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FLUVIOGLACIAL DEPOSITION LANDFORMS ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Photo sources credited where known – for educational use only.
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],1. OUTWASH PLAINS EXAMPLES: Kelling Heath and Salthouse Heath – North Norfolk
Remember – sands and gravels on outwash plains are sorted and graded! Source:  http://uregina.ca/~sauchyn/geog323/342.jpg
Kettleholes ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
These form on outwash plains and occur where channels of meltwater get become clogged by course deposits. This encourages the stream to divide and braid. They are common in outwash areas due to seasonal fluctuations in discharge. 2. BRAIDED STREAMS Source:  http://pubs.usgs.gov/of/2004/1216/b/images/braided2.gif   ,[object Object],[object Object],[object Object],[object Object],[object Object]
3. VARVES These are the vertical stratification of sediments and are found in the bottom of pro-glacial lakes. Sediment carried by meltwater streams is deposited when water enters a pro-glacial lake as the energy of the stream is lost. Meltwater streams vary in discharge seasonally and  Varves have alternative sequences of coarser (sand and gravel) and finer (clay and silt) bands. 1. Coarse sediment – deposited in summer (greatest because of fast melting – higher energy – larger material transported) 2. Finer sediment – deposited in winter – little or no coarse sediment washed into lake Each pair of varves represent’s a year’s accumulation (can therefore count varves to calculate age of sediment) Thickness varies (according to weather – can indicate climate change fluctuations) – thicker bands – indicate warmer conditions – more meltwater and more load – if darker – may indicate more organic matter and again therefore warmer conditions.
4. KAMES, KAME TERRACES & KAME DELTAS These are ice-contact stratified drift features – deposited in the vicinity of melting ice and partly sorted by water. ,[object Object],[object Object],[object Object],EXAMPLES: East Lothian – Scotland (a few hundred m long & tens of m high) Source:  http://www.uwsp.edu/geo/faculty/ritter/glossary/h_k/kame.html
[object Object],[object Object],[object Object],4.2 KAMES TERRACES Source:  http://www.fettes.com/Cairngorms/glacial%20landscapes%20deposition.htm   4.3 KAME DELTAS These are fan shaped mounds containing debris from ice and Fluvioglacial material. They are formed when glacial streams enter a pro-glacial lake. Where supra and en-glacial streams emerge at the snout and enter a pro-glacial lake they lose energy and deposit their load..
5. ESKERS These are long sinuous ridges of land – composed of sands and gravels – they can be 20-30m high and can meander across the landscape for many km. ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]

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Fluvioglaciation

  • 1.
  • 2.
  • 3. Remember – sands and gravels on outwash plains are sorted and graded! Source: http://uregina.ca/~sauchyn/geog323/342.jpg
  • 4.
  • 5.
  • 6. 3. VARVES These are the vertical stratification of sediments and are found in the bottom of pro-glacial lakes. Sediment carried by meltwater streams is deposited when water enters a pro-glacial lake as the energy of the stream is lost. Meltwater streams vary in discharge seasonally and Varves have alternative sequences of coarser (sand and gravel) and finer (clay and silt) bands. 1. Coarse sediment – deposited in summer (greatest because of fast melting – higher energy – larger material transported) 2. Finer sediment – deposited in winter – little or no coarse sediment washed into lake Each pair of varves represent’s a year’s accumulation (can therefore count varves to calculate age of sediment) Thickness varies (according to weather – can indicate climate change fluctuations) – thicker bands – indicate warmer conditions – more meltwater and more load – if darker – may indicate more organic matter and again therefore warmer conditions.
  • 7.
  • 8.
  • 9.