The Florida shelf represents a finite source of economic resources, including commercial and recreational fisheries, tourism, recreation, sand and gravel resources, phosphate, and freshwater reserves. Yet the basic information needed to locate resources, or to interpret and utilize existing data, comes from many sources, dates, and formats. A multi-agency effort is underway to coordinate and prioritize the compilation of suitable datasets for an integrated information system of Florida’s coastal and ocean resources. This report and the associated data files represent part of the effort to make data accessible and useable with computer-mapping systems, web-based technologies, and user-friendly visualization tools. Among the datasets compiled and developed are seafloor imagery, marine sediment data, and existing bathymetric data. A U.S. Geological Survey-sponsored workshop in January 2007 resulted in the establishment of mapping priorities for the state. Bathymetry was identified as a common priority among agencies and researchers. State-of-the-art computer-mapping techniques and data-processing tools were used to develop shelf-wide raster and vector data layers. Florida Shelf Habitat (FLaSH) Mapping Project (http://coastal.er.usgs.gov/flash) endeavors to locate available data, identify data gaps, synthesize existing information, and expand our understanding of geologic processes in our dynamic coastal and marine systems.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071397","usgsCitation":"Robbins, L.L., Hansen, M., Raabe, E., Knorr, P.O., and Browne, J., 2007, Cartographic production for the Florida Shelf Habitat (FLaSH) map study: generation of surface grids, contours, and KMZ files: U.S. Geological Survey Open-File Report 2007-1397, HTML Document, https://doi.org/10.3133/ofr20071397.","productDescription":"HTML Document","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":292444,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":292443,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1397/"}],"country":"United States","state":"Florida","otherGeospatial":"Florida Shelf","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.0,25.0 ], [ -87.0,30.0 ], [ -80.0,30.0 ], [ -80.0,25.0 ], [ -87.0,25.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f25fc4e4b03334187188fa","contributors":{"authors":[{"text":"Robbins, Lisa L. 0000-0003-3681-1094 lrobbins@usgs.gov","orcid":"https://orcid.org/0000-0003-3681-1094","contributorId":422,"corporation":false,"usgs":true,"family":"Robbins","given":"Lisa","email":"lrobbins@usgs.gov","middleInitial":"L.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":498611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hansen, Mark","contributorId":81893,"corporation":false,"usgs":true,"family":"Hansen","given":"Mark","affiliations":[],"preferred":false,"id":498613,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Raabe, Ellen","contributorId":98402,"corporation":false,"usgs":true,"family":"Raabe","given":"Ellen","affiliations":[],"preferred":false,"id":498614,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Knorr, Paul O. pknorr@usgs.gov","contributorId":3691,"corporation":false,"usgs":true,"family":"Knorr","given":"Paul","email":"pknorr@usgs.gov","middleInitial":"O.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":498612,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Browne, Joseph","contributorId":102398,"corporation":false,"usgs":true,"family":"Browne","given":"Joseph","email":"","affiliations":[],"preferred":false,"id":498615,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70103487,"text":"ofr20071047SRP108 - 2007 - Structure of the central Terror Rift, western Ross Sea, Antarctica","interactions":[],"lastModifiedDate":"2014-05-05T13:32:52","indexId":"ofr20071047SRP108","displayToPublicDate":"2007-01-01T13:15:00","publicationYear":"2007","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":"2007-1047-SRP-108","title":"Structure of the central Terror Rift, western Ross Sea, Antarctica","docAbstract":"The Terror Rift is a zone of post-middle Miocene faulting and volcanism along the western margin of the \nWest Antarctic Rift System. A new seismic data set from NSF geophysical cruise NBP04-01, integrated with the \nprevious dataset to provide higher spatial resolution, has been interpreted in this study in order to improve \nunderstanding of the architecture and history of the Terror Rift. The Terror Rift contains two components, a \nstructurally-controlled rollover anticlinal arch intruded by younger volcanic bodies and an associated synclinal basin. \nOffsets and trend changes in fault patterns have been identified, coincident with shifts in the location of depocenters that \ndefine rift sub-basins, indicating that the Terror Rift is segmented by transverse structures. Multiple phases of faulting \nall post-date 17 Ma, including faults cutting the seafloor surface, indicating Neogene rifting and possible modern \nactivity.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. 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The Early Rift phase (?latest Eocene to Early \nOligocene) comprises wedges of strata confined by early extensional faults, and which contain seismic facies consistent \nwith drainage via coarse-grained fans and deltas into discrete, actively subsiding grabens and half-grabens. The Main \nRift phase (Early Oligocene to Early Miocene) comprises a lens of strata that thickens symmetrically from the basin \nmargins into a central depocenter, and in which stratal events pass continuously over the top of the Early Rift \nextensional topography. Internal seismic facies and lithofacies indicate a more organized, cyclical shallow marine \nsuccession, influenced increasingly upward by cycles of glacial advance and retreat into the basin. The Passive Thermal \nSubsidence phase (Early Miocene to ?) comprises an evenly distributed sheet of strata that does not thicken appreciably \ninto the depocentre, with more evidence for clinoform sets and large channels. These patterns are interpreted to record \naccumulation under similar environmental conditions but in a regime of slower subsidence. The Renewed Rifting phase \n(? to Recent, largely unsampled by coring thus far) has been further divided into 1, a lower interval, in which the section \nthickens passively towards a central depocentre, and 2. an upper interval, in which more dramatic thickening patterns \nare complicated by magmatic activity. The youngest part of the stratigraphy was accumulated under the influence of \nflexural loading imposed by the construction of large volcanic edifices, and involved minimal sediment supply from the \nwestern basin margin, suggesting a change in environmental (glacial) conditions at possibly c. 2 Ma.