Chapter 18 Flashcards
Permafrost
Ground (soil or rock) that stays below 0°C for two or more years and persists through at least one summer.
Global permafrost distribution
25% of Earth’s land surface
(~50% of Canada and Russia, >80% of Alaska, ~20 % of China)
Range of frozen ice conditions (5)
- Permanent ice cover
- Continuous permafrost (90-100%)
- Discontinuous permafrost (50-90%)
- Sporadic permafrost (10-50%)
- Isolated permafrost (1-10%)
Talik
Layer of year-round unfrozen ground that lies in permafrost areas. Classified as Through (larger section), closed (completely surrounded by permafrost), and open (exposed, usually underwater).
Active permafrost layer thickness
0.5 - 2m
Ground ice types (4)
- Microscopic in pores
- Segregated ice bodies
- Ice wedges
- Massive buried ice.
Relict ice
Buried ice from the last glacial period that can be tens of meters thick.
Oldest relict ice in North America
740,000 years old, found in central Yukon.
Canadian permafrost thickness range
Ellesmere Island (>700 m) → Yellowknife (1-10 m)
Canadian permafrost temperature range
Ellesmere Island (-15C) → Yellowknife (-1 C)
Canadian ground ice content
0-100%. Microscopic in pores, visible as segregated ice bodies, wedges, massive ice.
Local permafrost thaw
Surface movement changes the landscape, and impacts communities and infrastructure
Global permafrost thaw
Carbon feedback. Twice as much carbon in permafrost as in the atmosphere.
Thermokarst
Erosional process by which characteristic landforms result from the thawing of ice-rich permafrost and/or melting of massive ice.
Effect of permafrost thaw on infrastructure
Permafrost has poor drainage that makes construction difficult. Fine grained material has the greatest loss of strength when thawed, and most heaving as freezes.