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Salt Creek Falls was formed when glaciers receded during the last glacial period, and water from newly formed lakes upstream carved a valley through the forest.A main glacier in the Salt Creek valley seems to have deepened this canyon well below the level of the stream's tributaries, leaving those side valleys towering high above the bed of Salt Creek. [5]
Below the falls, the creek enters a narrow canyon shaped by glaciation and basaltic lava flows from higher in the Cascades. [9] [12] McCredie Hot Springs, at the former community of McCredie Springs, are natural hot springs along the lower half of Salt Creek beside Route 58. [13] [14] The Salt Creek watershed is a temperate coniferous forest.
The classic option is an easy 1.5 to 2-mile out-and-back snowshoe trek to 286-foot Salt Creek Falls, a breathtaking sight in winter that looks its best after a nice low-elevation snow. From the ...
At 272-feet, Watson is typically considered the third-tallest frequently visited waterfall after Multnomah and Salt Creek falls. The difference is unlike those two, which are major tourist stops ...
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.
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The Salt Creek Tunnel. Oregon Route 58 is of high importance as a freight corridor. It is the primary route between the Willamette Valley and south-central Oregon, including the Klamath Falls region. It also is the preferred route to points further southeast, including Reno, Nevada.
A stunning new bridge has been installed to provide safer access to Diamond Creek Falls, a 120-foot cascade southeast of Oakridge.