Badger Mountain (Benton County, Washington) Explained

Badger Mountain
Photo Size:300
Elevation Ft:1593
Elevation Ref:[1]
Prominence Ft:915
Isolation Mi:8.44
Range:Columbia River Plateau
Country:United States
State:Washington
Subdivision2 Type:County
Subdivision2:Benton County
Settlement Type:City
Settlement:Richland
Map:USA Washington
Map Size:200
Label Position:right
Coordinates:46.2343°N -119.3215°W
Topo:USGS Badger Mountain
Easiest Route:Hike
Fetchwikidata:ALL

Badger Mountain is a small mountain in Richland, Washington. Badger rises above the Tri-Cities connected to the smaller Candy Mountain via Goose Gap, is visible throughout much of the area and is a popular hiking destination for a wide variety of climbers. There are a number of trails climbing the mountain with varying levels of difficulty. There are two summits on Badger Mountain, named the East Summit and the West Summit. The West Summit is the highest.

Most of Badger Mountain is protected by the Badger Mountain Centennial Preserve, but the radio towers at the peak are private property.[2] A non-profit group, Friends of Badger Mountain,[3] worked to procure this shrub-steppe area that has most native vegetation intact and then built a trail to the summit. The 1.2miles trail rises 984feet above the trail head in Richland.

Geology

Badger Mountain is a member of the Yakima Fold Belt, a series of topographical folds (or wrinkles) raised from tectonic compression. The Yakima Fold Belt extends from Interstate 90 near Vantage, Washington to the Columbia River near Wallula, Washington. The Yakima Fold Belt is a portion of the larger Olympic–Wallowa Lineament, which extends from near Port Angeles, Washington into northeastern Oregon.[4]

Badger Mountain is also a part of the Columbia River Basalt Group. Sometime between 10 and 15 million years ago, multiple lava flows poured out from the Yellowstone hotspot, then located in western Idaho. These lava flows covered large portions of Washington and Oregon on their way to the Pacific Ocean and are the cause of the underlying basalt of the region. In some areas, the basalt was 5900feet thick.[5]

During the time of the last ice age, glaciers extended into northern Washington, Idaho and Montana. This blocked the Clark Fork River creating Glacial Lake Missoula. Periodically during the ice age, the weight of the water behind the ice dam caused it to break creating the Missoula Floods. As these floods rushed toward the Pacific Ocean they carried glacial erratics, chunks of granite not typically found in eastern Washington. The surface elevation of the flood water reached 1250feet above sea level at Badger Mountain, making it into an island for a short time. Glacial erratics of various sizes can be seen up to this elevation on the mountain and there is a marker along the Canyon Trail at 1250 feet above sea level.[6]

Recreation

There are two trails leading to the peak of the mountain, with three other trails on the slopes of the mountain. Badger Mountain is a popular location for hiking and photography because of its height above the Tri-Cities and the views it gives. On a clear day from the peak one can see Rattlesnake Mountain, and the Blue Mountains as well as major Cascade Mountains such as Mount Hood, Mount Adams,[7] Mount Rainier and Mount Stuart.[8]

In 2010 more than 71,000 people visited the mountain.[9]

Hiking

The Canyon and Skyline Trails reach the peak. The Canyon Trail is 1.3miles long and starts at Trailhead Park. The Canyon Trail only allows hikers. The Skyline Trail is 2.9miles long and starts off of Dallas Road on the northwest side of Badger. The Skyline Trail goes along the spine of Badger Mountain and is open to hiking, mountain biking and horseback riding.

The Langdon, Sagebrush and Badger Flats Trails do not reach the peak. The Sagebrush Trail is a spur off of the Skyline Trail, connecting it to Trailhead Park. The Langdon Trail wraps around the south side of the mountain, offering views of Badger Canyon and the Horse Heaven Hills. It is open to hikers, mountain bikers and horseback riders. The Badger Flats Trail is completely within Trailhead Park and is 0.6miles in length.[2]

Climate and wildlife

Badger Mountain lies in the rain shadow of the Cascade Mountains and as such has a semi-arid climate with mild winters and hot summers. The average rainfall at the nearest airport is 7.94inches per year and temperatures above 100F are not uncommon.[10] Because of this, Badger Mountain shares much of the same wildlife as the surrounding area including sagebrush, jackrabbits and rattlesnakes. There are no naturally occurring trees on the mountain.

Winter snows are also not uncommon.

See also

External links

Notes and References

  1. 31 May 2015.
  2. Web site: Trails & Directions. friendsofbadger.org. 14 July 2015.
  3. http://www.friendsofbadger.org/ Friends of Badger Mountain
  4. Field Trip Guide to the Columbia River Basalt Group. May 2005. Pacific Northwest National Laboratory. 31 May 2015.
  5. Book: Bishop, Ellen Morris. 2003. In Search of Ancient Oregon: A Geological and Natural History. Portland, Oregon. Timber Press. 978-0-88192-789-4.
  6. Allen, John Eliot; Burns, Marjorie and Sargent, Sam C. (c. 1986). Cataclysms on the Columbia : a layman's guide to the features produced by the catastrophic Bretz floods in the Pacific Northwest. Portland, OR: Timber Press. p. 104. .
  7. https://www.facebook.com/photo.php?fbid=10205429411527758&set=pb.1624120700.-2207520000.1433102538.&type=3 Picture: Mount Adams from Badger Mountain
  8. http://www.heywhatsthat.com/?view=LGLAFMGJ HeyWhatsThat Badger Mountain
  9. http://friendsofbadger.org/photo-gallery/ Photo Gallery - Traveler Stats
  10. Web site: Monthly Temperature Charts, Pasco, WA. NOAA. 31 May 2015.