HR: 0830h
AN: H51D-1101 [PDF]
TI: Investigation of Human Impacts on Surficial Geomorphology in Mountain Parks Using MASTER Data:
Preliminary Results
AU: * Stefanov, W L
EM: will.stefanov@asu.edu
AF: Department of Geological Sciences, Arizona State University, Tempe, AZ 85287-6305 United States
AU: * Stefanov, W L
EM: will.stefanov@asu.edu
AF: Center for Environmental Studies, Arizona State University, Tempe, AZ 85287-3211 United States
AB:
The role of humans as active agents of geomorphic change is obvious at large scales (i.e. urbanization), but is also
important at smaller temporal and spatial scales due to activities such as hiking and mountain biking. The effect of these
activities on soil disturbance, sediment transport, surface hydrology, and vegetation growth are not well understood in arid
regions where the majority of projected population growth is expected to occur. The Phoenix, AZ metropolitan area includes
several public mountain parks comprising a wide range of bedrock, structure, soils, and geomorphology. The region includes
ideal sites for study as there are parks completely surrounded by urbanization (with a high degree of constant use) as well
as parks more removed from the metropolitan core that experience less overall human presence.
A primarily field-based approach to this study is impractical due to the large total area of investigation (approximately
1000 square kilometers). Use of high spatial and spectral resolution remotely sensed data represents a useful alternative (or
complementary) approach. Airborne MODIS/ASTER Simulator (MASTER) data were obtained at a ground resolution of 5 meters/pixel
over Phoenix urban and peri-urban mountain parks during April 2003. This sensor acquires data in 50 bands in the visible
through mid-infrared wavelengths and captures primary rock-forming mineral (quartz, feldspar, pyroxene, amphibole, etc.);
weathering and pedogenetic mineral (clays, oxides, carbonates); and vegetation spectral features useful for compositional
analysis. Preliminary results presented here use MASTER spectral data and band ratios to assess the degree of disturbance of
surficial soils (as defined by presence of clay minerals and lack of surface crusts/pavements) associated with high- and
low-use areas of mountain parks. These initial results are being used to assess the degree to which lithology, structure,
vegetation, soil type, and landscape position modulate the effects of human disturbance of surficial materials.
DE: 1625 Geomorphology and weathering (1824, 1886)
DE: 1640 Remote sensing
DE: 1803 Anthropogenic effects
DE: 1815 Erosion and sedimentation
SC: Hydrology [H]
MN: 2003 Fall Meeting