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.
Characteristics of granite dome.
Tonalite is a granite like rock of plutonic origin and usually has plagioclase as the sole feldspar.
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.
Despite the name most of the dome actually remains and it was originally formed as a narrow wedge shaped dome.
Dome mountains are generally smaller than mountains formed by folds in the crust and have a different shape.
As plagioclase weathers easily tonalite areas are more deeply weathered than nearby granite areas.
Dome shaped granite hills inselbergs such as the sugar loaf of rio de janeiro.
Granite dome is a massive piece of granite in the heart of the emigrant wilderness.
The softer layers of sedimentary rock were washed away leaving the hard granite dome.
Generally domical features such as these are known as bornhardts bornhardts can form in any type of plutonic rock but are typically composed of granite and granitic gneiss.
Granite domes are domical hills composed of granite with bare rock exposed over most of the surface.
Once the last glaciers retreated granite domes became exposed to the elements.
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.
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.
The tuolumne intrusive suite is the youngest and most extensive occupying about 1 3 of the park s area.
As granitic plutons cool kilometers below the earth s surface minerals in the rock crystallize under uniform confining.
It is the predominant mountain in this area with a smattering of picturesque lakes that provide both excellent camping and fishing opportunities.
There are ample climbing routes for all technical abilities ranging from easy class ii scrambles to more technical.
The tuolumne intrusive suite contains many famous rock types including the half dome granodiorite and cathedral peak granite.
