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Cascadia Cave is nearby. The cave is an 8,000-year-old American Indian petroglyph site considered to have the largest concentration of rock engravings in western Oregon. [3] Willamette Valley settlers developed a bypass at the park site for horse-drawn wagons. Old wagon ruts are still visible near where Soda Creek meets the South Santiam River. [2]
The Cascadia subduction zone is a 960 km (600 mi) fault at a convergent plate boundary, about 100–200 km (70–100 mi) off the Pacific coast, that stretches from northern Vancouver Island in Canada to Northern California in the United States
Jun. 21—Making maps, hiking, exploring the geology around them and making a seismometer are among the things kids in University of Texas Permian Basin's Geology Camp have learned about this week.
[1] [2] The stated mission of the center [3] is to (i) carry out basic and applied science research on earthquake hazards at the Cascadia Subduction Zone, (ii) promote access to careers in the geosciences, especially amongst minoritized individuals, and (iii) form partnerships between researchers and organizations in charge of response and ...
On the academic side, there are engineering camps, biology camps, Makerspace camps, geology camp and more. The biology camp is for kids 12 to 18 and will be from 9 a.m. to 3 p.m. June 24-27.
The name "Cascadia" was first applied to the whole geologic region by Bates McKee in his 1972 geology textbook Cascadia; the geologic evolution of the Pacific Northwest. Later the name was adopted by David McCloskey, a Seattle University sociology professor, to describe it as a bioregion. McCloskey describes Cascadia as "a land of falling waters."
Malibu Canyon, Santa Monica Mountains. The Pacific Coast Ranges (officially gazetted as the Pacific Mountain System [1] in the United States; French: chaînes côtières du Pacifique; Spanish: cadena costera del Pacífico) [2] are the series of mountain ranges that stretch along the West Coast of North America from Alaska south to Northern and Central Mexico.
Stumps of trees at the Neskowin Ghost Forest. The Neskowin Ghost Forest is the remnants of a Sitka spruce forest on the Oregon Coast of the United States. The stumps were likely created when an earthquake of the Cascadia subduction zone abruptly lowered the trees, that were then covered by mud from landslides or debris from a tsunami. [1]