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Elk River Destination Guide
Explore Elk River in United States
Elk River in the region of Idaho with its 125 inhabitants is a place in United States - some 2,034 mi or ( 3273 km ) West of Washington , the country's capital city .
Time in Elk River is now 05:22 AM (Tuesday) . The local timezone is named " America/Los Angeles " with a UTC offset of -7 hours. Depending on your budget, these more prominent locations might be interesting for you: Boise, Dent, Five Corners, Grangeville, and Lewiston. Since you are here already, consider visiting Boise . We saw some hobby film on the internet . Scroll down to see the most favourite one or select the video collection in the navigation. Where to go and what to see in Elk River ? We have collected some references on our attractions page.
Videos
289 Shattuck Ridge Rd Elk River ID 83827
View full virtual tour: www.justsnooping.com ..
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Interesting facts about this location
Elk River, Idaho
Elk River is a city in Clearwater County, Idaho, United States. The population was 125 at the 2010 census, down from 156 in 2000. It is accessed from State Highway 8 from Bovill, to the west in adjacent Latah County. Elk River was formerly the site of a Potlatch sawmill, phased out after several decades during the 1930s.
Located at 46.78 -116.18 (Lat./Long.); Less than 0 km away
Bovill, Idaho
Bovill is a city in Latah County, Idaho, United States. The population was 260 at the 2010 census, down from 305 in 2000.
Located at 46.86 -116.39 (Lat./Long.); Less than 18 km away
Dent Bridge
The Dent Bridge is a suspension bridge located near Orofino, Idaho, United States. It is located 17 miles up the North Fork of the former Clearwater River, now the Dworshak Reservoir. Completed in 1971, the bridge has a main span of 1,550 feet .
Located at 46.60 -116.18 (Lat./Long.); Less than 20 km away
Clarkia fossil beds
The Clarkia fossil beds (also known locally as the Fossil Bowl) is a Miocene lagerstätte near Clarkia, Idaho. The fossil beds were laid down in a lake roughly 15-million-years ago, when a drainage basin was dammed by the flood basalts of the Columbia River Plateau. Narrow and deep, the lake's cold, anoxic water and rapid sedimentation created perfect fossil conditions. The basin itself has remained tectonically stable, with little deformation since then.
Located at 46.99 -116.28 (Lat./Long.); Less than 24 km away
Related Locations
Information of geographic nature is based on public data provided by geonames.org, CIA world facts book, Unesco, DBpedia and wikipedia. Weather is based on NOAA GFS.