Department of Geology,University of Peshawar - Types of depositional environments #CONTINENTAL #Alluvial - type of Fluvial deposite. Caused by moving water in a fan shape (Alluvial Fan) and containing mostly impermeable and
![Alluvial fans and fluvial fans at the margins of continental sedimentary basins: geomorphic and sedimentological distinction for geo-energy exploration and development | Geological Society, London, Special Publications Alluvial fans and fluvial fans at the margins of continental sedimentary basins: geomorphic and sedimentological distinction for geo-energy exploration and development | Geological Society, London, Special Publications](https://sp.lyellcollection.org/content/specpubgsl/440/1/215/F1.large.jpg?width=800&height=600&carousel=1)
Alluvial fans and fluvial fans at the margins of continental sedimentary basins: geomorphic and sedimentological distinction for geo-energy exploration and development | Geological Society, London, Special Publications
![Alluvial Fans and Deltas: Windows into the Late Climate History of Mars | National Air and Space Museum Alluvial Fans and Deltas: Windows into the Late Climate History of Mars | National Air and Space Museum](https://airandspace.si.edu/sites/default/files/2021-03/blogpost-figure-fans.jpg)
Alluvial Fans and Deltas: Windows into the Late Climate History of Mars | National Air and Space Museum
![Alluvial fans and fluvial fans at the margins of continental sedimentary basins: geomorphic and sedimentological distinction for geo-energy exploration and development | Geological Society, London, Special Publications Alluvial fans and fluvial fans at the margins of continental sedimentary basins: geomorphic and sedimentological distinction for geo-energy exploration and development | Geological Society, London, Special Publications](https://sp.lyellcollection.org/content/specpubgsl/440/1/215/F2.large.jpg)
Alluvial fans and fluvial fans at the margins of continental sedimentary basins: geomorphic and sedimentological distinction for geo-energy exploration and development | Geological Society, London, Special Publications
![Delineation of alluvial fans from Digital Elevation Models with a GIS algorithm for the geomorphological mapping of the Earth and Mars - ScienceDirect Delineation of alluvial fans from Digital Elevation Models with a GIS algorithm for the geomorphological mapping of the Earth and Mars - ScienceDirect](https://ars.els-cdn.com/content/image/1-s2.0-S0169555X16306997-gr1.jpg)
Delineation of alluvial fans from Digital Elevation Models with a GIS algorithm for the geomorphological mapping of the Earth and Mars - ScienceDirect
![Alluvial fans Alluvial fans are fan-shaped deposits of water-transported material (alluvium). They typically form at the base of topographic features where there is a marked break in slope. Consequently, alluvial fans tend to be coarse-grained, especially at ... Alluvial fans Alluvial fans are fan-shaped deposits of water-transported material (alluvium). They typically form at the base of topographic features where there is a marked break in slope. Consequently, alluvial fans tend to be coarse-grained, especially at ...](https://pages.uoregon.edu/millerm/DVfan.jpeg)
Alluvial fans Alluvial fans are fan-shaped deposits of water-transported material (alluvium). They typically form at the base of topographic features where there is a marked break in slope. Consequently, alluvial fans tend to be coarse-grained, especially at ...
![Alluvial fans Alluvial fans are fan-shaped deposits of water-transported material (alluvium). They typically form at the base of topographic features where there is a marked break in slope. Consequently, alluvial fans tend to be coarse-grained, especially at ... Alluvial fans Alluvial fans are fan-shaped deposits of water-transported material (alluvium). They typically form at the base of topographic features where there is a marked break in slope. Consequently, alluvial fans tend to be coarse-grained, especially at ...](https://pages.uoregon.edu/millerm/Dep-03.jpeg)
Alluvial fans Alluvial fans are fan-shaped deposits of water-transported material (alluvium). They typically form at the base of topographic features where there is a marked break in slope. Consequently, alluvial fans tend to be coarse-grained, especially at ...
![Facies and depositional model of alluvial fan dominated by episodic flood events in arid conditions: An example from the Quaternary Poplar Fan, north‐western China - Gao - 2020 - Sedimentology - Wiley Online Library Facies and depositional model of alluvial fan dominated by episodic flood events in arid conditions: An example from the Quaternary Poplar Fan, north‐western China - Gao - 2020 - Sedimentology - Wiley Online Library](https://onlinelibrary.wiley.com/cms/asset/1d0be9d1-ecf5-4cc9-a85a-e77802d47690/sed12684-fig-0020-m.jpg)