOfPages":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":320068,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Upper Mississippi River basin","volume":"15","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"571210b1e4b0ef3b7ca643e9","contributors":{"authors":[{"text":"Andrews, W. J. 0000-0003-4780-8835","orcid":"https://orcid.org/0000-0003-4780-8835","contributorId":56261,"corporation":false,"usgs":true,"family":"Andrews","given":"W. J.","affiliations":[],"preferred":false,"id":626735,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stark, J. R.","contributorId":100406,"corporation":false,"usgs":true,"family":"Stark","given":"J. R.","affiliations":[],"preferred":false,"id":626736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fong, A. L.","contributorId":58309,"corporation":false,"usgs":true,"family":"Fong","given":"A.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":626737,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hanson, P. E.","contributorId":58683,"corporation":false,"usgs":true,"family":"Hanson","given":"P.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":626738,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":47906,"text":"b2166 - 1999 - The controversial origin of central Utah's geologic complexities","interactions":[],"lastModifiedDate":"2012-02-02T00:10:03","indexId":"b2166","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2166","title":"The controversial origin of central Utah's geologic complexities","language":"ENGLISH","doi":"10.3133/b2166","issn":"8755-531X","usgsCitation":"Witkind, I.J., 1999, The controversial origin of central Utah's geologic complexities (Version 1.0): U.S. Geological Survey Bulletin 2166, p. 16, illus. incl. sects., 1 table, geol. sketch map, 6 refs, https://doi.org/10.3133/b2166.","productDescription":"p. 16, illus. incl. sects., 1 table, geol. sketch map, 6 refs","costCenters":[],"links":[{"id":4064,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/b2166/","linkFileType":{"id":5,"text":"html"}},{"id":162733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db66898e","contributors":{"authors":[{"text":"Witkind, Irving J.","contributorId":14469,"corporation":false,"usgs":true,"family":"Witkind","given":"Irving","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":236501,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":6948,"text":"fs09299 - 1999 - Quality of Ozark streams and ground water, 1992-95","interactions":[],"lastModifiedDate":"2012-02-02T00:05:48","indexId":"fs09299","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"092-99","title":"Quality of Ozark streams and ground water, 1992-95","docAbstract":"This fact sheet summarizes a previous USGS publication, 'Water Quality in the Ozark Plateaus, Arkansas, Kansas, Missouri, and Oklahoma, 1992' (Circular 1158). The fact sheet describes the effects of some of the major land uses and human activities upon water quality in the Ozarks. Nutrients, bacteria, pesticides, and other organic compounds generally are found in high concentrations or more frequently in agricultural or urban areas than in forested areas. Several metals are found in higher concentrations in water, bed sediment, or biological tissue downstream from mining areas. Nutrient concentrations generally do not make water unsafe for drinking. Bacteria concentrations may be high enough to cause concern in some areas at some times. Pesticides and other organic compounds generally are not of concern. Metal concentrations in some mining areas are of concern to humans and wildlife. Biological communities are being altered by habitat and water-quality changes.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs09299","usgsCitation":"Petersen, J., Adamski, J.C., Bell, R.W., Davis, J., Femmer, S.R., Freiwald, D.A., and Joseph, R.L., 1999, Quality of Ozark streams and ground water, 1992-95: U.S. Geological Survey Fact Sheet 092-99, 1 folded sheet ([4] p.) : col. ill., col. maps ; 28 x 43 cm. folded to 28 x 22 cm. col. ill., col. maps ;, https://doi.org/10.3133/fs09299.","productDescription":"1 folded sheet ([4] p.) : col. ill., col. maps ; 28 x 43 cm. folded to 28 x 22 cm. col. ill., col. maps ;","costCenters":[],"links":[{"id":736,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://ar.water.usgs.gov/LOCAL_REPORTS/FS-092-99.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1999/0092/report-thumb.jpg"},{"id":34226,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1999/0092/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db65520a","contributors":{"authors":[{"text":"Petersen, James C. petersen@usgs.gov","contributorId":2437,"corporation":false,"usgs":true,"family":"Petersen","given":"James C.","email":"petersen@usgs.gov","affiliations":[{"id":129,"text":"Arkansas Water Science Center","active":true,"usgs":true}],"preferred":false,"id":153634,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adamski, James C.","contributorId":20316,"corporation":false,"usgs":true,"family":"Adamski","given":"James","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":153638,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bell, Richard W.","contributorId":44141,"corporation":false,"usgs":true,"family":"Bell","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":153639,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Davis, Jerri V. jdavis@usgs.gov","contributorId":2667,"corporation":false,"usgs":true,"family":"Davis","given":"Jerri V.","email":"jdavis@usgs.gov","affiliations":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":false,"id":153635,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Femmer, Suzanne R. sfemmer@usgs.gov","contributorId":2668,"corporation":false,"usgs":true,"family":"Femmer","given":"Suzanne","email":"sfemmer@usgs.gov","middleInitial":"R.","affiliations":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":false,"id":153636,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Freiwald, David A. freiwald@usgs.gov","contributorId":226,"corporation":false,"usgs":true,"family":"Freiwald","given":"David","email":"freiwald@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":153633,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Joseph, Robert L. rljoseph@usgs.gov","contributorId":3482,"corporation":false,"usgs":true,"family":"Joseph","given":"Robert","email":"rljoseph@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":153637,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":4411,"text":"cir1190 - 1999 - Sustainable growth in America's heartland: 3-D geologic maps as the foundation","interactions":[],"lastModifiedDate":"2020-03-27T10:07:01","indexId":"cir1190","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1190","title":"Sustainable growth in America's heartland: 3-D geologic maps as the foundation","docAbstract":"

The Central Great Lakes States of Illinois, Indiana, Michigan, and Ohio constitute one of the most productive and economically important regions in the country—America’s heartland. The agriculture, industry, business, recreation, and ecology of these States are based on a common geologic heritage.

