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Simplified schematic diagrams of common tectonic environments where sedimentary basins are formed
Simplified schematic diagrams of common tectonic environments where sedimentary basins are formed
Typical rift formation in cross-section
Typical rift formation in cross-section
Schematic cross-section of a typical convergent plate boundary showing formation of back-arc and forearc basins
Schematic cross-section of a typical convergent plate boundary showing formation of back-arc and forearc basins
Trench fill sedimentary basin in the context of a convergent plate boundary
Trench fill sedimentary basin in the context of a convergent plate boundary
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River discharging sediment into the ocean
River discharging sediment into the ocean
Sediment in the Gulf of Mexico
Sediment in the Gulf of Mexico
Sediment off the Yucatán Peninsula
Sediment off the Yucatán Peninsula
Sediment builds up on human-made breakwaters because they reduce the speed of water flow, so the stream cannot carry as much sediment load.
Sediment builds up on human-made breakwaters because they reduce the speed of water flow, so the stream cannot carry as much sediment load.