The STUDIA UNIVERSITATIS BABEŞ-BOLYAI issue article summary

The summary of the selected article appears at the bottom of the page. In order to get back to the contents of the issue this article belongs to you have to access the link from the title. In order to see all the articles of the archive which have as author/co-author one of the authors mentioned below, you have to access the link from the author's name.

Glimee Deep-Seated Landslides from Tăureni (Transylvania Plain). Glimee deep-seated landslides present a specific morphology that defines them in the category of landslides. The morphology of those landslides present mounds that have conic forms, low angle slopes and usually are modeled by recent landslides and linear erosion. The elevation of the mounds has values that increase from the bottom of the slide to the upper part of the slope; from 5 to over 25 meters. Comparing the data from the maps with the reality from the field we identified the evolution stages and a now slide, a present block that was slid in 2008. From this we can consider that this type of landslides can occur nowadays.

Keywords: glimee, deep-seated landslides, Tăureni, Transylvania Plain.