During the last 1.8 million years, glaciers repeatedly advanced and retreated across the region, leaving behind a thick, complex blanket of intermixed layers of mud, clay, silt, sand, and gravel. These glacial deposits contain bountiful resources—rich soils; plentiful ground water; minerals for construction; land for agriculture, development, recreation, and wildlife habitat; and lakes and rivers for recreation and wildlife habitat. These materials are also subject to natural hazards—floods, erosion, landslides, radon, and earthquakes—and manmade problems such as soil, sediment, and water contamination from point and nonpoint sources. Resulting land degradation has impaired and restricted human use and enjoyment of the land and caused degradation and loss of wildlife habitat.

The continued economic growth of the region and the security of its population and environment are related to fundamental issues involving land, water, mineral, and biological resources. Addressing the conflicting demands on these resources without adequate information can result in land-use decisions that are not compatible with sustainable development and a continued high quality of life for future generations. Decisionmakers need knowledge of the glacial deposits— their characteristics, three-dimensional (3-D) distribution, and thickness. To provide this knowledge, a coalition of State and Federal Geological Surveys (Illinois State Geological Survey, Indiana Geological Survey, Michigan Geological Survey Division, Ohio Division of Geological Survey, U.S. Geological Survey) has formed to conduct the necessary studies in these four States to depict the 3-D nature of these glacial and related deposits and to interpret these data in cooperation with the user community for specific societal needs.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir1190","usgsCitation":"Central Great Lakes Geologic Mapping Coalition, Illinois State Geological Survey, Indiana Geological Survey, Michigan Geological Survey Division, Ohio Division of Geological Survey, and Water Resources Division, U.S. Geological Survey, 1999, Sustainable growth in America's heartland: 3-D geologic maps as the foundation: U.S. Geological Survey Circular 1190, vi, 17 p., https://doi.org/10.3133/cir1190.","productDescription":"vi, 17 p.","costCenters":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":123402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/cir_1190.bmp"},{"id":63,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/circular/c1190","linkFileType":{"id":5,"text":"html"}},{"id":373581,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/c1190/c1190-72.pdf"}],"country":"United States","state":"Illinois, Indiana, Michigan, Ohio","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.5078125,\n 42.293564192170095\n ],\n [\n -81.8701171875,\n 41.934976500546604\n ],\n [\n -83.1005859375,\n 41.83682786072714\n ],\n [\n -82.96875,\n 42.391008609205045\n ],\n [\n -82.353515625,\n 43.45291889355465\n ],\n [\n -82.30957031249999,\n 45.02695045318546\n ],\n [\n -83.232421875,\n 45.49094569262732\n ],\n [\n -84.111328125,\n 46.31658418182218\n ],\n [\n -84.90234375,\n 46.98025235521883\n ],\n [\n -87.0556640625,\n 46.73986059969267\n ],\n [\n -87.9345703125,\n 47.07012182383309\n ],\n [\n -87.6708984375,\n 47.57652571374621\n ],\n [\n -87.978515625,\n 47.57652571374621\n ],\n [\n -89.69238281249999,\n 46.89023157359399\n ],\n [\n -90.2197265625,\n 46.49839225859763\n ],\n [\n -88.11035156249999,\n 45.9511496866914\n ],\n [\n -87.71484375,\n 45.182036837015886\n ],\n [\n -86.9677734375,\n 45.61403741135093\n ],\n [\n -85.78125,\n 45.1510532655634\n ],\n [\n -86.6162109375,\n 43.99281450048989\n ],\n [\n -86.220703125,\n 42.391008609205045\n ],\n [\n -87.451171875,\n 42.5530802889558\n ],\n [\n -90.439453125,\n 42.5530802889558\n ],\n [\n -90.04394531249999,\n 42.06560675405716\n ],\n [\n -91.01074218749999,\n 41.409775832009565\n ],\n [\n -91.62597656249999,\n 40.212440718286466\n ],\n [\n -90.7470703125,\n 39.06184913429154\n ],\n [\n -90.1318359375,\n 38.8225909761771\n ],\n [\n -90.17578124999999,\n 38.238180119798635\n ],\n [\n -89.20898437499999,\n 37.020098201368114\n ],\n [\n -88.06640625,\n 37.92686760148135\n ],\n [\n -86.044921875,\n 38.06539235133249\n ],\n [\n -84.90234375,\n 39.26628442213066\n ],\n [\n -82.3974609375,\n 38.44498466889473\n ],\n [\n -80.5078125,\n 40.111688665595956\n ],\n [\n -80.5078125,\n 42.293564192170095\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb8a0","contributors":{"authors":[{"text":"Central Great Lakes Geologic Mapping Coalition","contributorId":128101,"corporation":true,"usgs":false,"organization":"Central Great Lakes Geologic Mapping Coalition","id":528219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Illinois State Geological Survey","contributorId":127978,"corporation":true,"usgs":false,"organization":"Illinois State Geological Survey","id":528217,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Indiana Geological Survey","contributorId":128211,"corporation":true,"usgs":false,"organization":"Indiana Geological Survey","id":528220,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Michigan Geological Survey Division","contributorId":127870,"corporation":true,"usgs":false,"organization":"Michigan Geological Survey Division","id":528215,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ohio Division of Geological Survey","contributorId":127891,"corporation":true,"usgs":false,"organization":"Ohio Division of Geological Survey","id":528216,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528218,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":4410,"text":"cir1187 - 1999 - Surviving a tsunami: lessons from Chile, Hawaii, and Japan","interactions":[],"lastModifiedDate":"2014-09-30T11:01:28","indexId":"cir1187","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1187","title":"Surviving a tsunami: lessons from Chile, Hawaii, and Japan","docAbstract":"Actions that save lives, and actions that cost lives, as recounted by eyewitnesses to the tsunami from the largest earthquake ever measured--the magnitude 9.5 earthquake in Chile on May 22, 1960.