Characteristics Of Granite Dome

Dome mountains are generally smaller than mountains formed by folds in the crust and have a different shape.

Characteristics of granite dome.

As granitic plutons cool kilometers below the earth s surface minerals in the rock crystallize under uniform confining. Soaring 4 788 feet 1 459 4 m above the valley the distinctive granite dome has been literally sheared in half by weathering erosion and earthquakes. There are seven intrusive suites in yosemite national park. Once the last glaciers retreated granite domes became exposed to the elements.

Granite domes are domical hills composed of granite with bare rock exposed over most of the surface. Granite is much harder than other rock and so it doesn t erode as easily as the rest of the mountain. It is the predominant mountain in this area with a smattering of picturesque lakes that provide both excellent camping and fishing opportunities. The softer layers of sedimentary rock were washed away leaving the hard granite dome.

Well known dome mountains include half dome in california which is a fully exposed granite dome formed by cooled magma. Dome shaped granite hills inselbergs such as the sugar loaf of rio de janeiro. Granite is an intrusive igneous rock which means it was formed in place during the cooling of molten rock generally the slower the molten rock cooled the larger it s mineral crystals with k feldspar megacrysts forming in special circumstances greater than 5cm. There are ample climbing routes for all technical abilities ranging from easy class ii scrambles to more technical.

The tuolumne intrusive suite is the youngest and most extensive occupying about 1 3 of the park s area. The tuolumne intrusive suite contains many famous rock types including the half dome granodiorite and cathedral peak granite. Half dome a granite monolith in yosemite national park and part of the sierra nevada batholith a batholith from greek bathos depth lithos rock is a large mass of intrusive igneous rock also called plutonic rock larger than 100 square kilometres 40 sq mi in area 1 that forms from cooled magma deep in the earth s crust. As plagioclase weathers easily tonalite areas are more deeply weathered than nearby granite areas.

Granite dome is a massive piece of granite in the heart of the emigrant wilderness. Weathering causes sheets of exposed rock to slip away and fall due to cracks or joints in the rock creating sheer faces like on the other side on half dome.