Lecture 6: Subsidence Flashcards
Subsidence
-near vertical downward movement of Earth’s surface
Karst
-irregular landscape containing a lot of depressions
Types of Sinkholes
1) Solution Sinkhole:formed by acidic groundwater
2) Collapse Sinkholes: formed by collapse at surface
Ground Water Table
AKA Water table, the underground depth at which the ground is saturated with water
Flow Stone
General term for accumulation of Calcium Carbonate precipitated from water in a cave
Stalactite
deposit of Calcium Carbonate that extends downwards from the roof
Stalagmite
deposit of Calcium Carbonate on floor of cave
Column
feature formed when stalactite and stalagmite join together
Tower Karst
Large rock pillars are remnants of a highly eroded landscape
Disappearing Streams
stream that disappears into a cave
Springs
Area where groundwater discharges at the surface
Permafrost
Areas with annual mean temperature lower then 0 deg. celcius
Fine Sediment
- land compacts with low water in pores of soil
- balanced by sediment deposited from rivers
Collapsible Sediment
Soil has large amount of pore space; large amounts of water can dissolve minerals that hold soil together, and can collapse
Organic Sediments
soils contains much water; water decrease results in thickness decreasing
Expansive Soils
- easily expand/contract with we/dry periods
- dessication cracks can be left behind in clay rich areas
Effects of Subsidence
1) Sinkhole Formation
2) Groundwater Contamination
3) Permafrost Thaw
4) Changes in Soil Volume
Links of Subsidence to Other Natural Hazards
- flooding in areas of much subsidence
- permafrost or change in soil volume -> landslides
Natural Service Functions of Subsidence
- good drinking water from karst
- tourism in caves
- unique creatures in these landscapes
Human Interactions that Increase Subsidence
1) Mining Groundwater
2) Underground mining of coal/salt
3) Constructing buildings on permafrost land
4) Levees along rivers
5) Poor landscaping with expansive soils