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The Green River Formation is an Eocene geologic formation that records the sedimentation in a group of intermountain lakes in three basins along the present-day Green River in Colorado, Wyoming, and Utah. The sediments are deposited in very fine layers, a dark layer during the growing season and a light-hue inorganic layer in the dry season.
The Flatirons are rock formations in the western United States, near Boulder, Colorado, consisting of flatirons.There are five large, numbered Flatirons ranging from north to south (First through Fifth, respectively) along the east slope of Green Mountain (elev. 8,148 ft or 2,484 m), and the term "The Flatirons" sometimes refers to these five alone.
The Green River Basin is the largest sub-basin in the GGRB area at 10,500 square miles. It is defined by multiple outcrops the most prominent being Oyster Ridge, a North to South angled hogback that exposes the Cretaceous Frontier Formation sandstone. The next outcrop is White Mountain containing Mid-Eocene exposure.
Green Mountain National Forest is a national forest located in Vermont, a temperate broadleaf and mixed forest typical of the New England/Acadian forests ecoregion. The forest supports a variety of wildlife, including beaver , moose , coyote , black bear , white-tailed deer , wild turkey , and ruffed grouse .
1]: Length: 730 mi (1,170 km): Basin size: 48,100 sq mi (125,000 km 2): Discharge: : • location: Green River, Utah [2]: • average: 6,121 cu ft/s (173.3 m 3 /s) [2]: • minimum: 380 cu ft/s (11 m 3 /s): • maximum: 68,100 cu ft/s (1,930 m 3 /s): Basin features; Tributaries: : • left: Blacks Fork, Henrys Fork, Duchesne River, Price River, San Rafael River: • right: New Fork River, Big ...
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The Green Mountain Dam was built between 1938 and 1943 by the United States Bureau of Reclamation. The reservoir and its dam store water to benefit Colorado's Western Slope. Created by President Roosevelt as part of the Colorado-Big Thompson Project in 1937, Green Mountain was the first
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