Search results
Results from the WOW.Com Content Network
Geology of Table Mountain in relation to the geology of the rest of the Cape Peninsula. The upper approximately 600-metre (2,000 ft) portion of the one-kilometre-high (0.62 mi) table-topped mountain, or mesa, consists of 450- to 510-million-year-old rocks belonging to the two lowermost layers of the Cape Fold Mountains.
Table Mountain is northwest of Chaos Crags and Lassen Peak, southeast of Red Lake Mountain, Red Mountain, Eskimo Hill, and Latour Butte, and west of Prospect Peak. [ 1 ] Geology
Within the region of Table Mountain, the Table Mountain Latite is mapped as a part of the Mehrten Formation. Further north, it is considered part of a sequence of volcanic strata known as the Stanislaus Group. [4] [5] The Table Mountain Latite consists of high-potassium trachyandesite lavas. During the Pliocene, circa 10.4 Ma, these lavas were ...
Table Mountain seen from Signal Hill, across the Cape Town city bowl. The portion of the mountain made up of Table Mountain Sandstone is indicated on the right. [1] It is this mountain that has given its name to the geological structure that occurs in the mountains throughout the Western Cape Schematic diagram of an approximate 100 km west-east (left to right) geological cross-section through ...
Lupine field on Table Mountain. Table Mountain is most famous for its vast array of wildflowers, which bloom during spring time. The bloom usually lasts from the last two weeks of March, to the first two weeks of April. The flower bloom is the most popular attraction on Table Mountain.
Table Mountain is set in Yellowstone National Park and ranks as the third-highest peak in the park. [2] The mountain is located eight miles (13 km) southeast of Yellowstone Lake, and 2.18 miles (3.51 km) southwest of Eagle Peak which is the nearest higher peak, [5] as well as the park's highest point.
Between 1425 and 1450 AD the south side of Table Mountain sheared off and dammed the Columbia River in an event known as the Bonneville Slide. [4] The river soon carved a new bend around to the south, but for a while Native Americans living in the area could walk across. This led to the legend known as the Bridge of the Gods. [5]
A tableland is an area containing elevated landforms characterized by a distinct, flat, nearly level, or gently undulating surface. They often exhibit steep, cliff-like edges, known as escarpments, that separate them from surrounding lowlands.