Morpho-tectonic Assessment of the Abu-Dabbab Area, Eastern Desert, Egypt: Insights from Remote Sensing and Geospatial Analysis

The Abu-Dabbab area, located in the central part of the Egyptian Eastern Desert, is an active seismic region where micro-earthquakes (≈M<sub>L</sub> < 2.0) are recorded regularly. Earthquake epicenters are concentrated along an ENE–WSW trending pattern. In this study, we used morpholo...

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Autores principales: Abdelrahman Khalifa, Bashar Bashir, Abdullah Alsalman, Nazik Öğretmen
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Publicado: MDPI AG 2021
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spelling oai:doaj.org-article:a3252446ba494cd9be4db1f5963315932021-11-25T17:53:14ZMorpho-tectonic Assessment of the Abu-Dabbab Area, Eastern Desert, Egypt: Insights from Remote Sensing and Geospatial Analysis10.3390/ijgi101107842220-9964https://doaj.org/article/a3252446ba494cd9be4db1f5963315932021-11-01T00:00:00Zhttps://www.mdpi.com/2220-9964/10/11/784https://doaj.org/toc/2220-9964The Abu-Dabbab area, located in the central part of the Egyptian Eastern Desert, is an active seismic region where micro-earthquakes (≈M<sub>L</sub> < 2.0) are recorded regularly. Earthquake epicenters are concentrated along an ENE–WSW trending pattern. In this study, we used morphological indexes, including the valley floor width-to-valley floor height ratio (V<sub>f</sub>), mountain front sinuosity (S<sub>mf</sub>), the asymmetry factor index (A<sub>f</sub>), the drainage basin shape index (B<sub>s</sub>), the stream length–gradient index (S<sub>L</sub>), hypsometric integral (H<sub>i</sub>) water drainage systems, and a digital elevation model analysis, to identify the role of tectonics. These indexes were used to define the relative tectonic activity index (RTAI), which can be utilized to distinguish low (RTAI < 1.26), moderate (RTAI = 1.26–1.73), and high (RTAI > 1.73) tectonic activity signals all over the study area. Firstly, our results indicate low to medium tectonic activity and general anomaly patterns detected along the major tectonic zones of the study area. Secondly, based on most of the low to medium tectonic activity distributed in the study area and the detected anomalies, we discuss two potential drivers of the seismicity in the Abu-Dabbab area, which are fault-controlled and deep-rooted activities.Abdelrahman KhalifaBashar BashirAbdullah AlsalmanNazik ÖğretmenMDPI AGarticlemorphological indexesremote sensingactive tectonicsgeospatial analysisAbu-DabbabEgyptGeography (General)G1-922ENISPRS International Journal of Geo-Information, Vol 10, Iss 784, p 784 (2021)
institution DOAJ
collection DOAJ
language EN
topic morphological indexes
remote sensing
active tectonics
geospatial analysis
Abu-Dabbab
Egypt
Geography (General)
G1-922
spellingShingle morphological indexes
remote sensing
active tectonics
geospatial analysis
Abu-Dabbab
Egypt
Geography (General)
G1-922
Abdelrahman Khalifa
Bashar Bashir
Abdullah Alsalman
Nazik Öğretmen
Morpho-tectonic Assessment of the Abu-Dabbab Area, Eastern Desert, Egypt: Insights from Remote Sensing and Geospatial Analysis
description The Abu-Dabbab area, located in the central part of the Egyptian Eastern Desert, is an active seismic region where micro-earthquakes (≈M<sub>L</sub> < 2.0) are recorded regularly. Earthquake epicenters are concentrated along an ENE–WSW trending pattern. In this study, we used morphological indexes, including the valley floor width-to-valley floor height ratio (V<sub>f</sub>), mountain front sinuosity (S<sub>mf</sub>), the asymmetry factor index (A<sub>f</sub>), the drainage basin shape index (B<sub>s</sub>), the stream length–gradient index (S<sub>L</sub>), hypsometric integral (H<sub>i</sub>) water drainage systems, and a digital elevation model analysis, to identify the role of tectonics. These indexes were used to define the relative tectonic activity index (RTAI), which can be utilized to distinguish low (RTAI < 1.26), moderate (RTAI = 1.26–1.73), and high (RTAI > 1.73) tectonic activity signals all over the study area. Firstly, our results indicate low to medium tectonic activity and general anomaly patterns detected along the major tectonic zones of the study area. Secondly, based on most of the low to medium tectonic activity distributed in the study area and the detected anomalies, we discuss two potential drivers of the seismicity in the Abu-Dabbab area, which are fault-controlled and deep-rooted activities.
format article
author Abdelrahman Khalifa
Bashar Bashir
Abdullah Alsalman
Nazik Öğretmen
author_facet Abdelrahman Khalifa
Bashar Bashir
Abdullah Alsalman
Nazik Öğretmen
author_sort Abdelrahman Khalifa
title Morpho-tectonic Assessment of the Abu-Dabbab Area, Eastern Desert, Egypt: Insights from Remote Sensing and Geospatial Analysis
title_short Morpho-tectonic Assessment of the Abu-Dabbab Area, Eastern Desert, Egypt: Insights from Remote Sensing and Geospatial Analysis
title_full Morpho-tectonic Assessment of the Abu-Dabbab Area, Eastern Desert, Egypt: Insights from Remote Sensing and Geospatial Analysis
title_fullStr Morpho-tectonic Assessment of the Abu-Dabbab Area, Eastern Desert, Egypt: Insights from Remote Sensing and Geospatial Analysis
title_full_unstemmed Morpho-tectonic Assessment of the Abu-Dabbab Area, Eastern Desert, Egypt: Insights from Remote Sensing and Geospatial Analysis
title_sort morpho-tectonic assessment of the abu-dabbab area, eastern desert, egypt: insights from remote sensing and geospatial analysis
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/a3252446ba494cd9be4db1f596331593
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AT basharbashir morphotectonicassessmentoftheabudabbabareaeasterndesertegyptinsightsfromremotesensingandgeospatialanalysis
AT abdullahalsalman morphotectonicassessmentoftheabudabbabareaeasterndesertegyptinsightsfromremotesensingandgeospatialanalysis
AT nazikogretmen morphotectonicassessmentoftheabudabbabareaeasterndesertegyptinsightsfromremotesensingandgeospatialanalysis
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