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;","doi":"10.3133/cir1187","isbn":"0607928441","collaboration":"Revised and reprinted 2005. See also Spanish version, CIR 1218","usgsCitation":"Atwater, B.F., Cisternas, M.V., Bourgeois, J., Dudley, W.C., Hendley, J.W., and Stauffer, P.H., 1999, Surviving a tsunami: lessons from Chile, Hawaii, and Japan (Version 1.1 2005): U.S. Geological Survey Circular 1187, 18 p. :ill. (some col.), maps (some col.) ;22 x 28 cm., https://doi.org/10.3133/cir1187.","productDescription":"18 p. :ill. (some col.), maps (some col.) ;22 x 28 cm.","costCenters":[],"links":[{"id":117504,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/cir_1187.bmp"},{"id":62,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/circ/c1187/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.1 2005","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68815c","contributors":{"authors":[{"text":"Atwater, Brian F. 0000-0003-1155-2815 atwater@usgs.gov","orcid":"https://orcid.org/0000-0003-1155-2815","contributorId":3297,"corporation":false,"usgs":true,"family":"Atwater","given":"Brian","email":"atwater@usgs.gov","middleInitial":"F.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":149061,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cisternas, Marco V.","contributorId":84347,"corporation":false,"usgs":true,"family":"Cisternas","given":"Marco","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":149064,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bourgeois, Joanne","contributorId":57443,"corporation":false,"usgs":true,"family":"Bourgeois","given":"Joanne","email":"","affiliations":[],"preferred":false,"id":149063,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dudley, Walter C.","contributorId":54580,"corporation":false,"usgs":true,"family":"Dudley","given":"Walter","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":149062,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hendley, James W. II jhendley@usgs.gov","contributorId":2547,"corporation":false,"usgs":true,"family":"Hendley","given":"James","suffix":"II","email":"jhendley@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":false,"id":149060,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stauffer, Peter H. pstauffe@usgs.gov","contributorId":1219,"corporation":false,"usgs":true,"family":"Stauffer","given":"Peter","email":"pstauffe@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":149059,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70021282,"text":"70021282 - 1999 - An in situ occurrence of coal balls in the Amburgy coal bed, Pikeville Formation (Duckmantian), central Appalachian Basin, USA","interactions":[],"lastModifiedDate":"2025-03-11T16:25:36.548973","indexId":"70021282","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3000,"text":"Palaios","active":true,"publicationSubtype":{"id":10}},"title":"An in situ occurrence of coal balls in the Amburgy coal bed, Pikeville Formation (Duckmantian), central Appalachian Basin, USA","docAbstract":"Carbonate concretions containing permineralized peat, commonly called coal balls, were encountered in the Amburgy coal, a generally low-ash (9.4%), but commonly high-sulfur (3.6%), Middle Pennsylvanian coal of the Eastern Kentucky Coal Field. These are the first coal balls from the Amburgy coal, and one of only a few reported occurrences from the central Appalachian Basin. The coal balls occur in the upper part of the coal, between two paleochannel cut-outs at the top of the Pikeville Formation, and immediately beneath a scour with a marine fossil lag at the base of the Kendrick Shale Member, Hyden Formation. The coal is thickest (1.3 m) in a narrow (<300 m), elongate depression between the bounding paleochannels, and thins toward the occurrence of coal balls. Total biovolume as measured from acetate peels of coal balls indicates cordaites or lycopsid (36.1% each) dominance. Vertical sampling through one coal-ball aggregate shows zoning from a lower cordaites-dominant (88.7%) assemblage, to a middle, degraded, sphenopsid-rich assemblage, to an upper lycopsid-dominant (88.6%) assemblage. Beneath the coal balls, palynologic and petrographic analyses indicate the basal and middle portions of the bed are dominated by arborescent lycopsid spores and cordaites pollen, and by vitrinite macerals. The top part of the bed, above the coal balls, contains increased intertinite macerals, increased percentages of small fern spores, and variable ash yield (5-21%). Thickening of the Amburgy coal along a structural low, in combination with basal high-ash yields, vitrinite-dominance, and heterogenous palynoflora, indicate paleotopographic control on initial peat accumulation. Abundant lycopsid spores in the basal and middle part of the coal reflect rheotrophic conditions consistent with accumulation in a paleotopographic depression. Apparent zonation preserved in one of the coal-ball masses may document plant successions in response to flooding. Similar percentages of cordaites and lycopods, respectively, in the zones above and below the degraded incursion interval reflect development of a mixed, successional pattern in response to the flooding. Coal-ball formation may have been facilitated by channeling along the Kendrick ravinement, within a paleotopographic depression, at the split margin of the Amburgy peat, either through direct transmittal of carbonates and marine waters into the peat, or through degassing of the peat beneath the scour.","language":"English","publisher":"GeoScienceWorld","doi":"10.2307/3515395","usgsCitation":"Greb, S.F., Eble, C.F., Chesnut, D., Phillips, T., and Hower, J., 1999, An in situ occurrence of coal balls in the Amburgy coal bed, Pikeville Formation (Duckmantian), central Appalachian Basin, USA: Palaios, v. 14, no. 5, p. 432-450, https://doi.org/10.2307/3515395.","productDescription":"19 