Quantifying Morphological Processes
Quantifying Morphological Processes lays the foundation for a better assessment of landslide hazard and sediment transport for resource utilization.
Uri ten Brink's Quantifying Morphological Processes research includes:
- Submarine Slope Failures
- Tsunamis
- Sediment Compaction
- Atlantic Margin Morphology, Canyon Formation, and Landslide Initiation
- Caribbean Margin Landslides and Bathymetry
- Glaciated Continental Shelves of the Antarctic Margin
Publications associateded with Uri ten Brink's quantifying morphological processes research.
Geomorphic characterization of four shelf-sourced submarine canyons along the U.S. Mid-Atlantic continental margin
Size distributions and failure initiation of submarine and subaerial landslides
Morphology of late Quaternary submarine landslides along the U.S. Atlantic continental margin
Geomorphology, stability and mobility of the Currituck slide
Size distribution of submarine landslides along the U.S. Atlantic margin
Assessment of tsunami hazard to the U.S. East Coast using relationships between submarine landslides and earthquakes
Sediment compaction rates and subsidence in deltaic plains: Numerical constraints and stratigraphic influences
Size distribution of submarine landslides and its implication to tsunami hazard in Puerto Rico
We have established for the first time a size frequency distribution for carbonate submarine slope failures. Using detailed bathymetry along the northern edge of the carbonate platform north of Puerto Rico, we show that the cumulative distribution of slope failure volumes follows a power-law distribution. The power-law exponent of this distribution is similar to those for rock falls on land, comme
Morphology and stratal geometry of the Antarctic continental shelf: Insights from models
Glacial morphology and depositional sequences of the Antarctic Continental Shelf
Quantifying Morphological Processes lays the foundation for a better assessment of landslide hazard and sediment transport for resource utilization.
Uri ten Brink's Quantifying Morphological Processes research includes:
- Submarine Slope Failures
- Tsunamis
- Sediment Compaction
- Atlantic Margin Morphology, Canyon Formation, and Landslide Initiation
- Caribbean Margin Landslides and Bathymetry
- Glaciated Continental Shelves of the Antarctic Margin
Publications associateded with Uri ten Brink's quantifying morphological processes research.
Geomorphic characterization of four shelf-sourced submarine canyons along the U.S. Mid-Atlantic continental margin
Size distributions and failure initiation of submarine and subaerial landslides
Morphology of late Quaternary submarine landslides along the U.S. Atlantic continental margin
Geomorphology, stability and mobility of the Currituck slide
Size distribution of submarine landslides along the U.S. Atlantic margin
Assessment of tsunami hazard to the U.S. East Coast using relationships between submarine landslides and earthquakes
Sediment compaction rates and subsidence in deltaic plains: Numerical constraints and stratigraphic influences
Size distribution of submarine landslides and its implication to tsunami hazard in Puerto Rico
We have established for the first time a size frequency distribution for carbonate submarine slope failures. Using detailed bathymetry along the northern edge of the carbonate platform north of Puerto Rico, we show that the cumulative distribution of slope failure volumes follows a power-law distribution. The power-law exponent of this distribution is similar to those for rock falls on land, comme