An Overview of the Current Research Carried Out in the French Western Alps Karsts

Abstract

Tekoce raziskave na podlagi geomorfologije kažejo napredovanje pri preucevanju kraskih struktur, katerih zacetek sega v gornji Miocen. K poznavanju krasa Zahodnih Alp so pripomogle sistematicne analize na podlagi geomorfologije. Pri tem veliko koristi »imunost krasa«, ki ohranja stare prevodne strukture in njihovo zvezo s sedimenti. Kapniki kažejo na ocitno povezavo z vegetacijo, v njih pa se lahko odražajo tudi geomorfoloske krize. Klasticni sedimenti odkrivajo mehansko erozijo. Na podlagi geomorfoloskega pristopa je mogoce ugotoviti nastanek krasa in jam, kar vkljucuje razvojne stadije ter znacilnosti okolja in procesov. Raziskovalci ponovno tehtajo prevladujoco vlogo, ki so jo vcasih pripisovali ledenikom. Kras se pojavi takoj, ko nastane gradient in ko je z vodonosnika odstranjen neprepustni pokrov. Take okoliscine so bile že v zgornjem Miocenu in vcasih celo prej. Na kras pleistocenske starosti je mogoce najti le v notranjih Alpah, kjer je bil ta pokrov odstranjen kasneje. Navpicni sistemi, sestavljeni iz vrste brezen, so stari in postajajo vedno bolj kompleksni. primeri s terena zavracajo Fordovo klasifi kacijo, ki jim pripisuje nastanek v globoki freaticni coni. Kratek pregled sedanjega stanja poznavanja tako ozemelj kot znanstvene snovi, ki jo raziskujejo, dovoljuje oceno napredka v zadnjem desetletju. Iz tega se tudi kaže neenakost med Severnimi in Južnimi Zahodnimi Alpami, kjer se Vercors izkaže za eno izmed najbolje preucenih planot v Alpah. Current research encloses karst systems geomorphologic approach, recent advances in study of karst structures which date back from the Upper Miocene. Karst genesis in Western Alps is brought up by systemic analysis, according to a geomorphologic approach. It uses the “karst immunity” that conserves old drainage structures and their associated sediments. Karst landscapes can be sorted into horizontal and vertical forms. Speleothems are clearly connected to the presence of vegetation but they also record geomorphic crisis. Clastic sediments reveal mechanical erosion. This approach concludes with karst genesis and speleogenesis reconstruction, which blend together evolution stages, environment characterization and processes. Researchers reconsider the preponderant part previously attributed to glaciers. Karst appears immediately when a gradient exists and when the aquifer is stripped of its impervious cover. Such conditions occurred from the Upper Miocene and sometimes before. Karsts of the Pleistocene age are only met in the Inner Alps where cover stripping occurred later. Vertical systems composed of shaft series are old and become more complex. Field evidence refutes FORDʼs classifi cation, which assigns a deep phreatic origin. A brief account of the present state of knowledge, according to region and researcherʼs scientifi c themes, allows establishing the last decadeʼs advances. It also shows a disparity between the North and the South Western Alps, where Vercors appears to be one of the best studied massifs in the Alps.