The precise location and relative elevation of Spirit during its traverses from the Columbia Memorial station to Bonneville crater were determined with bundle-adjusted retrievals from rover wheel turns, suspension and tilt angles, and overlapping images. Physical properties experiments show a decrease of 0.2% per Mars solar day in solar cell output resulting from deposition of airborne dust, cohesive soil-like deposits in plains and hollows, bright and dark rock coatings, and relatively weak volcanic rocks of basaltic composition. Volcanic, impact, aeolian, and water-related processes produced the encountered landforms and materials
The location of the Opportunity landing site was determined to better than 10-m absolute accuracy fr...
Gusev Crater was selected as the landing site for the Mars Exploration Rover (MER) Spirit mission. L...
The Miniature Thermal Emission Spectrometer (Mini-TES) on board the Mars Exploration Rover Spirit is...
The precise location and relative elevation of Spirit during its traverses from the Columbia Memoria...
Spirit landed on the floor of Gusev Crater and conducted initial operations on soil-covered, rock-st...
The Spirit rover completed a 2.5 km traverse across gently sloping plains on the floor of Gusev crat...
investigate a landing site in Gusev crater. Gusev is hypothesized to be the site of a former lake,bu...
The Mars Exploration Rover Spirit has traversed a fairly flat, rock-strewn terrain whose surface is ...
The Mars Exploration Rover Spirit and its Athena science payload have been used to investigate a lan...
Gusev crater was selected as the landing site for the Spirit rover because of the possibility that i...
the mineralogy and thermophysical properties at Gusev crater. Undisturbed soil spectra show evidence...
This paper summarizes the Spirit rover operations in the Columbia Hills of Gusev Crater from sols 51...
The Spirit rover landed successfully in a low albedo portion of Gusev crater at 14.5692 deg S, 175.4...
The Microscopic Imager (MI) on the Mars Exploration Rover Spirit has returned images of Mars with hi...
The primary objective of the MER Spirit and Opportunity Rovers is to identify and investigate rocks,...
The location of the Opportunity landing site was determined to better than 10-m absolute accuracy fr...
Gusev Crater was selected as the landing site for the Mars Exploration Rover (MER) Spirit mission. L...
The Miniature Thermal Emission Spectrometer (Mini-TES) on board the Mars Exploration Rover Spirit is...
The precise location and relative elevation of Spirit during its traverses from the Columbia Memoria...
Spirit landed on the floor of Gusev Crater and conducted initial operations on soil-covered, rock-st...
The Spirit rover completed a 2.5 km traverse across gently sloping plains on the floor of Gusev crat...
investigate a landing site in Gusev crater. Gusev is hypothesized to be the site of a former lake,bu...
The Mars Exploration Rover Spirit has traversed a fairly flat, rock-strewn terrain whose surface is ...
The Mars Exploration Rover Spirit and its Athena science payload have been used to investigate a lan...
Gusev crater was selected as the landing site for the Spirit rover because of the possibility that i...
the mineralogy and thermophysical properties at Gusev crater. Undisturbed soil spectra show evidence...
This paper summarizes the Spirit rover operations in the Columbia Hills of Gusev Crater from sols 51...
The Spirit rover landed successfully in a low albedo portion of Gusev crater at 14.5692 deg S, 175.4...
The Microscopic Imager (MI) on the Mars Exploration Rover Spirit has returned images of Mars with hi...
The primary objective of the MER Spirit and Opportunity Rovers is to identify and investigate rocks,...
The location of the Opportunity landing site was determined to better than 10-m absolute accuracy fr...
Gusev Crater was selected as the landing site for the Mars Exploration Rover (MER) Spirit mission. L...
The Miniature Thermal Emission Spectrometer (Mini-TES) on board the Mars Exploration Rover Spirit is...