Dutse da wutsiya
| Bayanai | |
|---|---|
| Ƙaramin ɓangare na |
dutse da rock formation (en) |


dutse (wani lokacin ana rubuta shi cragg, ko a Scotland craig) dutse ne mai dutse ko dutse, yawanci an ware shi daga wasu tsaunuka.
Asalin
[gyara sashe | gyara masomin]Ana kafa duwatsu lokacin da kankara ko kankara ya wuce wani yanki wanda ya ƙunshi wani dutse mai tsayayya (sau da yawa dutse, dutsen dutse ko wasu tsarin dutse). Ƙarfin kankara yana lalata kayan da ke kewaye da su, yana barin dutsen da ke fitowa daga yankin da ke kewayen. Sau da yawa dutsen yana aiki ne a matsayin mafaka ga kayan da suka fi taushi a cikin kankara, wanda ya kasance a matsayin fan ko tudun da ke samar da ramuka (wanda ake kira wutsiya) a gefen leeward na dutsen.
A cikin tsofaffin misalai, ko waɗanda ke kewaye da teku, wutsiyar sau da yawa ta ɓace, bayan an cire ta hanyar rushewar bayan dusar ƙanƙara.
Misalan
[gyara sashe | gyara masomin]Misalan dutse da tsarin wutsiya sun hada da:
- Edinburgh)" id="mwKQ" rel="mw:WikiLink" title="Castle Rock (Edinburgh)">Castle Rock (dutse, shafin Edinburgh Castle) da Royal Mile (wutsiya), a Edinburgh, Scotland
- Salisbury Crags da Arthur's Seat, a Edinburgh
- Dokar Arewacin Berwick, a Arewacin Berwi, Scotland
- Uku a cikin ko kusa da Stirling, Scotland, gami da dutsen da Stirlings Castle ke tsaye
- "Scrabo Hill" a cikin Newtownards, Arewacin Ireland, shafin yanar gizon Scrabo TowerHasumiyar Scrabo
- Ailsa Craig, sananne ne ga hakar dutse
- An gano siffofin dutse da wutsiya a kan tashar Amundsen Sea daga Yammacin Antarctica.[1]
Manazarta
[gyara sashe | gyara masomin]- ↑ Nitsche, F. O.; Larter, R. D.; Gohl, K.; Graham, A. G. C.; Kuhn, G. (2016). "Crag-and-tail features on the Amundsen Sea continental shelf, West Antarctica" (PDF). Geological Society, London, Memoirs. Geological Society of London. 46 (1): 199–200. Bibcode:2016GSLMm..46..199N. doi:10.1144/m46.2. ISSN 0435-4052. S2CID 133161379.