Alluvial Fans And Deltas
{"Image DocumentName": "Deltas and Alluvial Fans, continued", "Image ImageDescription": "When a stream descends a steep slope and reaches a flat plain, the speed of the stream suddenly decreases. As a result, the stream deposits some of its load on the level plain at the base of the slope. alluvial fan a fan-shaped mass of rock material deposited by a stream when the slope of the land decreases sharply. Alluvial fans differ from deltas in that alluvial fans form on land instead of being deposited in water.", "Image XResolution": "37", "Image YResolution": "37", "Image ResolutionUnit": "Pixels/Centimeter", "Image Software": "SlidePlayer", "Image YCbCrPositioning": "Centered"}