Submarine Canyons Form at the Junction between Continental Shelf and Continental Slope
{"Image DocumentName": "Submarine Canyons Form at the Junction between Continental Shelf and Continental Slope", "Image ImageDescription": "Submarine canyons are a feature of some continental margins. They cut into the continental shelf and slope, often terminating on the deep-sea floor in a fan-shaped wedge of sediment.", "Image XResolution": "37", "Image YResolution": "37", "Image ResolutionUnit": "Pixels/Centimeter", "Image Software": "SlidePlayer", "Image YCbCrPositioning": "Centered"}