The Valley of the Alimbics

In Galaxy Federal Medical Frigate Atonement, Samus Alan is in a dormant state, but still she can not tolerate Anadyr V's injury. A laser explosion from a Crimson Hunter fighter has severely damaged her clothes and must be removed when repairing. While the medical staff were working on her lawsuit, Brigstone stood at the observation area of ​​the medical facility and saw Sams. When Sams was absent, Vision cleared her heart. Within seconds, she learned that she was a ghost in a big cave.

In Death Valley there lived an Indian Timbisha, who was in the valley for at least the past 1000 years. Timbisha means "rock paint" and is the name of the valley, tümpisa, which means the red ocher color paint that can be made from clay in the valley. Some families still live in the valley of the furnace creek. Another village is in the Grapevine Valley near the present Scotty Castle. It is called the Timbisha language maahunu and its meaning is uncertain, well-known, but hnu means "canyon"

Direction Very deep river valley may be called a canyon or canyon. The terms U and V are geological descriptive terms used to characterize valley shapes. Most valleys belong to one of these two main types, or to a mixture (at least) of them, for the cross section of the slope or slope of the hill. The valley of the most extensive geographical meaning is also called a valley. The valley through which a river passes is also called a valley. A small, hidden, tree-lined valley is known as Dell or is known as a Scottish canyon. A wide and flat valley through the river known as the Scottish canyon

The overhanging valley is a valley of a tributary, and there is a higher undulation on the ground than the main passage through which it flows. When tributary glaciers flow into larger glaciers, they are most often associated with U-shaped valleys. Major glaciers erode deep U-shaped valleys with nearly vertical sides. On the other hand, small tributary glaciers form shallower U-shaped valleys. Since the glacial surface was initially at the same height, the shallower valleys appeared to "hang" over the main valley. Normally a waterfall is formed at or near the exit of the upper valley. The valley of the cliff is also a product of different erosion rates in the main valley and tributary valley.