๐จ Late on July 30, 2024, the land along the southern bank of the#ChilcotinRiver in Farwell Canyon, British Columbia, #Canada, began to subside and flow into the valley below. The landslide formed a debris mound that stretched 1,000 meters in length and 600 meters in width. This obstructed the river, completely stopping its flow.
The multitemporal #Sentinel-1 composite below combines three images from different dates to reveal the dramatic changes in the landscape. [๐งต 1/3]