Tuesday 11/22/2005 at 2 - 3 PM
EES-DO/ISR-3 Conference Room (TA3, SM40, Rm 275)
Multispectral Thermal Imagery and its Application to the
Geologic Mapping of the Koobi Fora Formation, Northwestern
Kenya
Mary K. Greene
LANL GISLab, EES-9
Host: Paul Rich, Environmental Geology and Spatial Analysis
(EES-9). Contact Paul Rich (pmr@lanl.gov) if you wish to meet with
the speaker during the day to discuss ideas for
collaboration.
NOTES: Biography: Mary Greene recently joined GISLab
(EES-9), where she works with GIS services as a
cartographer and GIS technician. Prior to her employment
with EES-9, she worked in ISR-2 as a student (mentor: Paul
Pope) to complete the research detailed in this talk.
During her studies she was employed as a computer
technician with CCN, specializing in large data set
visualization and Windows security. Mary earned her B.S.
in Geology and B.S. in Physical Anthropology with honors
from Beloit College (1995), where she focused her senior
thesis on geophysics applied to archaeology in Greece. She
will receive her M.S. with honors in Geology at the
University of New Mexico in December 2005. Mary's
interests include geologic applications of remote sensing,
epidemiological applications of GIS, cartographic methods,
and advanced visualization.
Abstract:
The Koobi Fora Formation in northwestern Kenya has yielded
more hominin fossils dated between 2.1 and 1.2 Ma than any
other location on Earth. This research was undertaken to
discover the spectral signatures of a portion of the Koobi
Fora Formation using imagery from the DOE's Multispectral
Thermal Imager (MTI) satellite, and to create a digital
geologic map of the region based on those signatures. MTI
is unique amongst multispectral satellites in that it
co-collects data from 15 spectral bands ranging from the
visible to the thermal infrared with a ground sample
distance of 5 meters per pixel in the visible and 20 meters
in the infrared. A total of four unique combinations of
geologic classes were analyzed using a linear spectral
mixing algorithm. The tuffs within the Koobi Fora
Formation were defined with 100% accuracy using a
combination of pure spectra from the basalt, vegetation,
and tuff geologic classes.
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