p.","startPage":"432","endPage":"450","costCenters":[],"links":[{"id":229904,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kentucky","otherGeospatial":"eastern Kentucky","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -83.69980257547141,\n 38.70214789921263\n ],\n [\n -83.84300270599691,\n 37.75876408313333\n ],\n [\n -83.69980257547141,\n 36.80029100301837\n ],\n [\n -83.70457039308808,\n 36.64685681780912\n ],\n [\n -83.17474214453055,\n 36.75365616083732\n ],\n [\n -82.03874357522238,\n 37.44691270572568\n ],\n [\n -82.59245790499662,\n 38.15332014901537\n ],\n [\n -82.60201726667941,\n 38.47631209262711\n ],\n [\n -82.8216005215753,\n 38.72450440106374\n ],\n [\n -83.27024802949818,\n 38.66862072995167\n ],\n [\n -83.69980257547141,\n 38.70214789921263\n ]\n ]\n ],\n \"type\": \"Polygon\"\n },\n \"id\": 0\n }\n ]\n}","volume":"14","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ea74e4b0c8380cd4888f","contributors":{"authors":[{"text":"Greb, Stephen F.","contributorId":255517,"corporation":false,"usgs":false,"family":"Greb","given":"Stephen","email":"","middleInitial":"F.","affiliations":[{"id":51568,"text":"Kentucky Geological Survey, U. of Kentucky","active":true,"usgs":false}],"preferred":false,"id":389338,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eble, Cortland F.","contributorId":255518,"corporation":false,"usgs":false,"family":"Eble","given":"Cortland","email":"","middleInitial":"F.","affiliations":[{"id":51568,"text":"Kentucky Geological Survey, U. of Kentucky","active":true,"usgs":false}],"preferred":false,"id":389336,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chesnut, D.R. Jr.","contributorId":100548,"corporation":false,"usgs":true,"family":"Chesnut","given":"D.R.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":389340,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Phillips, T.L.","contributorId":43517,"corporation":false,"usgs":true,"family":"Phillips","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":389337,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hower, James C. 0000-0003-4694-2776","orcid":"https://orcid.org/0000-0003-4694-2776","contributorId":34561,"corporation":false,"usgs":false,"family":"Hower","given":"James C.","affiliations":[{"id":16123,"text":"University of Kentucky, Center for Applied Energy Research, 2540 Research Park Drive, Lexington, KY 40511, United States.","active":true,"usgs":false}],"preferred":false,"id":389339,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":21814,"text":"ofr99155 - 1999 - Geologic and seismic hazards investigations of the Cow Creek area, Death Valley National Park, California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:52","indexId":"ofr99155","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"99-155","title":"Geologic and seismic hazards investigations of the Cow Creek area, Death Valley National Park, California","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey],","doi":"10.3133/ofr99155","issn":"0566-8174","usgsCitation":"Machette, M., Martinez, C.N., Crone, A.J., Haller, K., and D’Addezio, G., 1999, Geologic and seismic hazards investigations of the Cow Creek area, Death Valley National Park, California: U.S. Geological Survey Open-File Report 99-155, ii, 42 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr99155.","productDescription":"ii, 42 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":154562,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0155/report-thumb.jpg"},{"id":8111,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/ofr-99-0155/","linkFileType":{"id":5,"text":"html"}},{"id":51303,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0155/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a816d","contributors":{"authors":[{"text":"Machette, Michael N.","contributorId":28963,"corporation":false,"usgs":true,"family":"Machette","given":"Michael N.","affiliations":[],"preferred":false,"id":185804,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martinez, Carlos N.","contributorId":21415,"corporation":false,"usgs":true,"family":"Martinez","given":"Carlos","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":185803,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crone, Anthony J. 0000-0002-3006-406X crone@usgs.gov","orcid":"https://orcid.org/0000-0002-3006-406X","contributorId":790,"corporation":false,"usgs":true,"family":"Crone","given":"Anthony","email":"crone@usgs.gov","middleInitial":"J.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":185801,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Haller, Kathleen M. haller@usgs.gov","contributorId":1331,"corporation":false,"usgs":true,"family":"Haller","given":"Kathleen M.","email":"haller@usgs.gov","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":false,"id":185802,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"D’Addezio, Giuliana","contributorId":42837,"corporation":false,"usgs":true,"family":"D’Addezio","given":"Giuliana","email":"","affiliations":[],"preferred":false,"id":185805,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":21741,"text":"ofr99144 - 1999 - Digital geologic map of the Sandpoint 1- by 2-degree quadrangle, Washington, Idaho, and Montana","interactions":[],"lastModifiedDate":"2023-06-15T12:11:10.313444","indexId":"ofr99144","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"99-144","title":"Digital geologic map of the Sandpoint 1- by 2-degree quadrangle, Washington, Idaho, and Montana","docAbstract":"

