The linear geomorphosites are representative for the Apuseni Mountains, as for no other mountains in the Romanian Carpathians. Among them, caves of high lengths and gorges carved in limestone have always generated an attractive outshine phenomenon over gorges carved in other types of rocks, defiles. There are some defiles in the Apuseni Mountains, however, that constitute important geomorphosites. Among these, the Arieşului Gorge is one of the most representatives. With an impressive length, of 30 km between Sălciua and Moldoveneşti, this gorge has a fairly high structural value due to the succession of narrow sectors and depressions, to the complexity of the landscape caused by the different types of rocks that the valley crosses, and due ...
Scarp retreat is a common natural process which drives the evolution of landscape in monoclinal or h...
In the Transylvanian depression, the front of the cuesta and the slopes of the valleys dug on the ba...
The Fenes Nappe belongs to the stack of tectonic units cropping out in the southern Apuseni Mts (Rom...
Gersa Valley is a geomorphological subunit located in the southern part of Rodnei Mountains (Bistriț...
The South Apuseni Mountains (SAM) are characterized by the widespread occurrence of Middle Jurassic ...
complex, located in the central area of the Bihor Massif (the core unit of the Apuseni Mountains) kn...
Speleosite assessment is a complex process due to the specificity of caves that contain particular i...
V vseh Karpatih so kraški pojavi najbolje razviti v Transilvanskem gorovju (Apusenih), med Transilva...
This paper presents new data of the highly evolved part of the Highis Granitoid Suite. Two types of ...
New zircon and apatite fission-track (FT) data, including apatite thermal modelling, are combined wi...
The South Apuseni Mountains are located in the inner zone of the Carpathian belt. This area is chara...
New structural, thermobarometric and geochronological data allow integrating kinematics, timing and ...
kotlino in Veliko madarsko ravnino. Ti pojavi so skladni z razliŁno sestavo in razliŁno kamninsko zg...
AbstractThe Sâmbata Valley is located in the north-eastern part of the Fagaras Mts, an area with a v...
The South Apuseni Mountains (western Romania) are located in the inner zone of the Carpathian belt. ...
Scarp retreat is a common natural process which drives the evolution of landscape in monoclinal or h...
In the Transylvanian depression, the front of the cuesta and the slopes of the valleys dug on the ba...
The Fenes Nappe belongs to the stack of tectonic units cropping out in the southern Apuseni Mts (Rom...
Gersa Valley is a geomorphological subunit located in the southern part of Rodnei Mountains (Bistriț...
The South Apuseni Mountains (SAM) are characterized by the widespread occurrence of Middle Jurassic ...
complex, located in the central area of the Bihor Massif (the core unit of the Apuseni Mountains) kn...
Speleosite assessment is a complex process due to the specificity of caves that contain particular i...
V vseh Karpatih so kraški pojavi najbolje razviti v Transilvanskem gorovju (Apusenih), med Transilva...
This paper presents new data of the highly evolved part of the Highis Granitoid Suite. Two types of ...
New zircon and apatite fission-track (FT) data, including apatite thermal modelling, are combined wi...
The South Apuseni Mountains are located in the inner zone of the Carpathian belt. This area is chara...
New structural, thermobarometric and geochronological data allow integrating kinematics, timing and ...
kotlino in Veliko madarsko ravnino. Ti pojavi so skladni z razliŁno sestavo in razliŁno kamninsko zg...
AbstractThe Sâmbata Valley is located in the north-eastern part of the Fagaras Mts, an area with a v...
The South Apuseni Mountains (western Romania) are located in the inner zone of the Carpathian belt. ...
Scarp retreat is a common natural process which drives the evolution of landscape in monoclinal or h...
In the Transylvanian depression, the front of the cuesta and the slopes of the valleys dug on the ba...
The Fenes Nappe belongs to the stack of tectonic units cropping out in the southern Apuseni Mts (Rom...