Camas Prairie Ripples
Camas Prairie Ripples The Camas Prairie Ripples, located 12 miles north of Perma, Montana, appear as prominent ridges 15 to 50 feet high, 100 to 250 feet wide, and from
The Ice Age Floods National Geologic Trail covers some 16,000 square miles (41,440 km2) in present day Montana, Idaho, Washington, and Oregon. We have hand picked some of the best of the best places along the Trail and present them here for you enjoy and explore! Check back often, we will be adding new and wonderful destinations for your entire Family to enjoy!
Camas Prairie Ripples The Camas Prairie Ripples, located 12 miles north of Perma, Montana, appear as prominent ridges 15 to 50 feet high, 100 to 250 feet wide, and from
Travelers’ Rest State Park Ice Age Floods National Geologic Trail Located at an historic and contemporary crossroads, Travelers’ Rest State Park and National Historic Landmark is a place where visitors
An 8 ton erratic left behind by Glacial Lake Missoula in the Bitterroot Valley on the property of a local rancher was relocated to serve as the focal point of
Lake Pend Oreille Ice Age Floods National Geologic Trail The Purcell Lobe of the Cordilleran Ice Sheet repeatedly formed a 2000′ tall ice dam in this area, which backed up
Glacial Lobe Dam at Green Monarch Ridge View Point Ice Age Floods National Geologic Trail As the Purcell Trench ice lobe of the Cordilleran Ice Sheet advanced south from Canada,
Green Monarch Ridge Ice Age Floods National Geologic Trail THIS IS WHERE IT ALL BEGAN! The Green Monarch Ridge viewpoint, just south of the Hope Fault, is positioned along the edge
Frenchman Coulee Ice Age Floods National Geologic Trail Frenchman Coulee is a short drive north and west from the Silica Road exit 123 off US-90, along the Old Vantage Road. It is one of the most beautiful features left behind by the great Ice Age
The 50-mile-long Grand Coulee should be on everyone’s bucket list for a “must see” feature. The immense power of the forces that created the Coulee are apparent to those who read the evidence recorded in its rocks and landforms. How did the Coulee form? Why
Lewis and Clark Interpretive Center Ice Age Floods National Geologic Trail, Lewis & Clark National Historic Trail English fur trader John Meares was mistaken as he stood on the northern shore of the mouth of the Columbia River in July 1788. He was in search
Tualatin Ice Age Walking Trail Ice Age Floods National Geologic Trail The Tualatin Ice Age Trail is a self-guided tour of sites representing the ancient history of our area. Along the trail, you’ll discover evidence of centuries-old ice, rock and bone, including the sites where a mastodon
Hat Rock State Park Ice Age Floods National Geologic Trail, Lewis & Clark National Historic Trail Hat Rock is an erosion remnant warn way by floods from glaciers which melted over ten thousand years ago. Lewis and Clark saw this monument on their expedition and
Erratic Rock State Natural Site (Bellevue Erratic) Ice Age Floods National Geologic Trail Six miles west of McMinnville just off of Hwy 18 sits a 90-ton rock, the Bellevue Erratic, that was floated as much as 500 miles in an iceberg by way of the
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