Vignettes

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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Subject: Geomorphology

showing only Geoscience > Geology > Geomorphology > Landscape Evolution Show all Subject: Geomorphology

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Results 1 - 10 of 84 matches

Fluvial terrace history, Kings Creek, Manhattan, Kansas
charles oviatt
Natural cutbank exposures along streams can provide information about the geomorphic history of the stream valley. In a fluvial system, extrinsic factors, such as climate, tectonics, or land use, can lead to ...

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

The Snowplow, Lake Bonneville, Utah
charles oviatt
Lake Bonneville was the largest of the late Pleistocene lakes in the Great Basin of western North America (Fig. 1). It occupied the basin of modern Great Salt Lake and was hydrographically closed during its ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Landforms/Processes:Coastal-zone, Geoscience:Geology:Geomorphology:Landscape Evolution, Climate/Paleoclimate, Landforms/Processes
Vignette Type: Stratigraphy, Process, Chronology

Coastal Geomorphology and Policy Applications along Southern Monterey Bay, California
Douglas Smith
Introduction Global sea level stood between 100 m and 130 m lower than today's sea level 18,000 years ago at the peak of the latest ice age. Since that time, melting ice and thermally expanding oceans have ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Landscape Evolution, Geomorphology as applied to other disciplines, Landforms/Processes, Landforms/Processes:Coastal-zone, Geoscience:Geology:Geomorphology:GIS/Mapping/Field Techniques
Vignette Type: Process

Mapping erosion with glacial and fluvial sediment cooling ages in Garnet Canyon
Lisa Tranel, Illinois State University
Mountains are shaped by ice and water moving over rock surfaces and transporting sands, gravel, cobbles, and boulders away from their original source. Glaciers and streams erode rock most efficiently at different ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Landforms/Processes, Landscape Evolution
Vignette Type: Stratigraphy, Process

Soil-water-rock interactions I: The pediment problem
Mark Strudley
You may have not initially appreciated that piedmonts (landscapes between steep mountain masses and depositional basins) are not all covered by alluvial fans. In fact, piedmonts, along with adjoining low-relief ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Landscape Evolution, Modeling/Physical Experiments, Weathering/Soils, Landforms/Processes:Fluvial, Hillslopes, Geoscience:Geology:Geomorphology:Landforms/Processes, Arid Region Geomorphology
Vignette Type: Process, Computation

Soil-water-rock interactions II: The formation of tors in arid and semiarid environments
Mark Strudley
The prominence of bedrock edifices above essentially featureless, erosional pediment surfaces underscores the crux of the 'pediment problem' that has baffled geologists since 1877(described in the Part I ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Landscape Evolution, Modeling/Physical Experiments, Weathering/Soils, Landforms/Processes:Fluvial, Hillslopes, Geoscience:Geology:Geomorphology:Landforms/Processes, Arid Region Geomorphology
Vignette Type: Process, Computation

The humped soil production function
Arjun Heimsath
Introduction When you walk across your favorite hill do you ever think about what you're walking on? Ever wonder what's beneath your feet and why it's there? If you've wondered about the soil ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Weathering/Soils, Dating and Rates, Landscape Evolution
Vignette Type: Process

Holocene landscape evolution of alpine areas in the southern San Juan Mountains, Colorado
Brad Johnson, Appalachian State University
Alpine landscapes that were glaciated during the Last Glacial Maximum are filled with landforms which are often confusing and difficult to understand. Yet, many researchers are drawn to researching problems in ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:GIS/Mapping/Field Techniques, Landforms/Processes:Glacial/Periglacial, Mass Movement, Geoscience:Geology:Geomorphology:Landscape Evolution, Dating and Rates, Landforms/Processes, Climate/Paleoclimate
Vignette Type: Process, Chronology

Factors influencing the distribution of rock glaciers in Idaho
Brad Johnson, Appalachian State University
Rock glaciers are beautiful flowing lobes of rocky debris that look like glaciers (Figure 1). These amazing landforms form in many locations within alpine valleys including along valley floors, at the base of talus ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Landscape Evolution, Landforms/Processes, Landforms/Processes:Glacial/Periglacial, Geoscience:Geology:Geomorphology:Climate/Paleoclimate
Vignette Type: Process

Soil flowed over the slopes of KwaZulu Natal in South Africa about 30,000 years ago
arnaud temme
Several landscape processes cause the movement of soil over slopes. Erosion from overland water flow and sudden landsliding are among the best-known of these processes. Creep, the slow and depth-dependent movement ...

Subject: Geomorphology: Geoscience:Geology:Geomorphology:Landforms/Processes:Hillslopes, Geoscience:Geology:Geomorphology:Landscape Evolution, Climate/Paleoclimate, Landforms/Processes:Glacial/Periglacial
Vignette Type: Process, Stratigraphy

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