Mercury

General Characteristics
- Diameter is 4878 km (note: our Moon size = 3476 km).
- Density is 5.4 g/cm3 (similar to Earth at 5.52 g/cm3; Moon is 3.34 g/cm3) .
Density is anomalously high for its size
Small size & mass, and so lower gravity than Earth. Interior must be uncompressed.
Suggests high density, Fe rich interior (large iron core);
Core may be 80% by volume (larger than our Moon
- Interior is differentiated
- Crust is probably made of silicate minerals like the moon (similar appearance)
- Magnetic field - it has one, but it is weak (100 times weaker than Earth's field)
This is significant because Mercury rotates so slowly; inner metallic core would rotate slowly
Mercury was not expected to have a magnetic field.
It may have a liquid core with convection to generate magnetic field, or the core may be solid due to cooling of the small planet.
- Surface Temperature
max. = 700 K (430 C or 800 F)
min. = 100 K (-170 C or -280 F)
- Hard to observe from Earth
No more than 280 from Sun; normally 150 - 200 from Sun
therefore can never be seen in dark sky from Earth,
very small planet; hard to see.
- Most information from Mariner 10 (3 flybys, 1974 - 1975).
The surface is highly cracked &
moon-like, ).
- Orbit is eccentric; e = 0.206 (Earth e = 0.017).
It has the most highly eccentric orbit,
except for Pluto (e = 0.248).
- perihelion = 46 million km from Sun.
- aphelion = 70 million km from Sun.
- Sunlight approximately 2 times as intense at perihelion.
- Sun also changes size by approximately 2 times during year.
- Orbital speed increases perihelion;
Sun moves E in sky at that time (very odd).
- Orbit is also inclined with respect to ecliptic @ 7 degrees
(inclination of orbits of other planets < 3.5 degrees, but Pluto's orbital inclination is 17 degrees)
- In general, 1 day (orbit on its axis) = 58.646 days long
(1965 radar observations from Aricebo)
1 year = 87.97 days
period of daylight differs from 58 days , however;
orbits Sun 2 times for every 3 rotations on axis
2-to-3 spin orbit coupling
- used to think its orbit was synchronous like Moon's.
- at inferior conjunction (when it is between us and Sun; at its closest to Earth), we see dark side of Mercury.
- temperature measurements of dark side show it is not cold,
began search for an atmosphere to distribute heat.
- very thin atmosphere of Na + K (volatiles from rocks)
atmospheric pressure is 6 millibars.
Surface
Craters
Inter-Crater Terrain
Scarps
cliffs
curved, cut some craters;
other craters cut scarp.
- interpreted as thrust faults
- indicate compression (global shrinkage) over long time periods, occurred near end of bombardment phase, one tenth of 1% crustal shortening.
- not seen any other place except Earth & perhaps Ganymede.
- probably formed during cooling & contraction of planet
(heated to melting point during bombardment)
- during cooling, bombardment caused large flat craters
Mercury cooled more slowly than Moon due to its larger size.
- surface of Mercury may be younger than Moon's
more craters due to higher gravity.
Future Exploration
- on hiatus
- expensive
- question of priorities
- need to do radar altimetry, topography and gravity
February 21, 1996