Geology of Mt Everest

Geology of Mt Everest

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Geology of Mt Everest – The Himalayan range, excess by 29,036 feet (8, 850 meter) Mount Everest, the most important point one invoke in the world, is one of the largest and most different geographic positions on the earth’s surface. The string, navigating northwest to southeast, elongates 1,400 miles (2,300 kilometers ) vary 140 miles and 200 miles wide ranging spans or abuts five countries India, Nepal, Pakistan, and Peoples Republic of China is the mother of three major rivers Indus, Ganges, and Tsampo Bramhaputra creeks and boasts over 100 ridges higher than 23,600 feet (7,200 lilts) all higher than any ridges on the other six continents.

Himalayas Created By The Collision Of 2 Plates

The Himalayas and Mount Everest are youth geologically pronouncing. They originated constituting over 65 million years ago when two of the earth’s great crustal plates the Eurasian plateful and the Indo Australian plate collided. The Indian sub continent steamed northeastward, flinging into Asia, folding and propagandizing the plate pieces, and steadily jostle the Himalayas over five miles high pitched. The Indian plateful, is change about 1.7 inches a year, is being gradually propagandized under or subducted by the Eurasian plateful, which obstinately refuses to move, moving the Himalayas and the Tibetan Plateau to rise from 5 to 10 millimeters a year. Geologists estimates that India will continue moving northward for almost a thousand miles in the course of the landing 10 million years.

Light Rocks Are Pushed Up As High Peaks

Heavier rock is pushed back down into the earth’s drapery at the point of contact, but lighter face, like limestone and sandstone is propagandized upward to form the lofty ridges.

At the combs of higher surfaces, like Mount Everest, it is possible to find 400 million year old fogies of ocean flavors and straws” thats been” situated at the bottoms of shallow muggy oceans. Now they are disclosed on the ceiling of the world, over 25,000 feet above sea level.

Summit Of Mt. Everest Is Marine Limestone

The massive sort reporter John McPhee wrote about Mount Everest in his subject Basin and Range : When the climbers in 1953 embed their signals on the most important point one invoke, they specify them in snow over the skeletons of flavors that had lived in the hot clear ocean that India, moving north, blanked out.

Possibly as much as twenty thousand hoofs below the seafloor, the skeletal stands had turned into face. This one actuality is a essay in itself on the movements of the surface of the earth. If by some fiat I had to restrict all this writing to one convict, this is the one I would choose : The slake of Mt. Everest is naval limestone.

Mount Everest’s Geology Is Simple

The geology of Mount Everest is very simple. The raising was a great slice of solidified sediments that once lay at the bottom of the Tethys Sea, an open waterway that exists among the Indian sub continent and Asia over 400 million years ago. The sedimentary rock was somewhat metamorphosed from its original deposition and then heightened upward at an amazingly immediate rate as much as 4.5 inches (10 centimeters) a year as the Himalayas rose.

Sedimentary Layers Form Most Of Everest

The sedimentary rock membranes can be obtained from Mount Everest are limestone, marble, shale, and pelite that are divided into face charters below them are older “rocknrolls” including granite, pegmatite interventions, and gneiss, a metamorphic face. The upper charters on Mount Everest and neighboring Lhotse are filled with naval fogies.

Three Distinct Rock Formations

Mount Everest is composed of three different face charters.

From the mountain base to the summit, they il be : the Rongbuk Formation the North Col Formation and the Qomolangma Formation. These rock and roll slice are disbanded by low angle blunders, moving each one in the course of the coming in a zigzag plan.

The Rongbuk Formation At The Bottom

The Rongbuk Formation becomes the basement “rocknrolls” below Mount Everest. The metamorphic face includes schist and gneiss, a finely stripped-down face. Levered between these old fashioned face drivels are immense sills of granite and pegmatite dikes where molten magma spurted into crackings and solidified.

The North Col Formation

The complex North Col Formation, defined between 7,000 and 8,600 metres high, subdivides into many different roles. The upper 400 tempo species the acclaimed Yellow Band, a yellowish brown face banding of marble, phyllite with muscovite and biotite, and semischist, a somewhat metamorphosed sedimentary rock.

The band also contains fogies of crinoid ossicles, a naval swine with a skeleton. Below the Yellow Band are more interspersing membranes of marble, schist, and phyllite. The lower 600 lilts is composed of various schists assembled by metamorphism of limestone, sandstone, and mudstone. At the bottom of the affecting is the Lhotse detachment, a protruding faulting that subdivides the North Col Formation from the underlying Rongbuk Formation.

The Qomolangma Formation At The Summit

The Qomolangma Formation, the most important point one “rocknroll” on the summit pyramid of Mount Everest, is organized by membranes of Ordovician age limestone, recrystallized dolomite, siltstone, and lamina. The affecting beginning at 8,600 tempo at a faulting neighborhood above the North Col Formation and purpose on the summit. The upper membranes have endless naval fogies, including trilobites, crinoids, and ostracods. One 150 feet thick bunk at the bottom of the summit pyramid contains the remains of micro-organisms including cyanobacteria, situated in shoal heated ocean.

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