The geology of the Sandpoint 1:250,000 quadrangle, Washington, Idaho, and Montana was mapped by F.K. Miller, R.F. Burmester, D.M. Miller, and R.E. Powell between 1963 and 1995 onto a scale-stable 1:250,000 topographic map base and subsequently input into an Arc/Info geographic information system (GIS) by P.D. Derkey. The digital geologic map database can be queried in many ways to produce a variety of derivative geologic maps.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr99144","usgsCitation":"Miller, F.K., Burmester, R., Powell, R.E., Miller, D., and Derkey, P.D., 1999, Digital geologic map of the Sandpoint 1- by 2-degree quadrangle, Washington, Idaho, and Montana: U.S. Geological Survey Open-File Report 99-144, Report: ii, 58 p.; 1 Plate: 43.00 x 28.00 inches; Readme; Metadata; Data Package, https://doi.org/10.3133/ofr99144.","productDescription":"Report: ii, 58 p.; 1 Plate: 43.00 x 28.00 inches; Readme; Metadata; Data Package","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":154156,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_99_144.png"},{"id":257339,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/0144/","linkFileType":{"id":5,"text":"html"}},{"id":257340,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0144/of99-144_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":257341,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1999/0144/of99-144_plate1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397636,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22659.htm"}],"scale":"250000","projection":"Universal Transverse Mercator","country":"United States","state":"Idaho, Montana, Washington","otherGeospatial":"Sandpoint 1 x 2 degree quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118,48 ], [ -118,49 ], [ -116,49 ], [ -116,48 ], [ -118,48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65ab44","contributors":{"authors":[{"text":"Miller, F. K.","contributorId":10803,"corporation":false,"usgs":true,"family":"Miller","given":"F.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":185489,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burmester, R. F.","contributorId":83539,"corporation":false,"usgs":true,"family":"Burmester","given":"R. F.","affiliations":[],"preferred":false,"id":185491,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Powell, R. E.","contributorId":93046,"corporation":false,"usgs":true,"family":"Powell","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":185492,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, D. M. 0000-0003-3711-0441","orcid":"https://orcid.org/0000-0003-3711-0441","contributorId":104422,"corporation":false,"usgs":true,"family":"Miller","given":"D. M.","affiliations":[],"preferred":false,"id":185493,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Derkey, P. D.","contributorId":55035,"corporation":false,"usgs":true,"family":"Derkey","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":185490,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":25903,"text":"wri964287 - 1999 - Hydrogeology and geochemistry of acid mine drainage in ground water in the vicinity of Penn Mine and Camanche Reservoir, Calaveras County, California: Summary report, 1993–95","interactions":[],"lastModifiedDate":"2022-01-10T20:33:07.717133","indexId":"wri964287","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"96-4287","title":"Hydrogeology and geochemistry of acid mine drainage in ground water in the vicinity of Penn Mine and Camanche Reservoir, Calaveras County, California: Summary report, 1993–95","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964287","usgsCitation":"Alpers, C.N., Hamlin, S.N., and Hunerlach, M., 1999, Hydrogeology and geochemistry of acid mine drainage in ground water in the vicinity of Penn Mine and Camanche Reservoir, Calaveras County, California: Summary report, 1993–95: U.S. Geological Survey Water-Resources Investigations Report 96-4287, vi, 59 p., https://doi.org/10.3133/wri964287.","productDescription":"vi, 59 p.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":394130,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16450.htm"},{"id":119074,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4287/report-thumb.jpg"},{"id":54662,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4287/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Calaveras County","otherGeospatial":"vicinity of Penn Mine and Camanche Reservoir","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.88,\n 38.229\n ],\n [\n -120.873,\n 38.229\n ],\n [\n -120.873,\n 38.236\n ],\n [\n -120.88,\n 38.236\n ],\n [\n -120.88,\n 38.229\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db627164","contributors":{"authors":[{"text":"Alpers, Charles N. 0000-0001-6945-7365 cnalpers@usgs.gov","orcid":"https://orcid.org/0000-0001-6945-7365","contributorId":411,"corporation":false,"usgs":true,"family":"Alpers","given":"Charles","email":"cnalpers@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":195453,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hamlin, S. N.","contributorId":46560,"corporation":false,"usgs":true,"family":"Hamlin","given":"S.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":195451,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hunerlach, M. P.","contributorId":73646,"corporation":false,"usgs":true,"family":"Hunerlach","given":"M. P.","affiliations":[],"preferred":false,"id":195452,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":23625,"text":"ofr9967 - 1999 - Simulation of the effects of operating lakes Mendota, Monona, and Waubesa, south-central Wisconsin, as multipurpose reservoirs to maintain dry-weather flow","interactions":[],"lastModifiedDate":"2015-10-15T13:29:50","indexId":"ofr9967","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"99-67","title":"Simulation of the effects of operating lakes Mendota, Monona, and Waubesa, south-central Wisconsin, as multipurpose reservoirs to maintain dry-weather flow","docAbstract":"

