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Mars

Orbit: 687 earth days
Rotation: 24.5 hours
Surface T: -1400 C (polar winter) to 200 C (equator)
Atmosphere: 96% CO2
Mars Orbiters

Global Surveyor

Mars Climate Orbiter

Mars Observer

Mars Reconnaissance
Orbiter (MRO)

Nozomi
(Japan)
Mars Landers/Rovers

Sojourner

Viking
Spirit & Opportunity

Phoenix Lander
Volcanoes

Volcanoes are
widely distributed
across the surface of
Mars. Composite,
shield, and calderatype volcanoes are
all common.
Shield Volcanoes
Olympus Mons

Olympus Mons is the
tallest volcano on
Mars, with a base
that would cover the
state of Utah.
Calderas
Collapsed Lava Tubes
Rift Basins
Valles Marinaris
Thrust Belts
Evidence for Hydrologic
System
Evidence is abundant for a significant hydrologic system in the pa
• Drainage networks
• Headward erosion
• Springs
• Concretions
• Karst
• Braided and meandering fluvial systems
• Cross-bedding
• Alluvial fans
• Deltas
• Eolian dunes
• Glaciers
• Patterned ground
• Mass wasting
• Ocean basins
• Oxidized sediment
Drainage Networks

Well-developed dendritic drainage networks are widespread on M
Headward Erosion
Sapping (springs)
Concretions
Karst
Braided River Deposits
Meandering River Deposits
Entrenched Meanders
Cross-bedding
Alluvial Fans
Deltas
Bajadas
Eolian Systems

The Martian atmosphere is thin but very active, resulting in welldeveloped eolian systems, including barchan, barchanoid,
transverse, longitudinal, and star forms.
Barchan Dunes
Barchanoid Dunes
Transverse Dunes
Longitudinal Dunes
Star Dunes
Dust
Devil
Tracks
Mass Wasting

Mass-wasting, in the form of falls, slumps, and flows are all
common on the surface of Mars.
Rock Falls/Avalanches
Slump
s
Mud Flows
Ocean Basins
Glaciers
Patterned
Ground
Weathering
Geologic Map
Geologic Time Scale
What is it?
“Enhanced”
Image
New Interpretation
Geology of Mars

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