6.3: Glacier hydrology - the role of meltwater Flashcards

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1
Q

Name the 2 main sources of meltwater from glaciers

A
  1. surface melting
  2. basal melting
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2
Q

Surface melting contributes most of the supply of glacial meltwater and peaks in late …?: it is the only source of meltwater for …? basal glaciers. supraglacial surface …? form running along the top of the ice, especially in the …? zone. They are often fast flowing and may plunge down into the glacier becoming …?

A
  1. summer
  2. cold
  3. streams
  4. ablation
  5. englacial
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3
Q

Basal melting occurs if temperatures of the ice at the base of a glacier is at …? melting point (in a warm-based glacier). The basal meltwater flows under …? pressure beneath the glacier and can excavate subglacial …? cutting through the bedrock. The meltwater streams eventually …? from glacial tunnels at the glacier snout via portals (…?)

A
  1. Pressure
  2. Hydrostatic
  3. tunnels
  4. emerge
  5. caves
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4
Q

Name 2 reasons why fluvo-glacial streams operate differently than other streams?

A

High pressure and velocity of flow

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5
Q

Fluvo-glacial steams have high pressure and …? of flow. This causes the erosion of underlying bedrock by abrasion, cavitation and …? means beneath the ice, and can also lead to intense …? by meltwater streams as they exit the glacier …?. The ablation rates are very …? during de-glaciation, and many if the meltwater streams have very high …? leading to powerful erosion.

A
  1. velocity
  2. chemical
  3. erosion
  4. snout
  5. high
  6. Discharges
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6
Q

When meltwater deposits material subglacial, englacial and supraglacial, the material is referred to as…

A

an ice-contact fluvio-glacial deposit

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7
Q

Name 3 key characteristics of fluvo-glacial deposits

A
  • generally smaller than glacial till as meltwater streams; although having high discharge, they still have less energy than large valley glaciers so they generally
  • generally smoother and rounder through water contact and attrition
  • sorted horizontally, especially in the case of outwash deposition, with the largest material found up-valley or nearer the glacier snout, and progressively finer material down-valley, due to the sequential nature of deposition mechanisms
  • stratified vertically with distinctive layers that reflect either seasonal or annual sediment accumulation
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8
Q

what is the difference between fluvo-glaivally deposited material and glacial till?

A

Glacial till is angular, poorly sorted and non-stratified whereas fluvo-glacial deposits tend to be rounder, smoother and sorted

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9
Q

What is the difference between fluvio-glacial deposits and outwash deposits?

A

Outwash deposits experience more attrition, causing clasts to become more rounded and the material is better sorted horizontally

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10
Q

Name the 3 zones of outwash deposits

A
  • Proximal zone
  • Medial zone
  • Distal zone
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11
Q

What zone of outwash plain is described?

Immediately in front of the glacier, close to the snout. Meltwater has greatest power here so the outwash deposit contains a large particle size. Outwash may be interbedded with layers of till as some glacial deposition may occur. Outwash may occur in alluvial fan forms.

A

Proximal zone

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12
Q

What zone of outwash plain is described?

Further from ice margin, meltwater streams tend to anastomose and form braided channels because of high daily and seasonal variability of meltwater discharge. Particle size is less coarse than in the proximal zone and clasts are more rounded.

A

Medial zone

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13
Q

What zone of outwash plain is described?

Furthest from ice margin. Drainage pattern resembles normal drainage system, with meanders on a broad flood plain. Outwash is well sorted and characterised by smaller and even more rounded particles.

A

Distal zone

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14
Q

Name this fluvo-glacial depositional feature by its description

Long, sinuous ridges on the valley floor

A

Eskers

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15
Q

Name this fluvo-glacial depositional feature by its description

Small mounds on the valley floor

A

Delta Kames

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16
Q

Name this fluvo-glacial depositional feature by its description

Ridges of material running along the edge of the valley floor

A

Kame Terraces

17
Q

Name this fluvo-glacial depositional feature by its description

Layers of sediment found at the bottom of lakes

A

Varves

18
Q

Name this fluvo-glacial depositional feature by its description

A flat expanse of sediment in the proglacial area

A

Outwash (sandur)

19
Q

Name this fluvo-glacial depositional feature by its description

Small circular lakes in outwash plains

A

Kettle holes

20
Q

Name this fluvo-glacial depositional feature by its formation

Material is deposited in subglacial tunnels as the supply of meltwater decreases at the end of the glacial period. As a glacier retreats it deposits this tunnelled material on the valley floor

A

Eskers

21
Q

Name this fluvo-glacial depositional feature by its formation

Englacial streams emerging at the snout of the glacier fall to the valley floor, lose energy and deposit their load, or supraglacial streams deposit material on entering ice marginal lakes.

A

Delta Kames

22
Q

Name this fluvo-glacial depositional feature by its formation

Supraglacial streams on the edge of the glacier pick up and carry lateral moraine, which is then deposited on the valley floor as the glacier retreats.

A

Kame Terraces

23
Q

Name this fluvo-glacial depositional feature by its formation

Sediment carried by meltwater streams is deposited on entering a lake as energy is lost. In summer, when large amounts of meltwater are available, the sediment is coarse and plentiful, leading to a wide band of sediment of relatively large material. In winter, with little meltwater present, sediment is limited in amount and size, so the bands are thin and fine.

A

Varves

24
Q

Name this fluvo-glacial depositional feature by its formation

As meltwater streams gradually lose energy on entering lowland areas, they deposit their material. The largest material is deposited nearest the snout and the finest further away.

A

Outwash (sandur)

25
Q

Name this fluvo-glacial depositional feature by its formation

During ice retreat blocks of dead ice become detached. Sediment builds up around them and, when they eventually melt, a small hollow is formed in which water accumulates to form a lake.

A

Kettle Holes

26
Q

Name the Fluvio-glacial landform from it’s description

They are formed along the front of glaciers and ice sheets where meltwater from the glacier becomes impounded within a depression blocked by glacier ice and bunded by high ground. They are ephemeral (temporary) features; depending on the rapidity of deglaciation the pro-glaciation lake can empty completely or stabilise at a lower level if the ice margin doesn’t completely disappear

A

Proglacial Lake (also known as ice-margin lakes)