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Aoraki/Mount Cook

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Aoraki/Mount Cook Evolution Step one Step 2 Step 3 Step 4 Glaciers Notes on what a glacier is + how a glacier forms SIHC\AorakiMC glaciers.doc Glacial recipe SIHC ... – PowerPoint PPT presentation

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Title: Aoraki/Mount Cook


1
Aoraki/Mount Cook
  • Evolution

2
Step one
3
Step 2
4
Step 3
5
Step 4
6
Glaciers
  • Notes on what a glacier is how a glacier forms
  • SIHC\AorakiMC glaciers.doc
  • Glacial recipe
  • SIHC\glacier formation 1.doc
  • Drawing on page 8 of El Bible Discussion of Key
    terms.

7
Terms
  • Neve (accumulation zone) The area where the ice
    accumulates.
  • Bedrock The rock that lies below the snow. In
    MC what will it be?
  • Ablatation Zone Area where the snow is
    beginning to be melted away and lost (area below
    the firn line)
  • Moraine Material that gets transported then
    deposited by the glacier.

8
Precis Sketch Drawing
  • Divide your picture of MC on page 9 into 8ths
    with doted ruled lines.
  • In your book draw a similar area once again
    divided into 8ths.
  • Now using the intersection of the lines you have
    ruled in our diagram draw an accurate precis
    sketch of MC.

9
How glaciers move
  • These rivers of ice flow at around 100,000 times
    slower than water and they do so at different
    speeds.
  • So how do they move? Ice Skater eg on Youtube.
  • Notes on how a glacier moves
  • SIHC\How Glaciers move.doc

10
Images
11
Images
12
Jason dwarfed by a Serac
13
Glacier features
  • Crevasse This is an umbrella term to describe a
    number of different features. A Crevasse is a
    crack in the ice created by tension.
  • Often crevasses are 70 metres deep.
  • Transverse Crevasse Go from one side of the
    glacier to the other.

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15
More features
  • Longitudinal crevasse found near the terminus or
    end of the glacier. The show the glacier is
    spreading outwards.
  • Marginal crevasse which point 40 degrees
    upstream.
  • Bergschrund A deep crevasse formed at the
    cirque.

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17
Pictures
18
Moraine and Till
  • Till Rock debris carried by glaciers.
  • Moraine The feature created by deposited till.
    Moraine shows where glaciers once were.
  • Lateral Moraine Found at the edges of glaciers.
    Debris usually originates from rockfalls and
    avalanches. Tasman glacier has impressive lateral
    moraines.

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More Moraines
  • Medial Moraines Formed by lateral moraines
    coming together when a tributary glacier flows
    into a main glacier.
  • Surface Moraines Occur most at the terminus of
    a glacier because ice melt exposes them.
  • Eglacial Moraine and subglacial moraine These
    are carried within and under the glacier. The
    greatest bulk of the debris is carried by these.
  • Terminal moraine The remains of a moraine that
    has receeded.
  • Firnline and equilibrium line Transition
    between the neve and melt zones.

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24
Melt-water features
  • Surface Moraines at Tasman glacier are 1-2 metres
    deep. They cover sinkholes or moulins.
  • A moulin starts as a small pothole that
    eventually deepen to join up with melt-water
    conduits that form the glacial plumbing system.
    On Tas glacier Moulins have expanded into large
    grey circular lakes.
  • These systems eventually find their way to the
    base of the glacier and they get dischard
    themselves into the fluvialglacial system
    carrying rock flour. The amount they discharge is
    enormous at present the outwash gravels are
    500-1000 metres deep.

25
Icefalls
  • Icefalls occur at Tasman glacier above the
    glacier. This is called the Hochstetter icefall.
  • Icefalls usually occur just below the neve.

26
Activity
  • Create your own mountain and glacier system.
  • Your Mountain can be called whatever you want
    (within reason) and each glacier or glacial
    feature can be called what you want (within
    reason).
  • On an a4 sheet of paper you are to create this
    glacier and accuratly add to it the different
    features glaciers create.

27
Surface Processes
  • Either created by abrasion or plucking.
  • Abrasion Scraping
  • Plucking Pulling of rocks from bedrock.
  • Small Scale features Striations, Polished rock,
    pot holes
  • Created by glacier running across the rock and
    either scraping or smoothing. Pot holes created
    by the glacier plumbing system.

