Cook is subject to various different types of weathering such as freeze thaw weathering. The Southern Alps are the first obstacle the winds encounter after South America, having moved east across the Southern Ocean.
Dislocation of river terraces across the Alpine Fault shows that over the past 10, years, this uplift has continued at an average of 10 millimetres or more a year.
The mountain itself has been formed by three main geological processes; one internal: Nothing but grey The mountain ranges that form the backbone of New Zealand are made of ancient greywacke, which is being rapidly uplifted and eroded.
The glaciers carved out the sheer-walled, U-shaped valleys and fiords of Fiordland, and the deep up to metres southern lakes.
Due to the wind Mt. These include the Tasman Glacier to the east of the mountain and the smaller Hooker Glacier immediately to its south. Westerly Winds External 1. Winter and spring are usually less settled than summer and autumn.
Combined with high rainfall, this results in very rapid rates of weathering and erosion. Present rate of uplift is mm a year but this is easily countered by weathering and erosion.
Cook and creates a transform fault. Cook has been shaped by powerful forces of weathering.
As the air rises towards the peaks, it expands and cools, and forms clouds. Boulders in many of the rivers are made almost entirely of this rock.
However, the south wind froze them and turned them to stone. Jane Thomsonconsidered at the time "a marvellous feat unequalled for daring in the annals of the Southern Alps". When the wind reaches the Southern Alps the air rises and drops rain on Mt. Cook formed differently compared to other mountains.
The climb crosses large crevasses, and involves risks of ice and rock falls, avalanches and rapidly changing weather conditions. Much of the sand on the beaches is made of tiny fragments of greywacke — which is why most New Zealand beaches are grey.
The results of this vigorous erosion is apparent in the widespread cones of eroding scree and the expanses of boulder and gravel that make up the beds of the larger rivers.
It last moved in This has resulted in a sharper topography of sheer-walled valleys, fiords and chiselled peaks.
When the water reaches the mountain it lands in a crack, it then freezes freezes and expands making the crack bigger. As they collide, the plates push up the land, forming mountains. This is credited as the first solo ascent, although Zurbriggen was accompanied part of the way up the ridge by J Adamson.
Much of the alps, Fiordland and the north-west ranges receive over 3, millimetres. Evidence of this uplift is apparent on the mount on the south ridge specifically the Endeavour col fold where sand, mud and silt has been folded and fractures forming vertical beds of silt and sandstone.
In the North Island the highest annual rainfall occurs on Mt Taranaki Mt Egmontincluding a record millimetres in 48 hours in These are greywacke that contains narrow bands of siltstone in the east, grading into schist west of the main divide.
Sideways movement As well as uplift, there has been major sideways movement along the plate boundary. On reaching the mountains the air rises, dropping rain on the west coasts. However, erosive forces are also powerful shapers of the mountains.In a dramatic scene of alpine erosion, a huge rock avalanche broke away from the High Peak of Aoraki/Mt Cook in December About 14 million cubic metres of rock and ice fell onto the surface of the Tasman Glacier, reducing the height of New Zealand’s highest mountain by 10 metres.
The Aoraki / Mount Cook massif is a major obstacle to the prevailing westerly winds as they push depressions and associated cold fronts of moist air from the subtropics in the northwest against the mountain range. As the air rises towards the peaks, it expands and cools, and forms clouds.
Mt Cook/Aoraki formation Vinoth Loganathan New Zealand is a country which ‘straddles’ between two tectonic plates; the indo-Australian and the Pacific. (descending members) Mount Tabor, Spiller, Landrum, and Wheelock References Bureau of Economic Geology,Crystal City-Eagle Pass Sheet, Geologic Atlas of Texas.
Jul 18, · Mount Cook (or Boundary Peak ) is a high peak on the Yukon Territory-Alaska border, in the Saint Elias Mountains of North America.
It is approximately 15 miles southwest of Mount Vancouver and 35 miles east-southeast of Mount Saint ultimedescente.com: Resolved.
Mt Cook/Aoraki formation Vinoth Loganathan New Zealand is a country which ‘straddles’ between two tectonic plates; the indo-Australian and the Pacific.
The location of the South Island is south of both Australia and South Africa; this is a major contributor to the geological process of weathering because it makes Mt.
Cook subject to the westerly .Download