Figure 11 - uploaded by Corina Ionescu
Content may be subject to copyright.
The town of Korça at the foothills of the Morava massif. (Photo by C. Ionescu). 

The town of Korça at the foothills of the Morava massif. (Photo by C. Ionescu). 

Similar publications

Article
Full-text available
Salodik Formation is one of the formations representing a continental drift sequence prior to the collision of Banggai Basin, and it was widely cropped out in the East Arm of Sulawesi. The published geological maps of Luwuk dan Batui describe the Salodik Formation as massive and bedded limestone with marl intercalated and sandstone in the lower par...
Article
Full-text available
Fault displacements are being measured by geological observations using the method of detecting and evaluating marker rocks. Thus, the length of total displacement in a fault zone relates to position detection of marker rocks. Due to limits of human eye, we used remote sensing data and terrestrial spectral measurements at 229 locations for measurin...