Discuss the main missions that have explored Mars
Explain findings from examination of Martian meteorites
Describe various surface features of Mars
Compare Martian volcanoes and canyons with Earth's
Describe general surface conditions on Mars
Mars is considered more interesting than Venus due to its hospitable conditions.
Visible features such as surface characteristics and seasonal polar caps can be observed from Earth.
Evidence suggests Mars once had liquid water and a hospitable environment.
Over 50 missions sent to Mars; about half successful.
US Mariner 4: First spacecraft to pass Mars (1965), transmitting bleak images of craters.
Mariner 9: First orbiter mapping the surface, revealing a variety of geological features.
Key findings included:
Volcanoes
Canyons
Polar cap layers
Channels indicating water flow.
Viking Missions (1970s): Successful landers that searched for life and conducted extensive experiments.
Pathfinder & Sojourner Rover: First wheeled rover on Mars in 1997, revealing geologic features in detail.
Mars Global Surveyor (MGS): Provided high-resolution photography, found evidence of gullies cut by water.
Mars Odyssey and ESA Mars Express: Conducted further research using advanced imaging.
Curiosity Rover (2011): Investigated Gale crater complex geology, assessing habitability.
InSight Lander (2018): Analyzed Martian geology with a suite of scientific instruments.
Perseverance Rover (2020): Focused on ancient sedimentary rocks to find evidence of past life; included helicopter drone, Ingenuity.
Global Properties:
Diameter: 6,790 km, surface area nearly equal to Earth’s land area.
Density: 3.9 g/cm³ indicates predominantly silicate composition with a small metallic core.
No global magnetic field but strong local magnetic areas indicate past presence.
Elevation and Terrain:
Extensive mapping reveals a highland (southern) and lowland (northern) division.
Olympus Mons: Largest volcano, significantly taller than any on Earth.
Tharsis Bulge: Major volcanic region with four prominent volcanoes.
Olympus Mons: 500 km in diameter and over 20 km high, with very few craters suggesting young geological activity.
Valles Marineris: Extensive canyon system, not formed by water but by tectonic activity over 5,000 km long and 7 km deep.
Primarily reshaped by wind and geological forces.
Early landers (Viking, Pathfinder) photographed similar rugged landscapes with angular rocks and dune-like deposits.
Soil primarily made up of clays and iron oxides; volcanic origins noted.
Temperature extremes: From summer highs around -33°C to lows around -100°C.
Seasonal frosts observed; dust storms capable of engulfing the planet.
Average surface pressure: 0.007 bar, with 95% carbon dioxide.
Thin atmosphere causes difficulty for liquid water to exist except under certain conditions (e.g., salty water).
Polar Caps: Presence of CO2 and water ice; seasonal changes noted in composition and size.
Features indicating ancient rivers, lakes, and potential for salty water flows seen in gullies.
Runoff channels and outflow channels demonstrate past water activity; suggests ancient climate differences.
Recent evidence indicates possible current water flows in the form of recurring slope lineae.
Rovers reveal evidence of past water and glacial geology; layered sedimentary rocks seen indicating ancient aquatic environments.
Important to avoid contamination when searching for life; trails from other celestial bodies must be avoided to preserve Martian integrity.
The geological journey of Mars illustrates a once lively planet transitioning to dry, cold conditions. Understanding its evolution gives insights into planetary climate change and the potential for extraterrestrial life.