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The carbonate-rock aquifer system is underlain by Ordovician shales and interbedded carbonate rocks that are virtually impermeable and regionally extensive. These units collectively form a barrier to ground-water flow that effectively limits the transfer of significant quantities of water through the base of the Silurian and Devonian carbonate aquifer. Where the shales and siltstones that make up the upper confining unit are present, the carbonate-rock aquifer is confined above by Devonian and Mississippian shales and siltstones. Where the confining unit above the aquifer has been eroded, the overlying glacial sediments partly confine the carbonate-rock.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/pp1423B","usgsCitation":"Casey, G.D., 1996, Hydrogeologic framework of the Midwestern Basins and Arches region in parts of Indiana, Ohio, Michigan, and Illinois: U.S. Geological Survey Professional Paper 1423, p. 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96526B","usgsCitation":"Ratcliffe, N.M., and Burton, W., 1996, Digital bedrock geologic map of the Weston quadrangle, Vermont: U.S. Geological Survey Open-File Report 96-526, 2 Computer Disks, https://doi.org/10.3133/ofr96526B.","productDescription":"2 Computer Disks","costCenters":[],"links":[{"id":108975,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18639.htm","linkFileType":{"id":5,"text":"html"},"description":"18639"},{"id":155049,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Vermont","otherGeospatial":"Weston quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -72.875,\n 43.375\n ],\n [\n -72.875,\n 43.25\n ],\n [\n -72.75,\n 43.25\n ],\n [\n -72.75,\n 43.375\n ],\n [\n -72.875,\n 43.375\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d574","contributors":{"authors":[{"text":"Ratcliffe, N. 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Horizontal fracture zones within the Lockport Group were represented by model layers, and connections between the zones were represented by vertical leakage between the layers. Results of steady-state simulations were compared with (1) the observed potentiometric surface of the weathered bedrock surface, (2) average heads measured by piezometers in underlying fracture zones, (3) low-flow measurements of springs and streams, and (4) measurements of discharge from tunnels and excavations. Results indicated that (1) measured flow into the Falls Street tunnel, an unlined storm sewer excavated in bedrock, exceeds the amount that can be sustained by the aquifer, and, therefore, a connection between the tunnel and the Niagara River can be assumed; (2) recharge within the urban parts of the modeled area is greater than in rural areas, possibly because of losses from the municipal water supply or infiltration from unlined storm sewers that intersect the bedrock; and (3) lowlands near the Niagara River might contain widespread areas of upward flow that discharge ground water through evapotranspiration and surface drainage.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wsp2487","usgsCitation":"Yager, R.M., 1996, Simulated three-dimensional ground-water flow in the Lockport Group, a fractured-dolomite aquifer near Niagara Falls, New York: U.S. Geological Survey Water Supply Paper 2487, v, 42 p. :ill. 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