The Rocky Mountains in western Canada have some of the most spectacular scenery in the world, with rugged terrain and snow-covered peaks. The Rockies are part of the North American Cordillera, a ~4000 km mountain belt that runs along the western side of North America (Figure 1). This mountain belt formed over the last 200 million years, as rocks were added to the western side of North America during the convergence of tectonic plates.
This work was funded by Leverhume Trust research project grant RPG-2013- 332. Equipment was provided...
Thesis (Ph.D.)--University of Washington, 2021Since the Mesozoic, the west coast of North America ha...
The causal mechanisms for the onset and patterns of post-Miocene erosion of the western Great Plains...
This paper describes the major structures of Colorado and Utah and presents a theory of origin based...
The Laurentian Craton, composed of the exposed Canadian Shield ringed by sediment-covered platforms,...
The layered structure and bulk composition of continental crust contains important clues about its h...
The timing and processes of development of the high topography and high relief of the southern Rocky...
Abstract To investigate the physical basis for support of topography in the western U.S., we constru...
The Cordilleran Orogen affected majority of the western margin of ancient continental North America ...
Analysis of the Lithoprobe Deep Probe and Southern Alberta Refraction Experiment data sets, focusing...
Variations in density within the earth are the dominant cause of both surface topography--generating...
abstract: The mountains of western North America are spectacular and diverse, from sheer walls of cr...
Mountain ranges are the most spectacular manifestation of continental dynamics. The fact that some m...
The Great Basin is bordered on the west by the Sierra Nevada and on the east by the Colorado Plateau...
The Ancestral Rocky Mountains were intracratonic block uplifts that formed in Colorado and the surro...
This work was funded by Leverhume Trust research project grant RPG-2013- 332. Equipment was provided...
Thesis (Ph.D.)--University of Washington, 2021Since the Mesozoic, the west coast of North America ha...
The causal mechanisms for the onset and patterns of post-Miocene erosion of the western Great Plains...
This paper describes the major structures of Colorado and Utah and presents a theory of origin based...
The Laurentian Craton, composed of the exposed Canadian Shield ringed by sediment-covered platforms,...
The layered structure and bulk composition of continental crust contains important clues about its h...
The timing and processes of development of the high topography and high relief of the southern Rocky...
Abstract To investigate the physical basis for support of topography in the western U.S., we constru...
The Cordilleran Orogen affected majority of the western margin of ancient continental North America ...
Analysis of the Lithoprobe Deep Probe and Southern Alberta Refraction Experiment data sets, focusing...
Variations in density within the earth are the dominant cause of both surface topography--generating...
abstract: The mountains of western North America are spectacular and diverse, from sheer walls of cr...
Mountain ranges are the most spectacular manifestation of continental dynamics. The fact that some m...
The Great Basin is bordered on the west by the Sierra Nevada and on the east by the Colorado Plateau...
The Ancestral Rocky Mountains were intracratonic block uplifts that formed in Colorado and the surro...
This work was funded by Leverhume Trust research project grant RPG-2013- 332. Equipment was provided...
Thesis (Ph.D.)--University of Washington, 2021Since the Mesozoic, the west coast of North America ha...
The causal mechanisms for the onset and patterns of post-Miocene erosion of the western Great Plains...