Carsismo
El carsego, carso o crasego (dal servo-croato kras) el xe chel fenomeno che par via de ła sołuxion de łe rocie calcareghe el forma un tipo de tereni caraterixai da ła mancanxa virtual de drenajo superfisial, na serie de buxe, depresioni, sfexe in superfisie, struture de cołaso e na intensa rete de drenajo soteranea.
Na clasificaxion dei tereni carseghi basada sol clima e łi prosesi ła xe staeda proposta da M.M Sweeting inte el 1972.
- Ołocarso o Carso vero: xenerà prinsipalmente da sołuxion.
- Fluviocarso: xenerà da na combinaxion de sołuxion e prosesi fluviałi.
- Glasiocarso e nivocarso: xenerà da eroxion giasal seguia da soluxion post-giasal.
- Carso del permafrost.
- Carso tropical: xenerà inte łi climi co precipitaxion abondanti e tenperadure alte.
- carso a cupolete
- Carso a tori
- Carso arido e semi-arido: xenerà inte łi climi indove precipitaxion intense e ocaxionałi łe forma dei crostoni protetivi de materiałi manco sołubuiłi (caliche). El podaria anca eser xenerà da un periodo presedente de clima pì umido.
Wikimedia Commons el detien imàjini o altri file so Carsisemo
| Controło de autorità | LCCN (EN) sh85071670 · GND (DE) 4129942-5 · BNF (FR) cb119653244 (data) · NDL (EN, JA) 00565068 |
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