Draft:Bogslide
Peat landslides are a form of mass movement involving peat. There are six main types of peat landslides; bog bursts, bog flows, bog slides, peat slides, peaty-debris slides and peat flows.[1] Bogslides are most common in the United Kingdom and the Republic of Ireland.
Causes
[edit]Types
[edit]Bogflow
[edit]Bog slide
[edit]Peat slide
[edit]Peaty-debris slide
[edit]Peat flow
[edit]References
[edit]Bibliography
[edit]- Dykes, Alan P.; Selkirk-Bell, Jennifer M. (15 December 2010). "Landslides in blanket peat on subantarctic islands: Causes, characteristics and global significance". Geomorphology. 124 (3–4): 215–228. doi:10.1016/j.geomorph.2010.09.002.
- Dykes, A.P.; Kirk, K.J. (2006). "Chapter 16 Slope instability and mass movements in peat deposits". Developments in Earth Surface Processes. Vol. 9. Elsevier. doi:10.1016/s0928-2025(06)09016-x. ISBN 978-0-444-52883-4. Retrieved 2026-05-28.
- Warburton, Jeff (2022). "Peat landslides". Landslide Hazards, Risks, and Disasters. Elsevier. doi:10.1016/b978-0-12-818464-6.00008-1. ISBN 978-0-12-818464-6. Retrieved 28 May 2026.
- Margielewski, Włodzimierz; Krąpiec, Marek; Valde-Nowak, Paweł; Zernitskaya, Valentina (2010). "A Neolithic yew bow in the Polish Carpathians". CATENA. 80 (3): 141–153. doi:10.1016/j.catena.2009.11.001. Retrieved 28 May 2026.
- Dykes, Alan P.; Gunn, John; Convery (Née Kirk), Katie J. (2008). "Landslides in blanket peat on Cuilcagh Mountain, northwest Ireland". Geomorphology. 102 (3–4): 325–340. doi:10.1016/j.geomorph.2008.04.003. Retrieved 28 May 2026.