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Subglacial stream information


Subglacial streams are conduits of glacial meltwater that flow at the base of glaciers and ice caps.[1] Meltwater from the glacial surface travels downward throughout the glacier, forming an englacial drainage system consisting of a network of passages that eventually reach the bedrock below, where they form subglacial streams.[1] Subglacial streams form a system of tunnels and interlinked cavities and conduits, with water flowing under extreme pressures from the ice above; as a result, flow direction is determined by the pressure gradient from the ice and the topography of the bed rather than gravity.[1] Subglacial streams form a dynamic system that is responsive to changing conditions, and the system can change significantly in response to seasonal variation in meltwater and temperature.[2] Water from subglacial streams is routed towards the glacial terminus, where it exits the glacier.[2] Discharge from subglacial streams can have a significant impact on local, and in some cases global, environmental and geological conditions.[3] Sediments, nutrients, and organic matter contained in the meltwater can all influence downstream and marine conditions.[4] Climate change may have a significant impact on subglacial stream systems, increasing the volume of meltwater entering subglacial drainage systems and influencing their hydrology.[2]

  1. ^ a b c [1] Hooke, Roger LeB. “Englacial and Subglacial Hydrology: A Qualitative Review.” Arctic and Alpine Research 21, no. 3 (August 1, 1989): 221–33. https://doi.org/10.1080/00040851.1989.12002734.
  2. ^ a b c Cite error: The named reference hubbard was invoked but never defined (see the help page).
  3. ^ Cite error: The named reference stevenson was invoked but never defined (see the help page).
  4. ^ [2] Ren, Ze, Nicolas Martyniuk, Isabella A. Oleksy, Anshuman Swain, and Scott Hotaling. “Ecological Stoichiometry of the Mountain Cryosphere.” Frontiers in Ecology and Evolution 7 (2019). https://www.frontiersin.org/article/10.3389/fevo.2019.00360.

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are frequently found in regions with limestone geologic formations. Subglacial streams are the braided rivers that flow at the beds of glaciers and ice sheets...

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a core. Thus, accretion and erosion of soft sediment by processes of subglacial deformation do not present unifying theories for all drumlins—some are...

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Kamb ice stream. The subglacial motion of water is expressed in the surface topography of ice sheets, which slump down into vacated subglacial lakes. The...

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400 m (1,300 ft) deep. Tunnel valleys were formed by subglacial erosion by water and served as subglacial drainage pathways carrying large volumes of meltwater...

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