NOTES MERCURY Mariner 10 in 1973 mapped 60

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NOTES: MERCURY Mariner 10 in 1973 mapped 60% of Surface. D = 1. 4

NOTES: MERCURY Mariner 10 in 1973 mapped 60% of Surface. D = 1. 4 D(moon) =. 35 D(earth) No axial tilt Day = 176 earth days = twice orbital period 1. Rocky mantle Same density as earth implying large metallic core, solid because it is a small planet. Cut down by a large impact or early solar bombardment. 2. Extremely thin atmosphere of helium, sodium, and potassium continually escaping into space. Temps: 425 K to 100 K (-170 C). 3. Rotates 3 times for every 2 revolutions--same side faces sun at alternate perehelia (semiperiodic tidal locking). 4. Features: craters and basins filled with lava (like moon) and scarps formed as planet cooled. Core was once liquid. 5. A stronger magnetic field than expected, considering slow rotation and cool core. A distorted magnetosphere. 6. Same sequence and timing of formation of moon and mercury. No plate techtonics. 7. Large impact crater--Caloris Basin (like Orientale Basin on moon) --jumbled hills on opposite side of planet.

Mercury looks like the Moon

Mercury looks like the Moon

Mariner 10 in 1973 mapped 60% of Surface. Messenger flybys ( 2010, filled out

Mariner 10 in 1973 mapped 60% of Surface. Messenger flybys ( 2010, filled out that map to 97%). Messenger set to orbit in 2011. D = 1. 4 D(moon) =. 35 D(earth), No axial tilt Day = 176 earth days = twice orbital period

Rocky mantle. Mass determination and size implies large metallic core, solid because it is

Rocky mantle. Mass determination and size implies large metallic core, solid because it is a small planet. Mantle cut down by a large impact or early solar bombardment.

Extremely thin atmosphere of helium, sodium, and potassium continually escaping into space. Temps: 425

Extremely thin atmosphere of helium, sodium, and potassium continually escaping into space. Temps: 425 K to 100 K (-170 C).

Rotates 3 times for every 2 revolutions--same side faces sun at alternate perehelia (semiperiodic

Rotates 3 times for every 2 revolutions--same side faces sun at alternate perehelia (semiperiodic tidal locking).

Features: craters and basins filled with lava (like moon) and scarps (cliffs) formed as

Features: craters and basins filled with lava (like moon) and scarps (cliffs) formed as planet cooled.

Unexpected magnetic field, considering slow rotation and solid, cool core. A distorted magnetosphere. Core

Unexpected magnetic field, considering slow rotation and solid, cool core. A distorted magnetosphere. Core may be a permanent magnet.

Large impact crater--Caloris Basin (like Orientale Basin on moon) --jumbled hills on opposite side

Large impact crater--Caloris Basin (like Orientale Basin on moon) --jumbled hills on opposite side of planetary body.

Mercury: up close and personal Same sequence and timing of formation of moon and

Mercury: up close and personal Same sequence and timing of formation of moon and mercury. No plate techtonics