WebOkotoks, Alberta 1-403-362-4451. Website. Share. Add to Wishlist Print. Overview. The Okotoks Erratic is the largest known rock in the Foothills Erratics Train, a group of rocks that were carried by ice along the mountain front and let down as the glacier melted more than 10,000 years ago. The erratics lie in a narrow band extending from Jasper ... WebFeb 17, 2015 · About 7 km west of the town of Okotoks in Alberta, in Canada, on the flat prairie lies a massive piece of rock 41 meters long, 18 meters wide and 9 meters high, and weighs 16,500 tons. It’s a glacial erratic - a rock transported far from its place of origin by glacial ice thousands of years ago. The Okotoks Erratic, also known as “the Big ...
Okotoks Erratic: In-Depth CyArk
http://dictionary.sensagent.com/Glacial%20erratic/en-en/ WebMovement of some glacial erratics in southern Alberta. The Foothills Erratics Train (Stalker 1956) is shown along A-B (from Klassen 1989, p.144). Source publication +8 Geology of the Frank... therapeutic pictures
Geology: Cosmogenic 36 Cl dating of the Foothills erratics …
WebTopic: Geology, palaeontology, and natural history of the Alberta badlands Theme: Unlocking the secrets of the canadian Badlands proGrAm DescripTion: rocks that come alive and the mysterious popcorn rock are just a few of the wonders ... The glacial erratics are igneous and metamorphic rocks. Formed in the canadian shield and the rocky WebErratics can range in size from pebbles to large boulders such as Big Rock (15,000 metric tons / 17,000 short tons) in Alberta. Geologists identify erratics by studying the rocks surrounding the position of the erratic and the composition of the erratic itself. Erratics are significant because: WebThe Foothills erratics train (FET) of Alberta is comprised of hundreds of angular quartzite boulders ranging from <1 m to the Big Rock near Okotoks with an estimated mass of … signs of height growth