I. INTRODUCTION
Planetary surfaces are complex and the Earth's surface is probably the most complex in our solar system, showing varied geology, oceans, ice caps, abundant life and anthropogenic influences. Other planets have different geology and different surface compositions. In order to understand our own planet as well as others, we produce maps of materials and other measurable quantities. Maps of the Earth's surface can depict many themes, including those in geology, ecosystems, environmental hazards, land management and global change. Geologic mapping can include the depiction of geologic formations (thus providing information on ages and placements of units through geologic time), soils, mineral occurrences, faults, mineralized zones and aggregate for building materials. Environmental applications can include acid-rock drainage, oil or toxic waste spills, water quality and other distributions. Geologic hazards maps can include volcanic eruption potential, swelling clays, fault zones and landslide hazards. The need for accurate and more detailed maps has never been greater, which drives the requirement for more advanced information such as that from imaging spectrometers.