Ads
related to: basalt idahohometogo.com has been visited by 100K+ users in the past month
Ready to take vacation rental metasearch global - Tnooz
Search results
Results from the WOW.Com Content Network
As of the census [3] of 2010, there were 394 people, 132 households, and 108 families residing in the city. The population density was 1,313.3 inhabitants per square mile (507.1/km 2).
The Columbia River Basalt Group (including the Steen and Picture Gorge basalts) extends over portions of four states. The Columbia River Basalt Group (CRBG) is the youngest, smallest and one of the best-preserved continental flood basalt provinces on Earth, covering over 210,000 km 2 (81,000 sq mi) mainly eastern Oregon and Washington, western Idaho, and part of northern Nevada. [1]
The Snake River Plain is a geologic feature located primarily within the U.S. state of Idaho. It stretches about 400 miles (640 km) westward from northwest of the state of Wyoming to the Idaho-Oregon border. The plain is a wide, flat bow-shaped depression and covers about a quarter of Idaho.
The historic district is named for Map Rock, [2] a massive basalt rock covered in petroglyphs, named by Robert Limbert in the early 1920s. Limbert believed that the rock depicts a map of the Snake River valley, and some authors have suggested that if it is a map then it may be the oldest map in the world.
The dam site is composed of basalt and rhyolite, both of which are considered unsuitable for dam construction [citation needed] because of their high permeability. This was confirmed by long-term pump-in tests at rates of 165 to 460 US gal (620 to 1,740 L) per minute. [ 11 ]
The Columbia Plateau is an important geologic and geographic region that lies across parts of the U.S. states of Washington, Oregon, and Idaho. [1] It is a wide flood basalt plateau between the Cascade Range and the Rocky Mountains , cut through by the Columbia River .
The search engine that helps you find exactly what you're looking for. Find the most relevant information, video, images, and answers from all across the Web.
The Sinker Creek Zeolite Occurrence is in southern Idaho. [8] It is known for producing calcite, chabazite, nontronite, phillipsite, and thomsonite. [9] The minerals occur in Late Pleistocene age basalt in a road cut by milepost 35 on Route 78. [9] [10]