Add to ORKGDuring 1974, the U.S. Geological Survey began a comprehensive hydrologic study of the oil-shale area in the southeastern Uinta Basin of Utah and Colorado. From 1976 to 1978, six deep test holes were drilled principally to obtain information about aquifers in the Green River Formation of Tertiary age. Information obtained from the drilling project includes description of lithologic samples from core and drill cuttings, temperature and geophysical logs, drilling logs, packer tests, aquifer (pumping and recovery) tests, and analyses of water samples
This text is to be used in conjunction with Coal Resource Occurrence (CRO) and Coal Development Pote...
Due to recent land use changes, runoff has greatly increased In Bowling Green, necessitating the dri...
In mid-April, 1983, an old landslide near Thistle, Utah, began to move, and within days had blocked ...
The control of mesquite is a major range problem in the Southwest. Mesquite is a thorny, woody shrub...
What we do: Since 1892, the Iowa Geological and Water Survey (IGWS) has provided earth, water, and m...
Located on the western flank of the Boulder batholith of southwestern Montana, the mineralized brecc...
North Horn Mountain is part of a deeply dissected plateau in central Utah which is characterized by ...
The Grassy Butte area lies in southern McKenzie County, just southwest of the deepest part of the Wi...
In Utah all water, both on or below the ground surface, is considered public property. The right to ...
Salty soils are recognized as an ever increasing problem connected with irrigation agriculture. Mill...
The Fox Hills Formation in Emmons County, North Dakota, consists of 250-350 feet of medium to fine g...
In North Dakota the Pierre shale was deposited in all portions of the State except the southeastern ...
Lake County is in the extreme northwestern corner of Indiana. The county is divided into three physi...
This text is to be used in conjunction with Coal Resource Occurrence (CRO) and Coal Development Pote...
Since 1892, the Iowa Geological and Water Survey (IGWS) has provided earth, water, and mapping scien...
This text is to be used in conjunction with Coal Resource Occurrence (CRO) and Coal Development Pote...
Due to recent land use changes, runoff has greatly increased In Bowling Green, necessitating the dri...
In mid-April, 1983, an old landslide near Thistle, Utah, began to move, and within days had blocked ...
The control of mesquite is a major range problem in the Southwest. Mesquite is a thorny, woody shrub...
What we do: Since 1892, the Iowa Geological and Water Survey (IGWS) has provided earth, water, and m...
Located on the western flank of the Boulder batholith of southwestern Montana, the mineralized brecc...
North Horn Mountain is part of a deeply dissected plateau in central Utah which is characterized by ...
The Grassy Butte area lies in southern McKenzie County, just southwest of the deepest part of the Wi...
In Utah all water, both on or below the ground surface, is considered public property. The right to ...
Salty soils are recognized as an ever increasing problem connected with irrigation agriculture. Mill...
The Fox Hills Formation in Emmons County, North Dakota, consists of 250-350 feet of medium to fine g...
In North Dakota the Pierre shale was deposited in all portions of the State except the southeastern ...
Lake County is in the extreme northwestern corner of Indiana. The county is divided into three physi...
This text is to be used in conjunction with Coal Resource Occurrence (CRO) and Coal Development Pote...
Since 1892, the Iowa Geological and Water Survey (IGWS) has provided earth, water, and mapping scien...
This text is to be used in conjunction with Coal Resource Occurrence (CRO) and Coal Development Pote...
Due to recent land use changes, runoff has greatly increased In Bowling Green, necessitating the dri...
In mid-April, 1983, an old landslide near Thistle, Utah, began to move, and within days had blocked ...