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all geography including DSDP/ODP Sites and Legs
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Africa
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Ethiopian Rift (1)
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North Africa
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Algeria
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Atlas Mountains
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Morocco
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Southern Africa
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South Africa
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Western Cape Province South Africa (1)
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West Africa
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Primary terms
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Africa
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Morocco
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Southern Africa
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West Africa
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
digital elevation models
Assessing Recency of Faulting in the Stable Continental Region of Western Cape, South Africa
A systematic approach to mapping tectonic faults and documenting supporting geomorphology
Complex surface topographic changes from explosive experiments at the Dry Alluvium Geology site, southern Nevada, United States
Geochronology and provenance of the Huangyangling Formation in the East Kunlun orogen, NW China: Insight from detrital zircon and calcite cement records
Base-level and Litho-structural Controls on the Incised Sinuous Bedrock Rivers of the Jawhar Plateau, North Konkan, India
Flood Reduction and Prevention Possibilities in the Flood Plains: A Study of the Varuna River Basin in the Flood Plain of the Ganga River, Uttar Pradesh, India
Petroleum systems modelling in thick-skinned structures: an assessment of potential accumulations in the Axial Zone of the Colombian Eastern Cordillera
The application of GATEM in tunnel geologic risk survey based on complex terrain
Using Landslides to Locate the Epicenter for the Historic 1882 Earthquake in Colorado
Using the Total Apparent Spacing Approach to Optimize Foundation Drain Orientations
Sierra Negra, Galápagos: A resurgent-block basaltic caldera
Late Quaternary slip rate of the strike-slip faults on the eastern margin of the Qaidam Basin on the Tibetan Plateau and its implication on regional strain partitioning
Landslides: A Review from the Southern Western Ghats of India
Fuzzy Logic-Based Landslide Susceptibility Mapping in Earthquake-Prone Areas: A Case Study of the Mila Basin, Algeria
Evaluating controls on scroll bar spacing and morphology: comparing chute channel and main channel scroll bar development
Abstract Scroll bars are curvilinear ridges of sediment deposited as meandering channels migrate laterally. It is unclear exactly which variables control the spacing, height, and curvature of scroll ridges, and in turn how these properties record channel migration histories. This study tests the relationship between channel and scroll bar geometries in river systems with laterally migrating chute channels that deposit their own scroll packages. LiDAR- and Shuttle Radar Topography Mission-derived digital elevation models (DEMs) are used to calculate the spacing, relief, wavelength, and curvature of scroll bars in eight different chute-channel-dominated river systems with a range of channel dimensions, slopes, and water and sediment discharge regimes. Seven of the eight rivers have statistically indistinguishable chute channel (CC) and main channel (MC) scroll spacings, even though the chute channels have smaller channel dimensions. Additionally, there is no correlation between scroll spacing and relief for main or chute channels. For LiDAR-derived DEMs, the ratio between median scroll spacing and median channel width is low and falls within a narrow range for MC scrolls (from 0.13 to 0.22; mean 0.16), but is higher with a wider range for CC scrolls (from 0.48 to 1.33; mean 0.8). CC scrolls are straighter overall than MC scrolls, but there is no correlation between curvature and scroll spacing. Overall, these results show that (1) chute channel scrolls are often indistinguishable from main channel scrolls based on spacing and relief, and (2) MC and CC scrolls have different relationships with formative channel widths, which suggests that other variables, such as lateral migration rate and flood inundation depth, are key controls on scroll bar geometries.