28
Large Scale Features
  • When Glaciers move they carve out the landscape
    they travel over. Due to the mass material they
    move they create u shaped valleys. Rivers dont
    carve out as much and therefore only create
    v-shaped valleys.
  • U-shaped valleys often get damned up by terminal
    moraine which creates finger lakes. Lakes Tekapo,
    Pukaiki and Ohau are finger lakes.

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30
Conitued
  • The Cirque Where the neve/accumulation zone was.
    Often contains a small lake called a tarn.
  • Roche Moutonee Foliage hill provides an eg of
    this. It is a hill under the glacial ice. One
    side is a smooth gradual slope the other is a
    rough plucked cliff side.

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Continued
  • Hanging Valleys Created by tributary glaciers
    not cutting as deep a path as the main glacier
    therefore hang above.
  • Arete South ridge at MC provides a good example
    of this. It is a ridge between two criques
  • Col A pass where 2 Cirques converge. Tuckett Col
    is a good example of this.

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36
Glacial transportation
  • Glaciers act as massive conveyor belts. They
    transport both fine and large material down the
    glacial system. Around the terminus products of
    glacial transportation are ever present. The
    Tasman glacier used to extent much further and
    material found at the snout of this glacier
    showed where it used to flow to.

37
Human Modification of the environment.
  • Copy in the glacier system and explain it briefly
    underneath.
  • Glaciers work on the equation of accumulation vs.
    ablation. This is called the Mass budget.
  • This is how Humans have affected glaciers. Global
    warming has heated the earth which has meant that
    less snow is being deposited in the neve and more
    is being melted. This affects the glaciers
    ability to erode, transport and deposit.

38
Continued
  • Copy in paragraph written in italics.
  • When Answering these Questions be sure to include
    your question within the answer!!!!
  • Using text explain the following terms
    downwasting, ablation, accumulation.
  • How much of its volume is Tasman glacier losing
    each year?
  • Describe what you think a trimline is.
  • How much has the Tasman glacier dropped since
    1895?
  • At the Muellar glacier why dont the melt waters
    breach the moraine.
  • What glacier mentioned has a terminus that hasnt
    receeded yet.
  • How much has the temp at mount cook risen since
    the 1900s
  • How has El Nino affected glaciers in the
    neighbouring regions?

39
Humans and Glaciers
  • Global Warming created by the Greenhouse affect
    has led to some recession in glaciers. This
    combined with El Nino, La Nina and the Southern
    Oscillation has meant the amount caused by Humans
    is difficult to tell.

40
Climate
  • Air Pressure Air Pressure always moves from
    areas of high pressure to low pressure.
  • Wind The movement of air from low pressure to
    high pressure.
  • Precipitation Moisture in the atmosphere rain,
    hail snow, fog. Precipitation occurs when air is
    forced to rise and therefore it cools and
    condenses to dew point.

41
Rainfall
  • There are three different types of rainfall
    Frontal when two fronts collide, convection when
    a water source gets evaporated and orographic.
  • Orographic rainfall is the focus for Mt. Cook.
  • This is because the Southern Alps act as a
    massive barrier to the moisture laden westerly
    winds that flow from the Tasman sea.

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43
Climate
  • The west coast of New Zealand receives 7600mm of
    rainfall annually.
  • The area to the east of the SIHC is the driest in
    the country because of the rain shadow provided
    by the southern alps.

44
Vegetation (DW)
  • The levels of vegetation at Aoraki Mt. Cook
    differ vastly. At the top of the 3754m peak there
    is no vegetation. To the west at the foothills
    there is temperate rainforest and to the East
    there is grasslands what is the reasoning for
    these differences?

45
Vegetation
  • Life is hard for plants to survive at Aoraki Mt.
    Cook.
  • The climate is cold and blustery
  • The soil is thin and infertile
  • The landscape is steep
  • The alitude is high
  • Plants need to be resilient to survive these
    conditions
  • What would be the issues with each of the points
    above for plants?

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47
vegetation
  • The temperatures at Mt. Cook drop around a degree
    every 200 metres.
  • This inhibits the plants that can grow and the
    process of plants growing at different heights is
    called altitudinal zonation.
  • At Aoraki Mt. Cook there is over 400 different
    species of plants.
  • At the lower altitudes (up to 1300m) the
    temperate rainforest grows. This includes species
    of podocarps like Kahikatea.

