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City of Rocks National Reserve: Cassia: 14,407 5,830: 5,720 1,740: 1988: Showcases granite spires and monoliths popular for rock climbing. Dworshak State Park: Clearwater: 850 340: 1,600 490: 1989: Comprises three properties on the shore of the reservoir created by the Dworshak Dam. Eagle Island State Park: Ada: 545 221: 2,724 830: 1983
U.S. Route 20, approximately 1 mile southwest of Island Park 44°20′41″N 111°27′39″W / 44.3447°N 111.4608°W / 44.3447; -111.4608 ( Island Park Land and Cattle Company Home Island Park
Granite Island Recreation Park is a protected area including all of Granite Island which is about 0.6 kilometres (0.37 miles) south-east of Victor Harbor in South Australia and about 120 kilometres (75 miles) south of Adelaide. It is reported as being 'the most visited park in South Australia'. [5]
The City of Rocks National Reserve, also known as the Silent City of Rocks, is a United States National Reserve and state park in south-central Idaho, approximately 2 miles (3.2 km) north of the border with Utah. It is widely known for its enormous granite rock formations and excellent rock climbing.
Atomic City: Butte: federal (Bureau of Land Management) A 2,500 ft Rhyolitic dome that rises over the Eastern Snake River Plain. It illustrates the scope and dimensions of Quaternary volcanism in the western United States. Big Springs: 1980
The Colorado state wildlife areas are managed for hunting, fishing, observation, management, and preservation of wildlife. The Colorado Parks and Wildlife division of the U.S. State of Colorado manages more than 300 state wildlife areas with a total area of more than 860 square miles (2,230 km 2 ) in the state.
Idaho Power 1967 Island Park Dam: Henrys Fork: Earthfill 94 29 Island Park Reservoir: 135,205 0.166773 0 USBR 1939 Little Camas Dam: Little Camas Creek: Earthfill 44 13 Little Camas Reservoir: 18,400 0.0227 0 Mountain Home Irrigation District 1912 Little Wood River Dam: Little Wood River: Earthfill 169 52 Little Wood River Reservoir: 33,300 0. ...
A specimen of stibnite. The Stibnite Mining District sits atop the Idaho Batholith, one of the signature features of Idaho’s unique geology.The Idaho Batholith is nearly 14,000 square miles (36,000 km 2) of granite, formed from the collision of the oceanic plate and the North American Plate around 100 million years ago during the Cretaceous period. [10]