Geology and groundwater resources of the Peace River district, northwestern Alberta
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Geology and groundwater resources of the Peace River district, northwestern Alberta by John Frederick Jones

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Published by Queen"s Printer in Edmonton .
Written in English

Subjects:

Places:

  • Alberta,
  • Peace River district.

Subjects:

  • Hydrology -- Alberta -- Peace River district.,
  • Geology -- Alberta -- Peace River district.,
  • Water-supply -- Alberta -- Peace River district.

Book details:

Edition Notes

Bibliography: p. 125-130.

Statementby J. F. Jones.
Classifications
LC ClassificationsQ180.C2 R34 no. 16
The Physical Object
Pagination143 p. In portfolio with 7 fold. illus. and 6 fold. maps (part col.)
Number of Pages143
ID Numbers
Open LibraryOL4967779M
LC Control Number76457805

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Water well records constitute the basic data in any groundwater exploration program and the compilation herein presented is intended as a fundamental aid in the development of the groundwater resources of the Peace River District of northwestern Alberta. The Peace River is a river in Canada that originates in the Rocky Mountains of northern British Columbia and flows to the northeast through northern Alberta. The Peace River flows into the Slave River, a tributary of the Mackenzie River. The Mackenzie is the 12th longest river in the world, preceded by the Mekong and followed by the Niger River. Peace River Geology Report The Alberta Energy Regulator ensures the safe, efficient, orderly, and environmentally responsible development of hydrocarbon resources over their entire life cycle. This includes allocating and conserving water resources, managing public lands, and protecting the environment while providing. The Peace River Formation is a stratigraphical unit of middle Albian age in the Western Canadian Sedimentary Basin.. It takes the name from the Peace River, and was first described on the banks of the river, downstream from the Smoky River confluence to the mouth of Coordinates: 56°12′N °20′W / .

The Kern River alluvial fan is the southernmost major alluvial fan built by the streams which drain the west side of the Sierra Nevada. The climate is semiarid with rainfall near 5 inches per year. Agricultural development within the area uses over half the , acre-feet per year flow of the Kern River, plus a considerable amount drawn from the ground-water reservoir particularly during. Author(s) Water Resources Program: Description: Geology and ground-water resources of northwestern King County, Washington. Water Supply Bulletin 20 () describes an investigation into the occurrence, quantity and quality of ground water supplies in northwestern King County. EG GS: EGN c.3 (X^JL^uu^-j Hydrogeologyofthe GreenRiverLowlandand AssociatedBedrockValleys inNorthwesternIllinois eth YunxiaXu on EnvironmentalGeology DepartmentofNaturalResources ILLINOISSTATEGEOLOGICALSURVEY ¥too«DV APR Author: David R. Larson, Beverly L. Herzog, Robert C. Vaiden, Cheri A. Chenoweth, Yunxia Xu, Richard C. Ande. Peace River, originally named Peace River Crossing, and known as Rivière-la-Paix in French, is a town in northwestern Alberta, Canada, situated along the banks of the Peace River, at its confluence with the Smoky River, the Heart River and Pat's is located kilometres ( mi) northwest of Edmonton, and kilometres ( mi) northeast of Grande Prairie, along Highway d sortation area: T8S.

reports on the geology and groundwater resources of North Dakota. The main purposes of these studies are: (1) to provide a geologic map of the area, (2) to locate and define aquifers, (3) to determine the location and extent of mineral resources in the counties, and (4) File Size: 9MB. This banner text can have markup.. web; books; video; audio; software; images; Toggle navigation. Don River Watershed Plan: Geology and Groundwater Resources – Report on Current Conditions Toronto and Region Conservation CFN: 5 wider study, include the compilation of a database of water related information (boreholes, wells, climate, streamflow, etc), refinement of the three dimensional stratigraphy provided by. Williams County, in northwestern North Dakota, is located near the center of the structural and sedimentary Williston basin. The preglacial sedimentary formations beneath the county are as much as 14, feet thick. Their beds dip generally to the south except along the flanks of the north-south striking Nesson anticline in the eastern part of the county.