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The Williston Basin is a large intracratonic sedimentary basin in eastern Montana, western North Dakota, South Dakota, southern Saskatchewan, and south-western Manitoba that is known for its rich deposits of petroleum and potash. The basin is a geologic structural basin but not a topographic depression; it is transected by the Missouri River ...
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The Bakken Formation (/ ˈ b ɑː k ən / BAH-kən) is a rock unit from the Late Devonian to Early Mississippian age occupying about 200,000 square miles (520,000 km 2) of the subsurface of the Williston Basin, underlying parts of Montana, North Dakota, Saskatchewan and Manitoba. The formation was initially described by geologist J. W ...
It is not clear who was the first European explorer to enter the Goose Lake Valley. A map of the Oregon Country prepared by United States Army Corps of Topographical Engineers in 1832 shows Pit Lake with a hot springs north of the lake. Given the lake's location on the map, it is clearly Goose Lake, and the hot springs are Hunter's Hot Springs.
The Pacific Basin is bounded by the Continental divide to the east and Pacific Ocean to the west; the basin excludes the endorheic Great Basin in the west. The Great Basin has a closed loop boundary encompassing substantially all of Nevada, the western half of Utah and parts of Oregon, California, Idaho, and Wyoming.
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