Glacial Landscapes Flashcards

1
Q

What is a glacier?

A

A large accumulation of snow and ice which moves under its own weight.

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2
Q

How does a glacier form?

A

Precipitation falls as snow.

Each Layer becomes heavier and compresses the layers underneath.

This is called diagenesis

Real glacial ice is when there is only 20% of air as bubbles

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3
Q

What is an open system?

A

A system that allows the transfer of both matter and energy to neighbouring systems

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4
Q

What is a glacial period

A

Periods of very cold and dry climate in which land ice and valley glaciers have grown to their maximum levels
The last one ended 10,000 years ago

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5
Q

What is an interglacial period

A

Warmer periods during which much of the ice has retreated
Current interglacial period is known as the Holocene

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6
Q

Inputs of a glacial system

A

Snow, hail, avalanches, rock debris, solar energy

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7
Q

Outputs of a glacial system

A

Calving, melting, sublimation, evaporation, previously eroded material that has been transported and deposited by the glacier

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8
Q

Give an example of a positive feedback loop in a glacial environment

A

Temperature rises - Permafrost melts - Co2 released - Greenhouse effect - Temp rises

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9
Q

Give an example of a negative feedback loop in a glacial environment

A

Temp rises - Permafrost melts - Plants absorb more co2 - Reduces greenhouse effect - Temp cools

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10
Q

Name the 4 types of polar environments

A

Polar, Periglacial/tundra, alpine, glacial

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11
Q

What is the albedo effect

A

When incoming solar radiation is reflected back into space due to light colours such as ice
This causes it to be cooler in these areas

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12
Q

Outline the characteristics of the climate in periglacial environments

A

Very cold and dry all year round
little seasonality

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13
Q

What are the main features of soil in periglacial environments?

A

Lack of clearly defined layers

Thin organic layer, often acidic

Waterlogged in summer

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14
Q

What are the main features of vegetation in periglacial environments?

A

Low level of production

Low levels of biodiversity

Vegetation close to the ground

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15
Q

What does aspect mean?

A

The direction the slope faces

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16
Q

What does accumulation mean

A

The addition of snow and ice over time

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17
Q

What does ablation mean?

A

The loss of snow and ice overtime

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18
Q

What is the net balance of a glacier

A

The difference between accumulation and ablation

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19
Q

What is pressure melting point

A

That temperature at which ice is on the verge of melting

20
Q

Outline the characteristics of a warm based glacier

A

Found at high altitude locations

Meltwater means the glacier is more mobile

More rates of erosion, transportation and deposition

Athabasca Glacier

21
Q

Outline the characteristics of a cold based glacier

A

Found at high latitude locations

Less meltwater so often does not move much

Much less erosion, transportation and deposition

Meserve Glacier

22
Q

Outline the process of internal deformation

A

Explains the movement of cold based glaciers
Under great pressure at the base of a glacier the ice crystals allign themselves to the direction of movement of the glacier
Most likely near the bed as pressures are highest
Cracks can emerge leading to the formation of crevasses
Glacier remains frozen to the bedrock

23
Q

Corries

A

Form when snow continues to build up in a nivation hollow and eventually compacts to form a glacier

Glacier becomes trapped within the hollow, only way it can move is rotational slip

Back wall eroded through plucking and frost shattering, hollow deeped via abtasion

Water can fill corries to make tarns

24
Q

Arêtes

A

A knife edged ridge formed between two corries (when two steep backwalls meet)

