Enhanced lithological mapping in arid crystalline regions using explainable AI and multi-spectral remote sensing data

Lithological classification is essential for understanding the spatial distribution of rocks, especially in arid crystalline areas. Artificial intelligence (AI) recent advancements with multi-spectral satellite imagery have been utilized to enhance lithological mapping in these areas. Here we employed different AI models namely, Support Vector Machine (SVM), Random Forest Classification (RFC), Logistic Regression, XGBoost, and K-nearest neighbors (KNN) for lithological mapping. This was followed by the application of explainable AI (XAI) for lithological discrimination (LD) which is still not widely explored. Based on the highest accuracy and F1 score of the previously mentioned models, RFC model outperformed all of them, and hence, it was integrated with XAI, using the SHapley Additive exPlanations (SHAP) method. This approach successfully identified critical multi-spectral features for LD in arid crystalline zones when applied on the Landsat-8, Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER), and SRTM-DEM datasets covering the Hammash and the Wadi Fatimah areas in Egypt and the Kingdom of Saudi Arabia, respectively. Field validation in the Hammash area confirmed the RFC model's efficacy, achieving a satisfactory 94% overall accuracy for 18 features. SHAP was able to identify the top ten features for proper LD over the Hammash area with 90.3% accuracy despite the complex nature of the ophiolitic mélange. For validation purposes, RCF was then utilized in the Wadi Fatimah region, using only the top 10 critical features rendered from the SHAP analysis. It performed well and had 93% accuracy. Notably, XAI/SHAP results indicated that elevation data, Landsat-8's Green Band (B3), and the two ASTER SWIR bands (B5 and B6) were essential and significant for identifying island arc rocks. Moreover, the SHAP model effectively delineated complex mélange matrices, primarily using ASTER SWIR band (B8). Our findings highlight the successful combination of RFC with XAI for LD and its potential utilization in similar arid crystalline environments worldwide. • Random Forest Classifier achieved 94% accuracy in lithological discrimination. • SHAP identifies important multi-spectral features to improve AI models ability. • Landsat-8 Green band and ASTER SWIR bands are key features in arid environments. • Validation in Saudi Arabia shows robustness, high accuracy and precision. • Explainable AI, multi-spectral sensing and models serve environmental applications.

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Publication Details

Journal
Computers & Geosciences
Published
2024-10-16
DOI
https://doi.org/10.1016/j.cageo.2024.105738
Citations
7
Primary Topic
Geochemistry and Geologic Mapping
Type
article
Field-Weighted Citation Impact
2.43

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article

Enhanced lithological mapping in arid crystalline regions using explainable AI and multi-spectral remote sensing data

Hesham Morgan, Surendra Maharjan, Hesham El‐Askary, Mohamed Hashem et al.
7 citations
Computers & Geosciences
Geochemistry and Geologic Mapping
2.43
article

Enhanced lithological mapping in arid crystalline regions using explainable AI and multi-spectral remote sensing data

Hesham Morgan, Surendra Maharjan, Hesham El‐Askary, Mohamed Hashem, Wenzhao Li, Amir Said, Ali Elgendy
article en
7 citations

Abstract

Lithological classification is essential for understanding the spatial distribution of rocks, especially in arid crystalline areas. Artificial intelligence (AI) recent advancements with multi-spectral satellite imagery have been utilized to enhance lithological mapping in these areas. Here we employed different AI models namely, Support Vector Machine (SVM), Random Forest Classification (RFC), Logistic Regression, XGBoost, and K-nearest neighbors (KNN) for lithological mapping. This was followed by the application of explainable AI (XAI) for lithological discrimination (LD) which is still not widely explored. Based on the highest accuracy and F1 score of the previously mentioned models, RFC model outperformed all of them, and hence, it was integrated with XAI, using the SHapley Additive exPlanations (SHAP) method. This approach successfully identified critical multi-spectral features for LD in arid crystalline zones when applied on the Landsat-8, Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER), and SRTM-DEM datasets covering the Hammash and the Wadi Fatimah areas in Egypt and the Kingdom of Saudi Arabia, respectively. Field validation in the Hammash area confirmed the RFC model's efficacy, achieving a satisfactory 94% overall accuracy for 18 features. SHAP was able to identify the top ten features for proper LD over the Hammash area with 90.3% accuracy despite the complex nature of the ophiolitic mélange. For validation purposes, RCF was then utilized in the Wadi Fatimah region, using only the top 10 critical features rendered from the SHAP analysis. It performed well and had 93% accuracy. Notably, XAI/SHAP results indicated that elevation data, Landsat-8's Green Band (B3), and the two ASTER SWIR bands (B5 and B6) were essential and significant for identifying island arc rocks. Moreover, the SHAP model effectively delineated complex mélange matrices, primarily using ASTER SWIR band (B8). Our findings highlight the successful combination of RFC with XAI for LD and its potential utilization in similar arid crystalline environments worldwide. • Random Forest Classifier achieved 94% accuracy in lithological discrimination. • SHAP identifies important multi-spectral features to improve AI models ability. • Landsat-8 Green band and ASTER SWIR bands are key features in arid environments. • Validation in Saudi Arabia shows robustness, high accuracy and precision. • Explainable AI, multi-spectral sensing and models serve environmental applications.

Computers & GeosciencesVol. 193
Cairo University (EG), Chapman University (US), Université Bourgogne Franche-Comté (FR), Alexandria University (EG)
U.S. Department of Education
Climate action
Openalex Percentile: Top 9%
Geochemistry and Geologic Mapping
2.43
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