A digital reservoir routing model was used to simulate the operation of Lakes Mendota, Monona, and Waubesa, south-central Wisconsin for various levels of minimum release. Twenty-five years of record (1970?94) were used in model simulation. The amount of water available to maintain streamflow and lake levels during dry periods has declined because of extensive pumping of ground water for municipal use and diversion of the effluent around the lakes. The goal of the simulation was to determine whether using the lakes as multipurpose reservoirs to maintain flow during periods of low flow would appreciably lower the lake levels. The model results indicated that it would be possible to maintain a minimum flow of 36 cubic feet per second in all but the driest years simulated (1970, 1976, 1977, 1981, 1989, and 1991) without lowering the lake levels more than they have been lowered from 1970 to 1994 under current operating conditions. Maintaining minimum flow would require detailed computations to guide the operation of the dams during the year.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9967","issn":"0094-9140","usgsCitation":"Krug, W., 1999, Simulation of the effects of operating lakes Mendota, Monona, and Waubesa, south-central Wisconsin, as multipurpose reservoirs to maintain dry-weather flow: U.S. Geological Survey Open-File Report 99-67, iv, 18 p., https://doi.org/10.3133/ofr9967.","productDescription":"iv, 18 p.","numberOfPages":"21","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":154913,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0067/report-thumb.jpg"},{"id":1665,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr99-067","linkFileType":{"id":5,"text":"html"}},{"id":52902,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0067/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Dane County","otherGeospatial":"Lake Mendota, Lake Menona, Lake Waubesa","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.59075927734375,\n 42.896088552971065\n ],\n [\n -89.59075927734375,\n 43.180145655844626\n ],\n [\n -89.0936279296875,\n 43.180145655844626\n ],\n [\n -89.0936279296875,\n 42.896088552971065\n ],\n [\n -89.59075927734375,\n 42.896088552971065\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f1da6","contributors":{"authors":[{"text":"Krug, W.R.","contributorId":23147,"corporation":false,"usgs":true,"family":"Krug","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":190442,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23643,"text":"ofr99132 - 1999 - How to build a model illustrating sea-floor spreading and subduction","interactions":[],"lastModifiedDate":"2017-03-09T14:17:46","indexId":"ofr99132","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"99-132","title":"How to build a model illustrating sea-floor spreading and subduction","docAbstract":"

This report describes how to build a model of the outer 300 km (180 miles) of the Earth that can be used to develop a better understanding of the principal features of plate tectonics, including sea-floor spreading, the pattern of magnetic stripes frozen into the sea floor, transform faulting, thrust faulting, subduction, and volcanism. In addition to a paper copy of this report, the materials required are a cardboard shoebox, glue, scissors, straight edge, and safety razor blade.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr99132","issn":"0094-9140","usgsCitation":"Lahr, J., 1999, How to build a model illustrating sea-floor spreading and subduction: U.S. Geological Survey Open-File Report 99-132, 16 p. , https://doi.org/10.3133/ofr99132.","productDescription":"16 p. ","costCenters":[],"links":[{"id":154918,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0132/report-thumb.jpg"},{"id":1684,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/ofr-99-0132/","linkFileType":{"id":5,"text":"html"}},{"id":52913,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0132/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bd1e","contributors":{"authors":[{"text":"Lahr, J.C.","contributorId":34892,"corporation":false,"usgs":true,"family":"Lahr","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":190473,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23059,"text":"ofr99169 - 1999 - An ARC/Info point coverage of Mineral Resource Data System (MRDS) locations in eleven western states","interactions":[],"lastModifiedDate":"2023-06-15T12:12:12.607525","indexId":"ofr99169","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"99-169","title":"An ARC/Info point coverage of Mineral Resource Data System (MRDS) locations in eleven western states","docAbstract":"

This ARC/Info coverage, derived from the USGS Mineral Resource Data System (MRDS), contains 60,490 records that fall within the states of Arizona, California, Colorado, Idaho, Montana, New Mexico, Nevada, Oregon, Utah, Washington, Wyoming. The dataset has 13 fields containing information on record identification, location, commodity, geology, and deposit type. The data for this report was retrieved from the master database as a tab text file and imported into a Microsoft Access database. The data was then imported into ESRI’s ArcView where shape files were created. These shape files were then converted into an ARC/INFO coverage.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr99169","usgsCitation":"Frank, D.G., 1999, An ARC/Info point coverage of Mineral Resource Data System (MRDS) locations in eleven western states: U.S. Geological Survey Open-File Report 99-169, Report: 14 p., Metadata, https://doi.org/10.3133/ofr99169.","productDescription":"Report: 14 p., Metadata","numberOfPages":"14","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":403665,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16674.htm"},{"id":284617,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1999/0169/westmrds.zip"},{"id":284616,"rank":4,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/1999/0169/westmrds.met"},{"id":284618,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1999/0169/mrdsplot.aml"},{"id":52429,"rank":7,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0169/pdf/of99-169.