San Francisco Peaks Research Paper Example | Topics and Well Written Essays - 1000 words

San Francisco vizors - Research Paper poserHowever this entire mystery was resolved in 1980 when Mount St. Helens erupted. It is because of this erosion that the scientists and geologists were able to sorting out that due to volcanoes a mountains entire face can disappear. Further, with the help of the geologicalal testing and feeler photos it was concluded that the San Francisco Peaks experience the same kind of erosion and that is why it took a unique formation. It is believed by the geologists that the authentic bankers bills were more than 16,000 feet high (San Francisco Peaks) The Peaks The San Francisco Peaks atomic number 18 located to the north of Flagstaff, Arizona and has a height of about 12,633 feet. It is considered to be the most distinct geological mark of the Colorado tableland. These peaks set about been named after the settler in the role the early 1620s named St. Francis of Assisi, however in the local area these are referred to as Peaks. The peaks are a embodied formation of six summits that encircle the volcanic crater, which is now a quiet volcano. Out of all the six, the highest peak in Arizona is Humphreys Peak that is 12,633 feet high, Agassiz Peak is about 12,356 feet and the Fremont Peak soars up to 11,969 feet. The remaining three peaks Aubineau Peak, Reese Peak and the Doyle Peak climb up to 11,838 feet, 11,474 feet and 11,460 feet respectively. Together all these peaks make a circular ring qualification the peaks the most significant geological display of volcanic rocks, together with the picturesque view of the lava flows and the deep alpine forest. As the peaks are a unique formation, they provide a dramatic landscape of the Flagstaff that is isolated, great and quite unexpected. Since the peaks are quite tower-like, these can be viewed from quite a distance even from the Wupatki theme Monuments (Priest, Duffield and Malis-Clark). Today these peaks dumbfound become tourist attractions as millions of people visit th is place every year. The Peaks have a protected alpine environment (Inner Basin), a ski resort (Arizona Snowbowl) and the Humphreys Peak (the highest point of Arizona). populate visit the place for hiking, wildlife viewing, camping, and skiing and wilderness seclusion. The Formation of the Peaks Arizonas volcanic pleasures begin to form about 6 million years ago when there were 600 volcanic eruptions in the region. It was due to these volcanic eruptions that the Peaks were formed, mainly the Humphreys peak that soared above the terrain making it a geological landscape, otherwise it would just have been a dry and arid plateau. Although the history of the formation of the Peaks varies in the region however the general geologic history remains quite the same. Nearly about 500 million years ago the Plateau region was below or at the sea levels and the sediments of limestone began to accumulate underneath. Although most of the volcanic eruptions are ripe the tectonic plates in the eart hs crust however Arizona has been quite far from the North American Plate. The causal agency of volcanic eruptions in this region is believed to be the molten rock that is the trapped area beneath the northern Arizona named as the hot spot. This molten rock occasionally rises, moving the plate to the west and creating volcanoes. The Peaks are believed to be formed nearly 500,000 to 1 million years ago however its inner toilet has been quite since its formation (Jones). Many geologists name this formation of the San Francisco Peaks as a stratovolcano meaning that it