* WHAT...Flooding caused by excessive rainfall continues to be possible. * WHERE...Portions of Oregon, including the following areas, Benton County Lowlands, Cascade Foothills of Marion and Linn Counties, Cascades of Lane County, Cascades of Marion and Linn Counties, Central Coast of Oregon, Central Columbia River Gorge I-84 Corridor, Central Oregon Coast Range, Central Oregon Coast Range Lowlands, Clackamas County Cascade Foothills, Clatsop County Coast, East Central Willamette Valley, East Portland Metro, Inner Portland Metro, Lane County Cascade Foothills, Lane County Lowlands, Linn County Lowlands, Lower Columbia River, North Oregon Cascades, North Oregon Coast Range, North Oregon Coast Range Lowlands, Outer Southeast Portland Metro, Portland West Hills and Chehalem Mountain, Tillamook County Coast, Tualatin Valley, Upper Hood River Valley, West Central Willamette Valley, West Columbia River Gorge I-84 Corridor and West Columbia River Gorge of Oregon above 500 ft and southwest Washington, including the following areas, Central Columbia River Gorge SR 14 Corridor, Cowlitz County Lowlands, East Clark County Lowlands, Inner Vancouver Metro, North Clark County Lowlands, South Washington Cascade Foothills, South Washington Cascades, South Washington Coast, West Columbia River Gorge SR 14 Corridor, Willapa Hills and Willapa and Wahkiakum Lowlands. * WHEN...Through Saturday afternoon. * IMPACTS...Creeks and streams may rise out of their banks. Flooding may occur in poor drainage and urban areas. Area creeks and streams are running high and could flood with more rain. * ADDITIONAL DETAILS... - Flood potential remains high today even though much less rain is forecast. Many area rivers and streams are rising this morning, and slow responding rivers could see rises into Saturday afternoon. With the saturated soils and high rivers and creeks, any additional rain will slow receding of the water and continue the potential for flooding. - http://www.weather.gov/safety/flood
It spans a substantial area, with a length of about 3 miles and a width of 1.5 miles. This impressive mountain offers a range of mountaineering opportunities for enthusiasts seeking a challenging adventure.
During the winter season, Sand Mountain experiences a diverse snowpack range, varying from year to year. Snow accumulations can reach significant depths, with an average snowpack depth of around 8 to 12 feet. This makes it an attractive destination for winter sports enthusiasts, such as snowshoers and backcountry skiers.
As for water runoff, Sand Mountain contributes to the flow of several creeks and rivers in the surrounding area. These waterways include the Sandy River, which receives runoff from melting snow and glaciers on the mountain. The Sandy River is renowned for its scenic beauty and is a popular destination for fishing, kayaking, and rafting.
The origins of the name "Sand Mountain" are not definitively known, but there are a few interesting theories and legends associated with it. Some believe that the name reflects the sandy nature of the slopes on the mountain, while others suggest it may have been named after an early settler or explorer with the surname Sand. Regardless of its origins, Sand Mountain remains an iconic and alluring destination for mountaineers and outdoor enthusiasts alike.