48
Higher up
  • From 1300-1900m asl smaller shrub like plants
    dominate these include
  • Spear grass, Mt. Cook lily the worlds biggest
    lily, Snow tussocks, vegetable sheep.
  • Above 1900m 14 different types of Lichens have
    been found.

49
Cultural perspectives and Human activity in the
SIHC
  • Culture is an important geographic idea and is
    simply defined as a common way of life
  • Cultural perspective perception
  • How people view things differently.

50
Land Use SIHC
  • Agriculture
  • Intensive farming is it an option in the SIHC?
    Why/why not?
  • Farmers in the SIHC have developed a farming
    system known as extensive pastoralism
  • Farms are characteristically large and carry few
    sheep because of the difficult environment
  • Sheep are the main animal grazed, for wool
    production rather than meat
  • Fodder crops are grown to feed livestock in
    winter when grass growth slows down or is under
    snow.

51
  • Farmers cultural perspective would be considered
    economic
  • The major impact on the natural landscape caused
    by extensive pastoralism is the accelerated soil
    erosion caused by burning pastures and
    overgrazing by stock
  • Grazing animals accelerate soil erosion by
    removing vegetation, thereby loosening the soil
    and making erosion
  • How else might the landscape be affected?

52
Viticulture
  • In Central Otago, viticulture has also become a
    very popular form of intensive farming.
  • What is viticulture?
  • The growing of grapes for making wine
  • The hot summers and low rainfall of the region
    make it well-suited for grape-growing
  • How would vintners affect the natural landscape?

53
Hydro-electric power
  • There are many hydroelectric power schemes
    located in the SIHC, where the rivers are fed
    each year by melting snow from the Southern Alps.
    The annual snow-melt usually provides enough
    power for much of the nation
  • The cultural perspective sustainable
    perspective
  • The largest hydroelectric schemes in the SI are
    the Waitaki Valley Scheme and the Clyde Project
    on the Clutha River

54
Tourism
  • The SIHC is one of the fastest growing regions in
    NZ
  • Resorts in QTown ? provide jobs ? bring to the
    region
  • Cold winter temps. are an advantage to tourist
    operators ? Cardrona, Coronet Peak, Treble Cone
  • Tourism is carried out from an economic
    perspective
  • Ecotourism involves nature-based attractions that
    are developed with local communities for
    sustainable tourism
  • What issues might tourism create?

55
Aoraki Mt. Cook the legend
  • Aoraki plays an important part in the creation
    stories of Te Waipounamu the South Island.
    Aoraki, along with his brothers, is believed to
    have brought his waka down from the skies to
    visit Papatuanuku. As they tried to return home
    failed and the waka fell back into the water and
    turned onto its side. As the brothers scrambled
    to the higher side of the canoe, they were turned
    to stone. They remain there today as the
    mountains of the Southern Alps, with Aoraki being
    the tallest.
  • Spiritual Perspective.

56
Ngai Tahu perspective
  • For Ngai Tahu, traditions such as the legend of
    Aoraki represent links between the world of the
    gods and Maori today. These stories are part of
    their identity and history and shape the
    attitudes and beliefs they hold towards Aoraki
  • To Ngai Tahu, Aoraki is tapu. It represents the
    most sacred of ancestors from whom Ngai Tahu
    descend. In particular, the summit and the melt
    waters that flow from Aoraki are sacred, since
    Maori do not believe it is appropriate to climb
    onto the head of an ancestor.

57
Ngai Tahu Settlement
  • In 1997, the Crown agreed to return Aoraki to
    Ngai Tahu. Ngai Tahu responded giving the
    mountain back to all the people of NZ
  • Topuni of Aoraki/Mt Cook protection
  • Topuni ? derives from Ngai Tahu tikanga (custom),
    where a chief extends his protection over a
    person by placing a cloak (topuni) over him or
    her
  • This can been extended over an area or place
  • DOC has been asked by the Govt. to promote
    certain principles

58
Encouragement of respect of Ngai Tahus
association with Aoraki
  • To promote these principles DOC will
  • Provide all visitors with information about the
    Ngai Tahu values and the existence of the topuni
    over Aoraki
  • Provide education material to all climbers and
    guides explaining that to Ngai Tahu, standing on
    the very top of the mountain does not respect its
    topuni status
  • Ensure the removal of all rubbish and wastes
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