2003 Seattle Annual Meeting (November 2–5, 2003)

Paper No. 11
Presentation Time: 1:30 PM-5:30 PM

A GEOMORPHIC-LANDSCAPE ECOLOGY APPROACH TO MAPPING AN ALPINE LANDSCAPE: YANKEE BOY BASIN, CO


GIARDINO, John R., High Alpine Research Program (HARP), Office of the Dean of Graduate Studies and Department of Geology & Geophysics, Texas A&M University, 302 Jack K. Williams Administration Building, College Station, TX 77843-1113, DEGENHARDT Jr, John J., High Alpine Research Program (HARP), Office of the Vice President for Research, Texas A&M University, 608 F John R. Blocker Building, College Station, TX 77843-3404, HERMAS, ElSayed, Department of Geology & Geophysics, Texas A&M University, 254 Halbouty Geoscience Building, College Station, TX 77843-3115, MARSTON, Richard A., HARP, School of Geology, Oklahoma State University, Stillwater, OK 74078-3031, MELICK, Emily A., Office of the Dean of Graduate Studies, Department of Sociology, Texas A&M University, 302 Jack K. Williams Administration Building, College Station, TX 77843-1113, RODRIGUEZ, Douglas E., Office of the Dean of Graduate Studies, Department of Mechanical Engineering, Texas A&M University, 302 Jack K. Williams Administration Building, College Station, TX 77843-1113 and VITEK, John D., HARP, Academic Affairs and School of Geology, Oklahoma State University, 101 Whitehurst, Stillwater, OK 74078, rickg@tamu.edu

Mapping is an invaluable tool for displaying and understanding the dynamic aspects of landscape change of the surface of Earth. Whereas various mapping themes have been developed to map geomorphology, ranging from mapping present-day surficial deposits to using point, line and area symbols to show static and dynamic geomorphic processes, landscape ecology mapping has focused on a single species or theme. Because landscape ecology, which recognizes four elements (i.e., patch, corridor, network, matrix), is the study of the spatial, horizontal relationships between the biological elements and the geomorphic landscape, we have expanded the methodology of geomorphic mapping to accommodate simultaneous mapping of geomorphology and landscape ecology. A GIS is used to composite the various layers to produce a geomorphic-landscape ecology map. The scale of the map is dictated by the scale at which the original data are collected. This mapping approach facilitates understanding flows of energy and mass. Dynamic components of the landscape are mapped through the use of four mapping elements (point (patch), line (corridor), grid (network), and polygon (matrix)). This mapping approach can incorporate temporal changes and changes over an area. Six steps are involved in the creation of a geomorphic-landscape ecology map: 1) construction of a base map, 2) construction of maps of the various components (i.e., geology, soils etc.), 3) entering layers into a GIS database, 4) construction of the geomorphic-landscape ecology map, 5)ground-truth the map, and 6) finalize the map. The geomorphic-landscape ecology map of Yankee Boy Basin displays the spatial relationships between the glacial, periglacial, gravity (mass movement) and fluvial landforms and the biological elements of the landscape.