Chapter 14 Flashcards
mid-term review
Glacial system input
-10% of Earth’s land surface; 95% in Antarctica and Greenland
-input to system in precipitation as snow, insufficient solar radiation to melt
-input is a combination of ice and mineral debris and eventually lose as meltwater
Geographical and topographical features that influence climate in the glacier system
latitude and distance from the ocean; altitude, relief, aspect influence precipitation and temperature
System Function of glacial system
Inputs: snow and rain; outputs: ablation (melting of the glacier); movement of the ice causes calving as large pieces break off
calving
the breaking of ice chunks from the edge of a glacier
ablation
the process of losing mass from a glacier due to melting, sublimation, evaporation, calving, or wind erosion
Transfer of mass in glaciers
- Internal shearing or deformation
- Basal sliding – glacier over its bed
-glaciers are a frozen drainage system
basal sliding
The temperature at the base of the glacier is above the pressure melting point, allowing melting to occur.
Meltwater acts as a lubricant, reducing friction and allowing the ice to slide over the valley floor.
It involves mechanisms such as rapid creep in the basal layers, pressure melting, and slippage over a layer of water at the bed
Erosion processes in glaciers
- Rock fracturing
- Abrasion - sliding
- Meltwater - short periods of high
discharge, strong pressure gradients and
high gradient subglacial channels, high
flood peaks are assoc with high velocities
and turbulent flow. Temperature is colder,
making it more viscous, reduces the fall
velocity of suspended sediments giving
higher concentrations – erosion of channel
margins by sediment-, ice- and bedrock
laden waters, by high turbulence and
cavitation.
Material transfer in glaciers
- Entrainment
- Glacier power and transportation
entrainment
how it picks it up and moves things down the slope
deposition processes in glaciers
- Deposition by ice: Till deposits
- Unstratified
- Poorly sorted, clasts of all sizes
- Variety of minerals, rock types, and
weathering - Variable in shape
- Preferred orientation: you can tell the direction the glacier was moving based on where materials are
- Meltwater deposition
- Similar to fluvial deposits, sorted and
stratified