If three meet they create a pyrmaidal peak

25
Glacial Troughs
A u-shaped valley formed by a glacier bulldozing and eroding through a river valley The glacier has enough force to erode a rivers interlocking spurs leaving smooth but steep truncated spurs aswell as a wide flat valley floor The original river will continue to flow but now as a misfit stream due to the difference in its size with its surroundings
26
Hanging Valleys
A smaller u-shaped valley caused by a tributary glacier. The smaller glacier does not have enough energy to erode to the valley floor leaving a hanging valley where waterfalls usually form
27
Roche mountonees
Glacier hits an obstacle that is too large/hard to pluck Hitting the obstacle creates pressure and friction increasing melting as the lower ice reaches PMP The meltwater allows the glacier to slide over the rock and smaller rocks abrade the stoss side When the glacier reaches the top of the obstacle friction and pressure drop Meltwater refreezes Frozen rocks are plucked from the lee side
28
Till plains
Unsorted glacial material formed through erosion and weathering Form when an ice sheet detaches from the main glacier and melts causing all of the till on top of and within the glacier to deposit on the valley floor
29
Erratics
A large boulder that is of a different rock type to the surrounding rock Would have been broken off by weathering and erosion then transported by a glacier and deposited when it has been moved to a different location
30
Moraines
Deposits of eroded material that are transported with the glacier Lateral: Material deposited on the sides of a glacier leaving a ridge when the ice melts Medial: Formed when two lateral morains meet in the middle of a glacier and deposit material Ground: Carried under the glacier and abraded between glacier and valley floor. Only sorted moraine Recessional: Forms at the end of a glacier
31
Drumlins
When a glacier hits an obstacle that cannot be eroded deposition from underneath the glacier builds up behind the obstacle The glacier moves over the large mound and drags excess deposition to the other side Tear drops shape with a long tapered edge Blunt end - stoss side Tapered end - Lee side
32
Why is plant growth difficult in the Tundra?
Waterlogged soils - thawed soils can’t infiltrate through permafrost and evaporation rates are low Strong winds Low levels of precipitation Low insulation Short growing season - no more than 60 days
33
Vegetation and soil characteristics in cold environments - polar
Slow nutrient cycles Climate means decomposers can’t thrive Cold, harsh climate with little rainfall - only highly adapted vegetation can grow such as mosses and lichen Overall there is a cycle where poor vegetation creates poor soil and poor soil causes poor vegetation
34
Vegetation and soil characteristics in cold environments - Alpine
Heavy snowfall in winter In summer there is heavy rainfall aswell meltwater Mild temps stimulate plant growth, thawing and decomposition Alpine vegetation is decomposed more quickly than in a polar climate, and grows quicker too due to soil fertility and climate. The nutrient rich vegetation allows a more fertile soil to develop when it decomposes, as the nutrients are transferred into the soil. This fertile soil allows more nutrient rich plants to grow.
35
Vegetation and soil in cold environments - periglacial tundra
Temperatures are consistently below freezing. The latitude of some permafrost regions also assists in the consistently cold temperatures, as winters in higher latitudes last longer with less daylight hours, making them colder. Vegetation is more prevalent than in polar regions, but only highly adapted plants can survive in the cold temperatures with little rainfall. The temperatures and poor soil leads to a slow nutrient cycle. The lack of nutrient rich plants contributes to the soil infertility. The cold climate causes the lower ground to be frozen all year around. However, slightly warmer summer temperatures cause the thawing of upper soil called the active layer. Soil is usually extremely waterlogged in summer due to thawing, which means plants become deoxygenated within the soil and cannot survive, and any nutrients are often leached out.
36
Vegetation adaptions to tundra environment
Vegetation grows close to ground - protects from strong winds Shallow roots - To allow it to get nutrients from the active layer Can photosynthesise at low temps - due to low temps from albedo effect, they can create energy Perennial plants - store food to allow them to survive during harsh winters
37
Impacts of climate change in cold environments: Reduced ice on rivers and lakes
Northern USA most lakes are freezing later and thawing earlier than 150 days ago - many isolated communities and the oil and gas industries rely on frozen rivers and lakes to transport vital supplies including drilling equipment, building materials
38
Impacts of climate change in cold environments - Shrinking glaciers
Globally 90% of glaciers are losing ice mass A gradual decrease in ice has been recorded since the 1850s with a short period of gain around 1970, but in the decades since the rate of loss has been unprecedented Millions of people rely on glacial meltwater as their freshwater supply so this would reduce the amount of freshwater available to these communities Reduce opportunities for tourism in places such as the alps
39
Impacts of climate change in cold environments: accelerated sea level rise
Studies show that rate of sea level rise for most of the 20th century was about 1.7mm per year. In 2019 NASA reported the current average rate is about 3.4mm per year - leading to the loss of land globally and this can cause the displacement of people in Tuvalu and the Maldives
40
Impacts of climate change in cold environments: highest expected temperature change to be in highest northern latitudes
Latitudes between 40 degrees North and 70 degrees North could rise betweeb 5 degrees and 8 degrees by 2100, due to the loss of sea ice and snow cover reducing albedo rates - higher temperature will increase the rate of ice and permafrost melting
41
Alaska case study - BACKGROUND INFO
North - tundra environment with permafrost South - relatively milder conditions One of the most sparsely populated places on earth - nearly 1/2 of its 750000 residents live in Anchorage Since the 1980s approximately 100,000 inuit have been joined by permanent settlers
42
OPPORTUNITIES FOR DEVELOPMENT IN ALASKA - Mineral extraction
Abundant mineral resources (coal, gold, copper) Gold rush in the 1800s 20% of Alaska's mineral wealth lies in gold
43
OPPORTUNITIES FOR DEVELOPMENT IN ALASKA - energy
1/3 of the state's income comes from the industry which employs over 100,000 people Oil is transported from Prudhoe Bay in the north to valdez in the south by the trans-alaskan pipeline The pipeline is raised above the land to avoid melting the permafrost, which could cause the pipeline to break
44
OPPORTUNITIES FOR DEVELOPMENT IN ALASKA - FISHING
Fishing industry employs 80000 people in Alaska - worth $8 billion to the economy Indigenous people use fish to provide food, clothing and oil as part of their subsistence lifestyle
45
OPPORTUNITIES FOR DEVELOPMENT - Tourism
Alaska attracts over 2 million tourists each year 60% of summer tourists arrive via cruise
46
DEVELOPMENT CHALLENGES IN ALASKA - Extreme temperature
Winter temperatures can drop below -30 degrees in the north of Alaska This along with limited sunlight makes working outside very challenging
47
DEVELOPMENTAL CHALLENGES IN ALASKA - Buildings and infrastructure
Roads are built on raised gravel beds to reduce heat transfer which can thaw the permafrost Many domestic services such as freshwater and sanitation have to be provided above ground in insulated utilidors to minimise the risk of freezing pipes and thawing the permafrost. In addition, runways are painted white to reflect the energy and reduce heat transfer from the sun