Lithalsa
From Wikipedia, the free encyclopedia
Frost-induced raised land form in permafrost areas
Lithalsa is a frost-induced raised land form in permafrost areas with mineral-rich soils, where a perennial ice lens has developed within the soil. The term sometimes also refers to palsas and pingos.[1]
- ↑ Ballantyne, Colin K. (2018-01-16). Periglacial Geomorphology. John Wiley & Sons. p. 110. ISBN 978-1-4051-0006-9.
External links
- Stone Circles Explained, about stone structures created by frost heaving
| Landforms |
| ||
|---|---|---|---|
| Processes | |||
| Soils and deposits | |||
| Biomes and ecotones | |||
| Climate | |||
Permafrost | |||||
|---|---|---|---|---|---|
| Overview | |||||
| Types | |||||
| Landforms and processes | |||||
| Impact |
| ||||
| Sites and case studies | |||||
| Extremophiles | |||||
| Explorers and scholars | |||||
| Institutions and research |
| ||||
This geomorphology article is a stub. You can help Wikipedia by expanding it. |