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156595,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0169/report-thumb.jpg"},{"id":1477,"rank":6,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/0169/","linkFileType":{"id":5,"text":"html"}}],"scale":"1250000","country":"United States","state":"Arizona, California, Colorado, Idaho, Montana, New Mexico, Nevada, Oregon, Utah, Washington, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.461,\n 31.329\n ],\n [\n -102.044,\n 31.329\n ],\n [\n -102.044,\n 49\n ],\n [\n -124.461,\n 49\n ],\n [\n -124.461,\n 31.329\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4c51e4b0b290850f0e6b","contributors":{"authors":[{"text":"Frank, David G. dfrank@usgs.gov","contributorId":3274,"corporation":false,"usgs":true,"family":"Frank","given":"David","email":"dfrank@usgs.gov","middleInitial":"G.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":189365,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23235,"text":"ofr99162 - 1999 - Geology of the Cordelia and the northern part of the Benicia 7.5 minute quadrangles, California: A digital map database","interactions":[],"lastModifiedDate":"2021-12-07T21:39:20.11529","indexId":"ofr99162","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"99-162","title":"Geology of the Cordelia and the northern part of the Benicia 7.5 minute quadrangles, California: A digital map database","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr99162","issn":"0094-9140","usgsCitation":"Graymer, R., Brabb, E.E., and Jones, D.L., 1999, Geology of the Cordelia and the northern part of the Benicia 7.5 minute quadrangles, California: A digital map database: U.S. Geological Survey Open-File Report 99-162, HTML Document, https://doi.org/10.3133/ofr99162.","productDescription":"HTML Document","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":109888,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23004.htm","linkFileType":{"id":5,"text":"html"},"description":"23004"},{"id":155377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1383,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/of99-162/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"California","otherGeospatial":"Cordelia and the northern part of the Benicia 7.5 minute quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.25,\n 38.044\n ],\n [\n -122.125,\n 38.044\n ],\n [\n -122.126,\n 38.25\n ],\n [\n -122.25,\n 38.25\n ],\n [\n -122.25,\n 38.044\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db681213","contributors":{"authors":[{"text":"Graymer, R. W.","contributorId":21174,"corporation":false,"usgs":true,"family":"Graymer","given":"R. W.","affiliations":[],"preferred":false,"id":189693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brabb, E. E.","contributorId":43780,"corporation":false,"usgs":true,"family":"Brabb","given":"E.","middleInitial":"E.","affiliations":[],"preferred":false,"id":189694,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jones, D. L.","contributorId":65045,"corporation":false,"usgs":true,"family":"Jones","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":189695,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":22499,"text":"ofr99514 - 1999 - Puget Sound aeromagnetic maps and data","interactions":[],"lastModifiedDate":"2012-02-02T00:08:07","indexId":"ofr99514","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"99-514","title":"Puget Sound aeromagnetic maps and data","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr99514","issn":"0094-9140","usgsCitation":"Blakely, R.J., Wells, R., and Weaver, C.S., 1999, Puget Sound aeromagnetic maps and data (Version 1.0): U.S. Geological Survey Open-File Report 99-514, multiple online maps and data files, https://doi.org/10.3133/ofr99514.","productDescription":"multiple online maps and data files","costCenters":[],"links":[{"id":1553,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/of99-514/","linkFileType":{"id":5,"text":"html"}},{"id":155607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db655ab1","contributors":{"authors":[{"text":"Blakely, Richard J. 0000-0003-1701-5236 blakely@usgs.gov","orcid":"https://orcid.org/0000-0003-1701-5236","contributorId":1540,"corporation":false,"usgs":true,"family":"Blakely","given":"Richard","email":"blakely@usgs.gov","middleInitial":"J.","affiliations":[{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":188358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wells, Ray E. 0000-0002-7796-0160 rwells@usgs.gov","orcid":"https://orcid.org/0000-0002-7796-0160","contributorId":2692,"corporation":false,"usgs":true,"family":"Wells","given":"Ray E.","email":"rwells@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":188360,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weaver, Craig S. craig@usgs.gov","contributorId":2690,"corporation":false,"usgs":true,"family":"Weaver","given":"Craig","email":"craig@usgs.gov","middleInitial":"S.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":188359,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":24464,"text":"ofr9968 - 1999 - Identification of potential wetlands in training areas on Ravenna Army Ammunition Plant, Ohio, and guidelines for their management","interactions":[],"lastModifiedDate":"2012-02-02T00:08:09","indexId":"ofr9968","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"99-68","title":"Identification of potential wetlands in training areas on Ravenna Army Ammunition Plant, Ohio, and guidelines for their management","docAbstract":"Potential wetlands in training areas on Ravenna Army Ammunition Plant, Ohio, were mapped by use of geographic information system (GIS) data layers and field inspection. The GIS data layers were compiled from existing sources and interpretation of aerial photography. Data layers used in the GIS analysis were wetland-plant communities, hydric soils, National Wetlands Inventory designated areas, and wet areas based on photogrammetry. According to review of these data layers, potential wetlands constitute almost one-third of the land in the training areas. A composite map of these four data layers was compiled for use during inspection of the training areas. Field inspection focused on the presence of hydrophytic vegetation and macroscopic evidences of wetland hydrology. Results of the field inspection were in general agreement with those predicted by the GIS analysis, except that some wet areas were more extensive than predicted because of high amounts of precipitation during critical periods of 1995 and 1996. Guidelines for managing wetlands in the training areas are presented.