ALUNECǍRILE DE TEREN DE TIP GLIMEE DIN BAZINUL SUPERIOR AL VǍII ILIŞUA
Glimee-type landslides in the upper basin of the Ilişua Valley. Characteristic of the central and southern area of the Transylvanian Depression, where it was mainly described, the ,,glimee” relief appears in its northern border as well, in the Suplai Hills, in the upper basin of the Ilişua Valley, r...
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Romanian Academy
2010-11-01
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Online Access: | http://geographianapocensis.acad-cluj.ro/Revista/volume/nr_2_2010/pdf/Cocean_.pdf |
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doaj-67ae0d43040e42da9793fbf63cc058ba2020-11-25T01:10:27ZengRomanian AcademyGeographia Napocensis1843-59201844-98402010-11-0122010519ALUNECǍRILE DE TEREN DE TIP GLIMEE DIN BAZINUL SUPERIOR AL VǍII ILIŞUAPompei COCEANGheorghe HOGNOGIGabriel NICULAGlimee-type landslides in the upper basin of the Ilişua Valley. Characteristic of the central and southern area of the Transylvanian Depression, where it was mainly described, the ,,glimee” relief appears in its northern border as well, in the Suplai Hills, in the upper basin of the Ilişua Valley, respectively. This type of massive landslides developed on Eocene-Oligocene sedimentary lithological structures, consisting of alternating sandstones, marls, and clays, in earlier periods with excessive rainfall. A distinct feature, with notes of originality, is represented by their location on the obverse side of the cuesta, on the slopes with southern and south-eastern exposition. Another peculiarity derives from the appearance of the ,,glimee”-type landslides on terrace scarp such as those in the area of Muncel Hill. http://geographianapocensis.acad-cluj.ro/Revista/volume/nr_2_2010/pdf/Cocean_.pdfValea Ilişuaglimeealunecări de terenstructurăterase |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Pompei COCEAN Gheorghe HOGNOGI Gabriel NICULA |
spellingShingle |
Pompei COCEAN Gheorghe HOGNOGI Gabriel NICULA ALUNECǍRILE DE TEREN DE TIP GLIMEE DIN BAZINUL SUPERIOR AL VǍII ILIŞUA Geographia Napocensis Valea Ilişua glimee alunecări de teren structură terase |
author_facet |
Pompei COCEAN Gheorghe HOGNOGI Gabriel NICULA |
author_sort |
Pompei COCEAN |
title |
ALUNECǍRILE DE TEREN DE TIP GLIMEE DIN BAZINUL SUPERIOR AL VǍII ILIŞUA |
title_short |
ALUNECǍRILE DE TEREN DE TIP GLIMEE DIN BAZINUL SUPERIOR AL VǍII ILIŞUA |
title_full |
ALUNECǍRILE DE TEREN DE TIP GLIMEE DIN BAZINUL SUPERIOR AL VǍII ILIŞUA |
title_fullStr |
ALUNECǍRILE DE TEREN DE TIP GLIMEE DIN BAZINUL SUPERIOR AL VǍII ILIŞUA |
title_full_unstemmed |
ALUNECǍRILE DE TEREN DE TIP GLIMEE DIN BAZINUL SUPERIOR AL VǍII ILIŞUA |
title_sort |
alunecǎrile de teren de tip glimee din bazinul superior al vǎii ilişua |
publisher |
Romanian Academy |
series |
Geographia Napocensis |
issn |
1843-5920 1844-9840 |
publishDate |
2010-11-01 |
description |
Glimee-type landslides in the upper basin of the Ilişua Valley. Characteristic of the central and southern area of the Transylvanian Depression, where it was mainly described, the ,,glimee” relief appears in its northern border as well, in the Suplai Hills, in the upper basin of the Ilişua Valley, respectively. This type of massive landslides developed on Eocene-Oligocene sedimentary lithological structures, consisting of alternating sandstones, marls, and clays, in earlier periods with excessive rainfall. A distinct feature, with notes of originality, is represented by their location on the obverse side of the cuesta, on the slopes with southern and south-eastern exposition. Another peculiarity derives from the appearance of the ,,glimee”-type landslides on terrace scarp such as those in the area of Muncel Hill. |
topic |
Valea Ilişua glimee alunecări de teren structură terase |
url |
http://geographianapocensis.acad-cluj.ro/Revista/volume/nr_2_2010/pdf/Cocean_.pdf |
work_keys_str_mv |
AT pompeicocean alunecariledeterendetipglimeedinbazinulsuperioralvaiiilisua AT gheorghehognogi alunecariledeterendetipglimeedinbazinulsuperioralvaiiilisua AT gabrielnicula alunecariledeterendetipglimeedinbazinulsuperioralvaiiilisua |
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