periglacial environments Flashcards

1
Q

what is Solifluction?
what landforms does it produce?

A

• The downward movement of the waterlogged the active layer due to the influence of gravity
• forms solifluction lobes

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2
Q

what are Solifluction Lobes

A

• a landform created when the soil falls down the hillside in tongue-shaped lobes.

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3
Q

what is nivation?
what landforms are produced by this?

A

• a combination of erosional and weathering processes due to snow and ice
• forms nivation hollows

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4
Q

what is the active layer?

A

•the surface of the ground, which is able to move because it has been thawed

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5
Q

what is permafrost?
and what are the three types?

A

•ground that has been permanently frozen for over two years

•there is continuous, discontinuous and sporadic permafrost

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6
Q

what is continuous permafrost ?
where is it found?

A

• permafrost that is very deep (up to 1500m deep in some cases) and has summers so cold that there is only very little surface melting
• found at the highest latitudes where almost all ground is frozen at a great depth

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7
Q

• what is discontinuous permafrost

A

• when the permafrost is relatively shallow and has parts of unfrozen ground
• occurs in areas with a mean annual temperature of -5°c and -1.5°c.
• the surface of discontinuous permafrost tends to melt over the summer months

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8
Q

what is sporadic permafrost ?

A

• permafrost found where the mean annual temperature is just below 0°c, and permafrost patches cover less than 50% of the landscape

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9
Q

what’s frost heave?
how does it happen?
what landforms does it create?

A

• Frost heave occurs when soil expands and rises due to the freezing of water within it.
•When the temperature drops, water in the soil freezes, creating ice lenses that force the soil upward.
• creates patterned ground and pingos. overtime frost heave is repeated which creates hills, or patterns where the soil has been forced out over the ice in the soil.

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10
Q

what’s frost action?

A

• any process that occurs in soil and rock due to the freezing and thawing of water eg frost heave

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11
Q

what’s meltwater erosion?
what features does it create?

A

• is the process by which water from melting snow or ice erodes the streams or river channels
• This can create features like valleys and braided rivers

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12
Q

what do high winds do to the periglacial environment?

A

• they can cause erosion by removing loose soil and sediment,
• it can also transport fine particles and dust, reshaping the landscape
• they can contribute to the formation of features like patterned ground by aiding in the movement of stones and soil.

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13
Q

how do ice wedges form?

A

• through freeze-thaw cycling.
•when it’s cold, water in the cracks of soil or permafrost freeze, and cracks widen. When temperatures rise again, the ice melts but the cracks remain. this process repeats and more water can enter the cracks and freeze, leading to the growth of the ice wedge.

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14
Q

what is a loess?
how does loess form?

A

• it’s a type of sediment that is made up of fine silt and dust particles.
• Loess forms when a glacier grinds the bedrock turning it into rock flour, and this sediment travels to the snout of the glacier in meltwater or through the wind.

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15
Q

how does patterned ground form ?

A

• When the ground repeatedly freezes and thaws, ice in the soil forces upwards rock and sediment creating cracks and patterns on the surface of the rock. These patterns can take various shapes,

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16
Q

how does a closed system pingos form?
how does it differ to an open system pingo?

A

• it forms when there is a layer of permafrost that has groundwater beneath it or on its surface. As the groundwater freezes, it expands and pushes the overlying soil upward, creating a dome shape.
• sometimes in summer, the ice lens can melt and the pingo will collapse, creating a hollow (ognip)

• one diff is they typically form in continuous permafrost areas
• the groundwater supply is not continuous

17
Q

where are periglacial area found today vs the past ?
and why is that the case?

A

• today periglacial areas are found at higher latitude, and some alpine areas (lower latitudes with higher altitudes)
• during the pleistocene epoch, periglacial areas were found in todays mid-latitude ; temperate areas
• there are less periglacial areas now due to global warming which has led to the melting of ice, so less land is in close proximity with glacial areas

18
Q

what are stone polygons?
how do they form?

A

• they are stones that are arranged in a polygonal pattern on the ground.
• they form when ice expands during freezing, which pushes stones to the surface through frost heave , creating patterns

19
Q

what is calving?

A

• the process where chunks of ice break off from the edge of a glacier into the a body of water , forming icebergs.

20
Q

what is ground ice ?

A

• ice that forms within the soil or sediment, often in permafrost regions.

21
Q

what are braided rivers?
how do they form?

A

• a type of river that has multiple channels that weave in and out around small islands or bars of sediment.
• formed when the a meltwater stream or river has a high sediment load and due to changes in water volume or energy, the sediment is deposited causing the river to find an easier course around the sediment

22
Q

what is a talik?
what type of permafrost is it found in?

A

• a layer of unfrozen ground that exists under or on top of a layer of permafrost.
• found in discontinuous permafrost

23
Q

what is a thaw lake?

A

• a lake that forms in permafrost regions when the ground thaws during warmer seasons and water fills in depressions in the landscape

24
Q

what are periglacial environments

A

• places that are on the fringe of glacial landscapes and have periods of extremely cold temperatures and the presence of permafrost

25
Q

what is isolated permafrost?

A

• permafrost that covers less than 10% of an area

26
Q

what is freeze thaw weathering / frost shattering?
what landforms does it form?

A

• when water gets into the cracks of rock, and freezes when the temperature drops, causing it to expand by around 10% , expanding cracks in the rock
• it forms felsenmeer (when on a flat surface) which is an accumulation of angular rock fragments, or forms scree when it’s on a slope

27
Q

what is groundwater freezing?
what features does it produce?

A

• when water in the ground or soil turns into ice.
• creates ice lenses and permafrost

28
Q

what is aeolian action?
what landforms does it form?

A

• the processes of erosion, transportation, and deposition of sediment by wind.
• it can create dunes & loess deposits,

29
Q

how do open system pingos form?
how do they differ from closed system pingos ?

A

• they form when groundwater flows through gaps in the permafrost causing water to accumulate and freeze, creating an ice lens
• the active layer surrounds the ice lens and forms a dome shaped hill
The key difference is that closed system pingos rely on trapped groundwater,
• one diff is that open system pingos depend on an external supply of water.
• open system pingos are typically found in discontinuous permafrost