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. 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J.","contributorId":31942,"corporation":false,"usgs":false,"family":"Wilson","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":492496,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nash, T.R.","contributorId":63721,"corporation":false,"usgs":true,"family":"Nash","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":492498,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70074741,"text":"ofr20071047SRP025 - 2007 - Basement and crustal structure of the Davis Sea region (East Antarctica): implications for tectonic setting and continent to oceanic boundary definition","interactions":[],"lastModifiedDate":"2014-02-03T13:14:29","indexId":"ofr20071047SRP025","displayToPublicDate":"2007-01-01T13:01:00","publicationYear":"2007","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":"2007-1047-SRP-025","title":"Basement and crustal structure of the Davis Sea region (East Antarctica): implications for tectonic setting and continent to oceanic boundary definition","docAbstract":"This study is based on about 8400 km of MCS, magnetic and gravity data as well as 20 sonobuoys collected \nby the Russian Antarctic Expedition during 2003 and 2004 in the Davis Sea and adjacent areas between 80°E and \n102°E. Major tectonic provinces and features are identified and mapped in the study region including: 1) A marginal rift \nwith a the extended continental crust ranging 130 to more than 200 km in width; 2) The marginal volcanic plateau of the \nBruce Bank consisting of the Early Cretaceous igneous rocks; 3) The Early Cretaceous and Late Cretaceous−Paleogene \noceanic basins; and 4) The Early Cretaceous igneous province of the Kerguelen Plateau. Four major horizons identified \nin the sedimentary cover of the Davis Sea region are attributed to main tectonic events and/or paleoenvironmental \nchanges.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. 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This study characterizes the textures, fabrics and grain-scale structures from thin \nsection analysis of samples of microfaults, veins, and clastic dikes. Microfaults are abundant and display two different \ntypes of textures, interpreted to record two different deformation modes: pre-lithification shearing and brittle faulting of \ncohesive sediment. Both clastic dikes and calcite veins commonly follow fault planes, indicating that injections of \nliquefied sediment and circulating fluids used pre-existing faults as conduits. The close association of clastic injections, \ndiagenetic mineralization, and faulting indicates that faulting was synchronous with deposition in the rift basin","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP053","usgsCitation":"Millan, C., Wilson, T., and Paulsen, T., 2007, Microstructural study of natural fractures in Cape Roberts Project 3 core, Western Ross Sea, Antarctica: U.S. Geological Survey Open-File Report 2007-1047-SRP-053, 4 p., https://doi.org/10.3133/ofr20071047SRP053.","productDescription":"4 p.","onlineOnly":"N","costCenters":[],"links":[{"id":282487,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP053.JPG"},{"id":282486,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp053/of2007-1047srp053.pdf"}],"otherGeospatial":"Antarctica;Ross Sea","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -165.07,-79.3 ], [ -165.07,-76.9 ], [ -157.42,-76.9 ], [ -157.42,-79.3 ], [ -165.07,-79.3 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd670fe4b0b29085101220","contributors":{"authors":[{"text":"Millan, C.","contributorId":94123,"corporation":false,"usgs":true,"family":"Millan","given":"C.","email":"","affiliations":[],"preferred":false,"id":490542,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, T.","contributorId":49581,"corporation":false,"usgs":true,"family":"Wilson","given":"T.","affiliations":[],"preferred":false,"id":490540,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Paulsen, T.","contributorId":78167,"corporation":false,"usgs":true,"family":"Paulsen","given":"T.","email":"","affiliations":[],"preferred":false,"id":490541,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70094739,"text":"ofr20071047SRP062 - 2007 - Metamorphic conditions during formation of a metapelitic sillimanite-garnet gneiss from Clemence Massif, Prince Charles Mountains, East Antarctica","interactions":[],"lastModifiedDate":"2014-02-24T13:57:27","indexId":"ofr20071047SRP062","displayToPublicDate":"2007-01-01T12:55:00","publicationYear":"2007","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":"2007-1047-SRP-062","title":"Metamorphic conditions during formation of a metapelitic sillimanite-garnet gneiss from Clemence Massif, Prince Charles Mountains, East Antarctica","docAbstract":"The pressure (P) and temperature (T) conditions during metamorphism of a metapelitic sillimanite-garnet \ngneiss from Clemence Massif, Antarctic Prince Charles Mountains, are estimated using mineral abundance information \nand petrogenetic P–T pseudosections computed in the chemical system MnO–N2O–CaO–K2O–FeO–MgO–Al2O3–\nSiO2–H2O–TiO2–Fe2O3 (MnNCKFMASHTO). Calculated mineral equilibria for the appropriate bulk composition predict that the observed assemblage, of K-feldspar–garnet–quartz–sillimanite–biotite–ilmenite–rutile, stabilised at \napproximately 8–9 kbar and 760–790ºC. Reaction microstructures are rare, but the preservation of relic spinel \ninclusions in garnet indicates an earlier low-P, high-T component and possible anticlockwise path.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. 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