3 edition of Aquifer test to determine hydraulic properties of the Elm Aquifer near Aberdeen, South Dakota found in the catalog.
Aquifer test to determine hydraulic properties of the Elm Aquifer near Aberdeen, South Dakota
Bryan D. Schaap
by U.S. Dept. of the Interior, U.S. Geological Survey, Information Services [distributor] in Rapid City, SD, Denver, CO
Written in English
Includes bibliographical references (p. 15-16).
|Statement||by Bryan D. Schaap ; prepared in cooperation with the city of Aberdeen.|
|Series||Water-resources investigations report ;, 00-4264|
|Contributions||Aberdeen (S.D.), Geological Survey (U.S.)|
|LC Classifications||GB701 .W375 no. 00-4264|
|The Physical Object|
|Pagination||iv, 23 p. :|
|Number of Pages||23|
|LC Control Number||2001315898|
About , wells pumped water from the aquifer to irrigate about 13 million acres in the High Plains in The High Plains aquifer is a regional water-table aquifer consisting mostly of near-surface sand and gravel deposits. In , the maximum saturated thickness of the aquifer was about 1, feet and averaged by: The High Plains aquifer extends from south of 32 degrees to almost 44 degrees north latitude and from 96 degrees 30 minutes to degrees west longitude. The outcrop area covers , square miles and is present in Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South .
An aquifer test of a water well located miles NNE of the abandoned Riley Pass uranium mine in the North Cave Hills was conducted to assess potential for aquifer contamination from past mining. (fig. 1), where the Dakota is used as a primary or secondary source of water. In the central Great Plains, the Dakota aquifer consists primarily of the Dakota Formation, which occurs in parts of Nebraska, South Dakota, North Dakota, Kansas, Iowa and Minnesota, according to Witzke and Ludvigson (). ForCited by: 2. Aquifer by Jonathan Freisen is a post-apocalyptic story. It is and there is only one fresh water source left in the world. Only one man, and his son, are capable of trading with the rats that live underground that protect the water source/5.
Listing of South Dakota Discontinued, Threatened, or Endangered Stations Choose Site Selection Criteria There sites with groundwater-level measurements. The Southern Hills aquifer system is the primary source of public water in the northern ten parishes of southeastern aquifer dips towards the Gulf of Mexico and extends from the northern limit of the recharge region near Vicksburg, Mississippi, and as far south as the Baton Rouge area in south Louisiana. There are about thirteen aquifer units composing the system in the southern Australia: Gnangara Mound, Great Artesian . Title: Two-Well Test Method for Determining Hydraulic Properties of Aquifers Created Date: Mon Dec 29
construction of computer produced views of three-dimensional data
Show and tell
A little book of Irish sayings
The capitulations and articles of peace betweene the Majestie of the King of England, Scotland, France, & Ireland, &c., and the Sultan of the Ottoman Empire
effect of a novel source of n-3 fatty acids on glycemic control in type 2 diabetes.
Bridges across Missouri River at or near Omaha, Nebr., and Council Bluffs, Iowa.
Company law reform
Islam and modernism.
Education and science in ...
Case Based Echocardiography
Walks round red brick
Contested election case, Gerling v. Dunn.
SyntaxTextGen not activated This digital data set consists of hydraulic pdf contours pdf polygons for the High Plains aquifer in the central United States. The High Plains aquifer extends from south of 32 degrees to almost 44 degrees north latitude and from 96 degrees 30 minutes to almost degrees west h Year: Final – Aquifer Test and Related Well Information for Public Water Supply Wells in Groundwater Management Area 8 viii Figure Aquifer Test Tool user interface prior to a well selection.
(The path shown in the red rectangle designates the location of the aquifer testFile Size: 8MB.The extent of the Dakota aquifer system in Kansas is shown in fig. ebook. Not all of the ebook formations comprising the Dakota aquifer are present throughout the aquifer's extent (Macfarlane, ).
In western and parts of central Kansas, the Dakota aquifer system is separated into upper and lower aquifers by an aquitard within the Kiowa Formation.