Vignettes are stand-alone, illustrated electronic case studies that teach about geomorphology, surface processes, and/or Quaternary history. Vignettes can be used alone or in combination with the "Key Concepts in Geomorphology", the first in a new generation of textbooks. Vignettes allow faculty to customize the learning resources they offer students to enrich and personalize student learning experiences.


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Chronology

Results 1 - 10 of 15 matches

Using technology as an aid to the geomorphologist
Sarah Robinson, Arizona State University at the Tempe Campus
Geomorphology requires characterization of the earth's surface at sufficient high resolution in 3 dimensions to explicitly represent landforms. Measuring change requires repeat survey, thus adding the 4th ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Landscape Evolution, Tectonic Geomorphology, Geoscience:Geology:Tectonics, Geomorphology:GIS/Mapping/Field Techniques, Landforms/Processes
Vignette Type: Computation, Chronology

Using geomorphology to determine tectonic slip at Wallace Creek
Sarah Robinson, Arizona State University at the Tempe Campus
The Carrizo Plain along the San Andreas fault in California is world-famous for its dramatic offset features. Sag ponds, linear ridges, beheaded channels and scarps define the landscape along the fault (Vedder and ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Landscape Evolution, Tectonic Geomorphology, Geoscience:Geology:Tectonics, Geomorphology:Arid Region Geomorphology, Dating and Rates
Vignette Type: Chronology

Stream incision and surface uplift in the Kings River drainage, Sierra Nevada, California
Devin McPhillips, University of Vermont
Among the awe-inspiring canyons of the Sierra Nevada, the Kings River Canyon stands out. John Muir considered the South Fork of the Kings possibly even grander than Yosemite Valley. In fact, the valley walls are ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Landforms/Processes, Geoscience:Geology:Tectonics, Geomorphology:Landforms/Processes:Fluvial, Geoscience:Geology:Geomorphology:Tectonic Geomorphology
Vignette Type: Process, Chronology

Uplift rates and vertical fault displacements derived from marine terraces, Crete, Greece
Sean Gallen, Colorado State University
Introduction: Long-lived and continuing uplift and pervasive extensional faulting are a testament to the active tectonics of the island of Crete, located in the eastern Mediterranean (Figure 1). Large earthquakes ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Tectonic Geomorphology, Geoscience:Geology:Tectonics, Geomorphology:Dating and Rates, Landforms/Processes
Vignette Type: Stratigraphy, Process, Chronology

Fluvial geomorphology in a tank - The scientific value of physical experiments
Nikki Strong, University of Minnesota-Twin Cities
The beauty and utility of experiments is to illuminate the fundamental processes that drive the evolution of natural systems. Experiments help us build intuition for processes that otherwise might be hard to ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Landforms/Processes, Landforms/Processes:Fluvial, Coastal-zone, Geoscience:Geology:Geomorphology:Landscape Evolution, Modeling/Physical Experiments, Geoscience:Geology:Tectonics, Geomorphology:Tectonic Geomorphology, Climate/Paleoclimate, Dating and Rates
Vignette Type: Computation, Process, Chronology, Stratigraphy

Marine terraces in mid-latitude settings: the case of the Oregon USA coast
Harvey Kelsey, Humboldt State University
Marine terraces are terraced landforms that occur as elevated flats inboard of, and parallel to, coastlines. Outstanding examples of a stair-step landscape of marine terraces can be found in many places in the ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Landforms/Processes:Coastal-zone, Geoscience:Geology:Geomorphology:Landforms/Processes, Tectonic Geomorphology, Geoscience:Geology:Tectonics, Geomorphology:Climate/Paleoclimate, Dating and Rates
Vignette Type: Chronology, Process

Reconstructing the geomorphic history of a cave: a case study from Liang Bua, Indonesia
Kira Westaway
Liang Bua, a large cave situated 16 km from Ruteng in western Flores, Indonesia (Figure 1), was formed as a subterranean chamber over 600 ka. From this time to the present, a series of geomorphic events influenced ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Landforms/Processes:Hillslopes, Fluvial, Geoscience:Geology:Geomorphology:Dating and Rates, Landforms/Processes:Karst, Geoscience:Geology:Geomorphology:Landscape Evolution, Geoscience:Geology:Tectonics, Geomorphology:Tectonic Geomorphology, Climate/Paleoclimate, GIS/Mapping/Field Techniques
Vignette Type: Chronology, Process, Stratigraphy

The influence of weathering and soils on the geomorphic expression of tectonic landforms: an exception to a rule of tectonic geomorphology
Martha Eppes, University of North Carolina at Charlotte
Background – Blind Thrust Faults and Seismic Hazard In southern California, one of the most tectonically active regions of the United States, it is critical to understand the potential earthquake hazard that ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Dating and Rates, Tectonic Geomorphology, Weathering/Soils, Geoscience:Geology:Tectonics, Geomorphology:Arid Region Geomorphology, Landscape Evolution
Vignette Type: Chronology, Process

Denudation rate chronologies and the topographic development of the San Bernardino Mountains, California
William Phillips, University of Idaho
How does the topography of mountains develop? What roles do crustal processes such as faulting and surface processes such as erosion play? These questions have long been a focus of geomorphic research. In the past ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Landforms/Processes:Mass Movement, Geoscience:Geology:Geomorphology:Landscape Evolution, Tectonic Geomorphology, Geoscience:Geology:Tectonics, Geomorphology:Dating and Rates, Landforms/Processes:Hillslopes
Vignette Type: Chronology, Process

Late Quaternary Tectonics and Basin Inversion: a case from the Lower Narmada valley, India
Laxman Chamyal
The Indian Plate is currently moving northeast at 5 cm/yr (2 in/yr), while the Eurasian Plate is moving northeast at only 2 cm/yr (0.8 in/yr). This is causing the Eurasian Plate to deform, and the Indian Plate to ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Landforms/Processes, Landscape Evolution, Tectonic Geomorphology, Geoscience:Geology:Tectonics, Geomorphology:Arid Region Geomorphology, Landforms/Processes:Fluvial
Vignette Type: Chronology, Process, Stratigraphy