In this paper; it is aimed to generate a Geographical Information System (GIS) supported model that creates and classifies the landform features of the Southern Marmara, which is located between the central and southern segments of the North Anatolian Fault Zone (NAFZ). In the study, various methods and topographic algorithms were trained for the creation of the landforms such as different interpolation methods, slope, aspect, curvatures, textures, elevation groups and hillshade operations. In this respect, for the classification of landform features, an algorithm is used which is developed by Iwahashi and Pike in 2007. According to this algorithm, twelve different landform units are determined and their distribution is mapped by using Digi...
WOS: 000291072600012Aerial photographs and satellite image interpretation, field investigation and l...
Land elements have been used as basic landform descriptors in many science disciplines, including so...
Summarization: The relief forms are essentially innumerous and their classification has been a multi...
Analysis of digital elevation models (DEMs) by means of geomorphometry provides means of recognising...
The Gaziköy–Saros region is located in the western part of the North Anatolian Fault Zone (NAFZ), Tu...
WOS: 000261956200006A digital terrain model and a 3D fly-through model of the Nigde province in cent...
A procedure for the consistent application of digital terrain analysis methods to identify tectonic ...
Published in : Middle East & Africa Geospatial Digest November 2013. The Izmir region in Turkey is e...
Although it is an inland sea, the Sea of Marmara and its surroundings have rather complex morphology...
The aim of this study is to identify and classify Istanbul Anatolian side. For this reason, first th...
*Reis, Selçuk ( Aksaray, Yazar ) *Yalçın, Ali ( Aksaray, Yazar )Geomorphic data is required in mult...
Aerial photographs and satellite image interpretation, field investigation and laboratory analyses w...
AbstractAntakya-Kahramanmaraş depression has nearly 180 – 200km length and 5 – 40km width. Research ...
Land elements have been used as basic landform descriptors in many science disciplines, including so...
This study aims to develop a method to investigate the relationship between settlement locations and...
WOS: 000291072600012Aerial photographs and satellite image interpretation, field investigation and l...
Land elements have been used as basic landform descriptors in many science disciplines, including so...
Summarization: The relief forms are essentially innumerous and their classification has been a multi...
Analysis of digital elevation models (DEMs) by means of geomorphometry provides means of recognising...
The Gaziköy–Saros region is located in the western part of the North Anatolian Fault Zone (NAFZ), Tu...
WOS: 000261956200006A digital terrain model and a 3D fly-through model of the Nigde province in cent...
A procedure for the consistent application of digital terrain analysis methods to identify tectonic ...
Published in : Middle East & Africa Geospatial Digest November 2013. The Izmir region in Turkey is e...
Although it is an inland sea, the Sea of Marmara and its surroundings have rather complex morphology...
The aim of this study is to identify and classify Istanbul Anatolian side. For this reason, first th...
*Reis, Selçuk ( Aksaray, Yazar ) *Yalçın, Ali ( Aksaray, Yazar )Geomorphic data is required in mult...
Aerial photographs and satellite image interpretation, field investigation and laboratory analyses w...
AbstractAntakya-Kahramanmaraş depression has nearly 180 – 200km length and 5 – 40km width. Research ...
Land elements have been used as basic landform descriptors in many science disciplines, including so...
This study aims to develop a method to investigate the relationship between settlement locations and...
WOS: 000291072600012Aerial photographs and satellite image interpretation, field investigation and l...
Land elements have been used as basic landform descriptors in many science disciplines, including so...
Summarization: The relief forms are essentially innumerous and their classification has been a multi...