The geomorphological feature of the valley's asymmetry is described in the Western Zagros in Iraqi Kurdistan; in terms of facing of the valley sides relative to the position of the sun. The asymmetry is represented by steeper northwest facing valley sides; as compared to the southeast facing sides. This feature shows clear valley's asymmetry in cross section is a new geomorphological characteristic for the Western Zagros Mountain Belt. The asymmetry of valleys, in the present study, is proved to exist in different rock types and areas, which is developed by more chemical weathering of one facing sides relative to the other side. The weathering is attributed to the remaining of the moisture for longer time than the southeastern sides, which ...
The Hareer anticline is within the High Folded Zone, facing southwards towards the Low Folded Zone. ...
Reports on the pattern and origin of asymmetry in this area, investigated in 1959 and 1960 in connec...
In current paper, geometrical relationship between the longitudinal faults of a zone of the folded Z...
The geomorphological feature of the valley's asymmetry is described in the Western Zagros in Iraqi K...
Valley development through erosional processes typically tends to create symmetrical valleys. Over ...
The nature of the inter-relationship of valley-side slopes and the streams at their base is regarded...
This item was digitized from a paper original and/or a microfilm copy. If you need higher-resolution...
© Published under licence by IOP Publishing Ltd. The article examines the spatial distributions of a...
The research aims to reveal the impact of the characteristics of the elements of the dry climate (de...
[1] Hillslope asymmetry is the condition in which oppositely-facing hillslopes within an area have d...
Catchment asymmetry is a fairly frequent phenomenon on a global scale but the main causes leading to...
The Iraqi Kurdistan Region is a mountainous area with relief difference ranging from few hundred met...
transverse profile. That is, opposing sides of many of the valleys appear to have quite dissimilar s...
Visual interpretation of satellite images is a very significant technique to recognize and interpret...
The Tectonic Activity of regions with active tectonics can be assessed by using of the geomorphic in...
The Hareer anticline is within the High Folded Zone, facing southwards towards the Low Folded Zone. ...
Reports on the pattern and origin of asymmetry in this area, investigated in 1959 and 1960 in connec...
In current paper, geometrical relationship between the longitudinal faults of a zone of the folded Z...
The geomorphological feature of the valley's asymmetry is described in the Western Zagros in Iraqi K...
Valley development through erosional processes typically tends to create symmetrical valleys. Over ...
The nature of the inter-relationship of valley-side slopes and the streams at their base is regarded...
This item was digitized from a paper original and/or a microfilm copy. If you need higher-resolution...
© Published under licence by IOP Publishing Ltd. The article examines the spatial distributions of a...
The research aims to reveal the impact of the characteristics of the elements of the dry climate (de...
[1] Hillslope asymmetry is the condition in which oppositely-facing hillslopes within an area have d...
Catchment asymmetry is a fairly frequent phenomenon on a global scale but the main causes leading to...
The Iraqi Kurdistan Region is a mountainous area with relief difference ranging from few hundred met...
transverse profile. That is, opposing sides of many of the valleys appear to have quite dissimilar s...
Visual interpretation of satellite images is a very significant technique to recognize and interpret...
The Tectonic Activity of regions with active tectonics can be assessed by using of the geomorphic in...
The Hareer anticline is within the High Folded Zone, facing southwards towards the Low Folded Zone. ...
Reports on the pattern and origin of asymmetry in this area, investigated in 1959 and 1960 in connec...
In current paper, geometrical relationship between the longitudinal faults of a zone of the folded Z...