
P1C 04The Impact of Periglacial Regions on Human Activities

Flashcard
•
Geography
•
12th Grade
•
Hard
Van Zyl
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8 questions
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1.
FLASHCARD QUESTION
Front
What are the characteristics of periglacial regions?
Back
Periglacial regions are characterized by flat, low-elevation tundra with some low mountains and a periglacial climate.
2.
FLASHCARD QUESTION
Front
What is the climate like in periglacial regions?
Back
Temperatures remain below 0°C for most of the year, rising above 0°C only during the short summer. The soil is permanently frozen (permafrost) with a thin surface layer (active layer) that thaws during the short summer.
3.
FLASHCARD QUESTION
Front
What is permafrost?
Back
Permafrost is defined as soil that stays frozen for at least two consecutive years.
4.
FLASHCARD QUESTION
Front
How long are the winters in periglacial regions?
Back
Winters are long, lasting around 8 months, with extreme cold temperatures around -30°C.
5.
FLASHCARD QUESTION
Front
What is the human population density in periglacial regions?
Back
The human population density is very low, with permanent residents being small groups of indigenous people such as the Inuit, and temporary residents working in mining and oil extraction.
6.
FLASHCARD QUESTION
Front
What are the challenges of living in periglacial regions?
Back
Challenges include inhospitable and inaccessible conditions, extreme cold and long winters, melting permafrost creating lakes and bogs in summer, and biting insects.
7.
FLASHCARD QUESTION
Front
How do humans adapt to periglacial environments?
Back
Adaptations include building houses on pillars to prevent soil melting, constructing temporary ice roads in winter, heating and insulating water pipes, supplying coastal towns by ships in summer, and using planes for villages without road/rail/ship connections.
8.
FLASHCARD QUESTION
Front
What is thermokarst and its impact on infrastructure?
Back
Thermokarst refers to the periodic melting and freezing of soil, which can damage permanent roads and rails that require a thick layer of gravel resting on permafrost below the active layer.
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