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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]
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.
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.
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Salt Creek washed out 25 miles (40 km) of Oregon Route 58 and undermined the SP viaduct footings. Landslides covered 700 feet (210 m) of SP track near Oakridge, and swept away 130 feet (40 m) of the Noisy Creek bridge 20 miles (32 km) north of Crescent Lake. The Willamette River washed out 300 feet (91 m) of SP track between Portland and Albany.
Barr Creek Falls in southern Oregon Benham Falls on the Deschutes River Kayaker heading over Bridal Veil Falls on Bridal Veil Creek in the Columbia Gorge Clearwater Falls on the Clearwater River in Douglas County Diamond Creek Falls Fairy Falls on Wahkeena Creek in the Columbia River Gorge Upper Horsetail Falls, also in the gorge Ki-a-Kuts Falls on the Tualatin River Latourell Falls in the ...
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The press call occurred as U.S. government agencies held a separate, classified briefing for all senators on Salt Typhoon's efforts to compromise American telecommunications companies.