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr9968","issn":"0094-9140","usgsCitation":"Schalk, C.W., Tertuliani, J., and Darner, R., 1999, Identification of potential wetlands in training areas on Ravenna Army Ammunition Plant, Ohio, and guidelines for their management: U.S. Geological Survey Open-File Report 99-68, iv, 78 p. :col. ill., col. maps ;28 cm., https://doi.org/10.3133/ofr9968.","productDescription":"iv, 78 p. :col. ill., col. maps ;28 cm.","costCenters":[],"links":[{"id":156643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0068/report-thumb.jpg"},{"id":53532,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0068/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faa64","contributors":{"authors":[{"text":"Schalk, C. W.","contributorId":64286,"corporation":false,"usgs":true,"family":"Schalk","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":191978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tertuliani, J.S.","contributorId":27490,"corporation":false,"usgs":true,"family":"Tertuliani","given":"J.S.","affiliations":[],"preferred":false,"id":191977,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Darner, R.A.","contributorId":19193,"corporation":false,"usgs":true,"family":"Darner","given":"R.A.","affiliations":[],"preferred":false,"id":191976,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":24022,"text":"ofr99170 - 1999 - Geochemical investigations and interim recommendations for priority abandoned mine sites on U.S.D.A. Forest Service lands, Mineral Creek watershed, San Juan County, Colorado","interactions":[],"lastModifiedDate":"2022-09-01T19:09:56.658793","indexId":"ofr99170","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"99-170","title":"Geochemical investigations and interim recommendations for priority abandoned mine sites on U.S.D.A. Forest Service lands, Mineral Creek watershed, San Juan County, Colorado","docAbstract":"Field observations, sampling of mine dumps and mine drainage waters, and\r\nlaboratory studies of dump materials have been made at mining areas deemed to be on\r\npublic lands administered by the USDA Forest Service in the Mineral Creek watershed.\r\nResults of chemical analyses of dump materials, leachates of those materials, and of\r\nsurface waters draining mines or dumps provide indications of where acid is generated or\r\nconsumed, and what metals are mobilized below mines or dumps. Information on 25\r\nsites is reviewed and reclamation priorities are ranked into four classes (high, medium,\r\nlow priority, or no work required).\r\nThe western side of the upper Animas watershed (the Mineral Creek watershed)\r\nhas a history of mining and prospecting for about 130 years. The intensity of miningrelated\r\ndisturbance is higher than in most parts of the San Juan Mountains region, but\r\nactually is much less than the eastern half of the watershed (US BLM lands) and none of\r\nthe mines moved millions of tons of rock and ore as in some of the eastern mines. The\r\nmajority of the roughly one thousand mining sites on the USFS lands are very small (less\r\nthan 100 tons or 70 cubic yards of dump material), are more than 2 miles from a major\r\nstream, or are so inaccessible as to prohibit reclamation. Twenty five sites have been\r\nconsidered by others to have significant size and potential for significant environmental\r\ndegradation. These most significant mining areas were evaluated by multiple criteria,\r\nincluding tendency to generate acid or liberate toxic metals, observed acidic pH or dead\r\nvegetation (?kill zones?) below dumps or adits, potential mobility of metals, and\r\nlikelihood of transport into streams of the watershed. In the author?s opinion, no single\r\nmeasurable parameter, such as metal concentration, is reliable for ranking significance or\r\nfeasibility of reclamation. Rather, subjective estimates are required to evaluate\r\ncombinations of, or interactions among, several parameters. The most subjective\r\nestimate in ranking feasibility of reclamation is the amount of natural and mine-related\r\ncontamination at each mining area. Mitigation of natural contributions at mines or\r\nunmined areas is beyond the scope of these Abandoned Mine Lands (AML)\r\ninvestigations, but must be considered when planning reclamation. Available\r\ninformation for the 25 problem sites is adequate for ranking, but at some sites additional\r\ninformation on groundwater conditions is needed for a more reliable ranking and\r\nevaluation of reclamation methods.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston","doi":"10.3133/ofr99170","usgsCitation":"Nash, J., 1999, Geochemical investigations and interim recommendations for priority abandoned mine sites on U.S.D.A. Forest Service lands, Mineral Creek watershed, San Juan County, Colorado: U.S. Geological Survey Open-File Report 99-170, 31 p., https://doi.org/10.3133/ofr99170.","productDescription":"31 p.","costCenters":[],"links":[{"id":156745,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1704,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/ofr-99-0170/","linkFileType":{"id":5,"text":"html"}},{"id":406087,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16449.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","county":"San Juan County","otherGeospatial":"Mineral Creek watershed","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.804,\n 37.78\n ],\n [\n -107.547,\n 37.78\n ],\n [\n -107.547,\n 38.025\n ],\n [\n -107.804,\n 38.025\n ],\n [\n -107.804,\n 37.78\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae242","contributors":{"authors":[{"text":"Nash, J. T.","contributorId":31751,"corporation":false,"usgs":true,"family":"Nash","given":"J. T.","affiliations":[],"preferred":false,"id":191178,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}