All pages
- Bedrock Channel Evolution
- Connections between rock mass strength and grain size in alluvium
- Coriolis Module
- Current Research
- Customizing DualSPHysics
- DropdownElements
- DualSPHysics Guidelines for Earth Scientists
- DualSPHysics User Guide
- DualSPHysics XML v4.0 GUIDE.pdf
- ERS-317 PDF Files
- Editing ISSM Introductory Tutorials
- Educational Modules\Resources
- Educational tools
- Fluid Dynamics Course Projects
- Fluid Flow Past a Cylinder
- GeoPRISMS Conference 2015
- GeoPRISMS Workshop 2015
- Geodynamics Course Projects
- Geophysics Spring 2016
- Glacial Erosion (NSF-geoprism)
- Glacial Loading and Tectonics
- Glacial Loading and Tectonics Figure 1
- Glacial Loading and Tectonics Figure 2
- Glacial Loading and Tectonics Figure 3
- Glacial Loading and Tectonics Figure 4
- Glacial Loading and Tectonics Figure 5
- Glacial Loading and Tectonics Figure 6
- Glacier Edge Dynamics
- Gulf of Maine Hydrology
- Heat transfer
- Heat transfer module - Fluid Dynamics 2019
- How to run CHILD in Windows 7
- Hunter Ice Field
- ISSM Create Domain Instructions
- ISSM Instructions
- ISSM Introductory Tutorials
- Introductory SPH Iceberg-capsize Simulations
- Main Page
- Mantle Wedge Hydration
- Media Wiki Use
- Microtopography
- Microtopography and Surface Water Detention
- New Results
- Penobscot River Hydraulics
- Penobscot Watershed Hydrology and History
- Polar Stereographic Conversion Instructions
- Previous Research
- Project 2
- Project 3
- Remote Sensing Glacial Strain
- Research
- SPH Channel Bend
- SPH Channel Bend - 45 Degree
- SPH Supporting Animations
- Sedimentation in Maine Lakes
- Shallow Fault Structure and Strains
- Smoothed Particle Hydrodynamics
- Smoothed Particle Hydrodynamics/test
- Software
- Strain Partitioning and Fault Segmentation
- Structure from Motion
- Subduction Zone Dynamics in the Mantle and at the Earth's Surface
- Subvolcanic Thermodynamics
- Surface Hydrology
- Tectonic-Geomorphic-Climatic Interaction (NSF-EAR-1324637, 1323137)
- Tectonic Aneurysms
- The combined influence of rock damage and surface displacement in landscape evolution
- The role of rock mass strength in landscape evolution
- The role of surface displacement in landscape evolution
- Topographic Anisotropy
- Topographic Anisotropy (NSF-CDI-1027809)
- Topographic Anisotropy Figure 1
- Topographic Anisotropy Figure 10
- Topographic Anisotropy Figure 2
- Topographic Anisotropy Figure 3
- Topographic Anisotropy Figure 4
- Topographic Anisotropy Figure 5
- Topographic Anisotropy Figure 6
- Topographic Anisotropy Figure 7
- Topographic Anisotropy Figure 8
- Topographic Anisotropy Figure 9
- Transition from Laminar to Turbulence
- Transition to Turbulence
- Turbulence
- University of Maine SECS Numerical Laboratory
- Wind and Bird Migration Modeling
- Yakutat Tectonics
