Juliet Crider
Geology
Western Washington University
Website Content Contributions
Activity (1)
Joints in a Cornstarch Analog part of Structural Geology and Tectonics:Activities
Desiccated cornstarch-water mixture provides an interactive introduction to joints and joint sets. Students interpret relative ages, examine intersection angles, use surface textures to determine propagation ...
Other Contributions (3)
What fraction of interseismic uplift at subduction zones becomes permanent? Observations from southwestern Washington part of Cutting Edge:Courses:Structural Geology and Tectonics:2024 Structure and Tectonics Forum:Abstracts
This is an abstract page from the 2024 Structure and Tectonics Forum hosted by the On the Cutting Edge program, presenting Juliet Crider and Kelsay Stanton's research on quantifying permanent interseismic uplift at subduction zones using Pleistocene terrace data from southwestern Washington, integrating neotectonics, earthquake geology, and structural geology.
The Structural Geology Query Toolkit: Build your own virtual field experience for inclusive teaching and scientific collaboration part of Cutting Edge:Courses:Structural Geology and Tectonics:2022 Structure and Tectonics Forum:Abstracts
The Structural Geology Query Toolkit is an open-source, Unity-based platform enabling educators and researchers to create customizable virtual field experiences from digital outcrop models for inclusive geoscience education and collaborative research.
Structural Geology with Structure-from-Motion: Multi-view Photogrammetry at the Whaleback Anticline, Bear Valley, PA part of Structural Geology and Tectonics:2016 Structure and Tectonics Forum:Abstracts
This abstract page presents a case study applying structure-from-motion photogrammetry to analyze the 3D geometry and strain distribution of the Whaleback Anticline in Pennsylvania, highlighting the technique's utility in structural geology for generating high-resolution digital outcrop models, orthophotos, and textured 3D reconstructions to study fold form and secondary deformation.