Glacial Landscapes Flashcards

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1
Q

What is plucking?

A

As the ice moves over the rock surface below, meltwater freezes around loose sections, pulling them away. Plucking is especially effective when the rock contains many joints (cracks) which the water can seep into.

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2
Q

Why is meltwater present under a glacier?

A

The sheer weight of ice above. Ice at the base of the glacier melts because of the great pressure it is under( this is called pressure melting). Also, meltwater has travelled from the surface of the glacier to its base through crevasses in the ice

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3
Q

What is abrasion?

A

Erosion is caused by rocks and boulders embedded in the base of the glacier. These act like sandpaper, scratching and scraping the rocks below. Very large boulders can do enormous damage this way, scarring the landscape with features called striations. These are still visible in the UK today.

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4
Q

How are striations formed?

A

Very large boulders scrape along the rocks below and scar the landscape.

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5
Q

What increases the rate of abrasion?

A

When a lot of plucking has taken place, large numbers of rocks and boulders become embedded into the ice.

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6
Q

Where does freeze thaw weathering take place in glaciated areas?

A

Takes place on rock surfaces above the surface of the ice and at its margins

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7
Q

How does freeze thaw weathering take place?

A

Water seeps into cracks in the rock face

The temperature falls at night, causing the water to freeze

Water expands by 9-10% when it turns to ice. This expansion puts pressure on the rock either side of the crack, prising it apart and causing the crack to tear wider open.

During the next 24 hour cycle, the ice melts, sinks deeper into the crack and then freezes again

Over time large boulders of rock can be shattered apart by repeated cycles of this weathering process

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8
Q

How is freeze thaw weathering evident?

A

Seen in landscape features called scree slopes and block fields.

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9
Q

What is the difference between weathering and erosion?

A

Erosion requires a moving force like ice to break apart rock and carry it away. In contrast, weathering describes the destruction of rock that take place in a particular place. Weathering is caused by temperature and moisture changes along with any chemical processes.

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10
Q

How do glaciers move?

A

Glacier ice forms from snow that is compressed

As the weight of the ice accumulates, gravity causes it to flow over the lip and down the mountain

The surface of the glacier cracks as the glacier moves over the uneven valley floor. Deep crevasses form.

The glacier slide over the underlying rock on a film of meltwater (basal flow). The ice speeds up and slows down in response to changes in gradient (internal deformation)

As the glacier moves, the valley floor and sides are eroded by plucking and abrasion. In result lots of moraine is left carpeting the valley floor

As the glacier descents the climate gets warmer, rock debris is deposited to from moraine

The end point of the glacier is called the snout. Large amounts of meltwater pour off the snout of the glacier qnd can carry debris far beyond here.

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11
Q

How does a glacier transport material?

A

The snout bulldozes material, soil, rocks and boulders are shoved forwards by the force of the glacier

Material is also carried in the surface of the glacier (conveyor belt model)

Plucking tears away rock and this becomes embedded into the glacier

Some rocks fall into crevasses which result in material being carried along the ground and deep inside the glacier

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12
Q

Why does deposition take place?

A

Deposition takes place when the glacier moves into lowland areas. The rocks that have been carried are deposited as the snout melts as the temperature gets warmer.

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13
Q

What is the dumped material of a glacier called?

A

Till

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14
Q

What is the sediment called that meltwater rivers carry?

A

Glacial outwash

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15
Q

How are upland areas affected by ice erosion?

A

Glaciated places across the world are home to unique landforms that give them a special character that is not found elsewhere.

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16
Q

How is a Corrie formed?

A

A snow patch in a hollow, deepens and compresses to become a dense mass of ice

Freeze thaw weathering increases its density by removing air

As it pulls away from the walls of the hollow, blocks of rock are plucked. Once embedded they abrade the hollow making it wider deeper and steeper

Freeze thaw weathering takes place on the back of the hollow, the surface soon becomes covered in uneven rock. Over time the back wall retreats backwards, cutting deeper into the mountain

17
Q

How is an arête formed?

A

Two corries develop side by side or back to back. Creating freeze thawed ridge that is narrow.

18
Q

How is a pyramidal peak formed?

A

When three or more corries grow in hollows on all sides of a mountain creating a sharp point.

19
Q

How are glacial troughs formed?

A

Before glaciation, a river valley would have been v shaped. River tributaries flowed down the gentle valley sides to reach a meandering valley floor.

During glaciation, the rock in the valley is torn away by a combination of plucking and abrasion. The result is a u shaped valley or a GLACIAL TROUGH. It is very steep and has a wide valley floor

20
Q

How is a hanging valley formed?

A

The tributaries that used to flow down the river valley sides now exit abruptly through a gap in the new cliff shaped valley wall. The water cascades down form a high altitude and creates a waterfall. The portion of the original tributary valley that remain is now called a HANGING VALLEY. Abrasion and plucking tore the sides away.

21
Q

How are truncated spurs formed?

A

Abrasion and plucking tear the rocks away. The ices has erosive power to remove any obstacle in its path.

22
Q

When are depositions landforms produced?

A

Depositional landforms are produced when a glacier loses the ability to carry material

23
Q

What are moraines?

A

Accumulations of rock debris.

24
Q

Name the different types of moraine?

A

Lateral moraine

Medial moraine

Ground moraine

Terminal moraine

25
Q

What is lateral moraine?

A

A ridge of material that runs along the edges of a glacial trough close to the valley side. The source of material is freeze thaw weathering, high on the valley sides, causing shattered blocks of rock to fall onto the glacier below. As the ice melts and the glacier gets smaller, this material is slowly lowered to and deposited on the valley floor

26
Q

What is medial moraine?

A

When glaciers meet, something very interesting happens,. Two lateral moraines merge together to form a very large ridge of rock debris: the medial moraine.

27
Q

What is ground moraine?

A

The material that gets lodged and deposited underneath the glacier is simply called ground moraine. Vast amounts of ground moraine can be produced when glaciers disappear entirely in response to climate change. Ground moraine covers large areas of the UK as a legacy of the last ice age.

28
Q

What is terminal moraine?

A

This is the enormous ridge of material that gets bulldozed by the snout of the glacier. These allow us to work out how far the ice advanced during the last ice age.

29
Q

What are drumlins?

A

Drumlins are egg shaped hills composed of mounds of till

30
Q

How are drumlins formed?

A

Material is deposited under a glacier as ground moraine

This ground moraine is sculpted to form drumlins shapes by further ice movements

31
Q

What is a glacial erratic?

A

An erratic is a large boulders that stands out like a sore thumb in the landscape. This is because it is composed of a rock type that is nowhere else to be seen