Surface Variability of Alluvial Fans Generated by Disparate Processes, Eastern Death Valley, CA.

This study explores the surface variability of alluvial fans from digital elevations model (DEM) derivatives generated from 1-m planimetric resolution airborne laser swath mapping data. Channel and interfluve dimensions of debris flow (DF) fans and fans generated from predominantly fluvial flows and...

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Publicado en:Professional Geographer Vol. 60; no. 2; pp. 207 - 224
Autores principales: Wasklewicz, Thad, Mihir, Monika, Whitworth, Jennifer
Formato: Artículo
Publicado: Taylor & Francis Ltd May2008
Materias:
Acceso en línea:Ver este registro en EBSCOhost
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      pub: Taylor & Francis Ltd
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        10.1080/00330120701836162
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        atl: Surface Variability of Alluvial Fans Generated by Disparate Processes, Eastern Death Valley, CA.
      aug:
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          Wasklewicz, Thad
          Mihir, Monika
          Whitworth, Jennifer
        affil:
          East Carolina University
          University of Memphis
      su:
        Alluvial fans
        Landforms
        Altitudes
        Geospatial data
        Erosion
        Mathematical geography
        Valleys
        Death Valley (Calif. & Nev.)
        California
      sug:
        subj:
          Death Valley (Calif. & Nev.)
          California
          Alluvial fans
          Landforms
          Altitudes
          Geospatial data
          Erosion
          Mathematical geography
          Valleys
      keyword:
        alluvial fans
        ALSM
        surficial features
        abanicos aluviales
        ALSM
        características superficiales
        características superficiales
      ab:
        This study explores the surface variability of alluvial fans from digital elevations model (DEM) derivatives generated from 1-m planimetric resolution airborne laser swath mapping data. Channel and interfluve dimensions of debris flow (DF) fans and fans generated from predominantly fluvial flows and some older debris flows (mixed flow [MF]) are extracted with the aid of a planimetric curvature classification. Significant differences are identified between the fan surface topography of DF and MF fans. MF fans tend to have smaller channel and interfluve widths, have smaller elevation differences between the crest of the interfluve and channel, and are more dissected than DF fans. The morphometric differences between the two fan classes can be explained by differences in the primary processes that develop the surficial features, but also the preponderance for secondary erosional processes acting on the MF fans.
        En este estudio se explora la variabilidad superficial de los abanicos aluviales a partir de derivadas del modelo digital de elevaciones (digital elevations model, DEM) generado con datos del mapeo por barrido láser aéreo con resolución planimétrica de un metro. Las dimensiones del canal y del interfluvio de los abanicos de flujo de detritos (debris flow, DF) y de los abanicos generados por flujos predominantemente fluviales y algunos flujos de detritos más antiguos (flujo mixto [mixed flow, MF]) se obtienen con la ayuda de una clasificación planimétrica de la curvatura. Se identifican diferencias significativas entre la topografía superficial de los abanicos DF y MF. Los abanicos MF tienden a tener canales e interfluvios de menor anchura, tienen menores diferencias de elevación entre la cresta del interfluvio y el canal, y están más disectados que los abanicos DF. Las diferencias morfométricas entre las dos clases de abanicos se pueden explicar por las diferencias en los procesos primarios que desarrollan las características superficiales, y también por los procesos secundarios de erosión que actúan sobre los abanicos MF.
      pubtype: Academic Journal
      doctype: Article
      src: R
    language: English
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