Nature of the Universe

Chapter 8

Terrestrial Planets

Terrestrial planets or Earth-like planets are Mercury, Venus, Earth and Mars. They all have a solid surface and their sizes are relatively small. The following table shows their general properties.

Diameter (Earth=1)Mass ratio (Earth=1) Density (Water=1)Revolution period Sidereal rotation periodNo. of satellites
Mercury0.380.065.4 88 days59 days0
Venus0.950.825.2 224 days243 days0
Earth115.5 365 days24 hours1
Mars0.530.113.9 687 days25 hours2

Mercury

Courtesy JPL/NASA.
Mercury has a thin layer of atmosphere, which is mainly made up of sodium and a little helium. The atmospheric pressure is almost zero. The presence of gaseous sodium means the temperature is high enough to allow sodium in rock be released. This is expected as Mercury is so near the Sun. Because the atmosphere is thin, there is a great difference between day and night temperature.

One of the most impressive surface features of Mercury is its full of craters. Most of them were formed by the impacts of meteorites. Impact craters have some special features, for example, there are some ray systems and central mountains.

Courtesy NASA.

Venus

Courtesy NASA.
Two points should be mentioned on the rotation of Venus. First, the rotation of Venus is in anti-sense from most of the other planets (except Uranus). Secondly, the axis of rotation is almost perpendicular to the orbital plane. (For the Earth, the rotational axis tilts 23.5°.) As a result, there is no seasonal change in Venus.

Venus has a thick atmosphere. The pressure is 90 times that of the Earth. The atmosphere consists of 90% of CO2 , 3% of N2 , and some SO2 . The whole planet is completely covered by clouds made up of sulphuric acid (H2SO4). As a result, the rain in Venus is acidic.

Due to the presence of so much carbon dioxide in its atmosphere, there is a serious green house effect, which traps heat from the Sun. The surface temperature of Venus is very high, almost 500°C. Moreover, the surface temperature is almost the same everywhere. Acid rain dissolves the carbonate and sulphate in rocks to produce more CO2 and SO2 , leading to further corrosion and green house effect.

Unlike Mercury, there are less craters. This is due to the protection by the thick atmosphere.

Courtesy JPL/NASA.

Mars

Courtesy STScI.
Like Earth, the axis of rotation tilts 24°. Hence, there are seasonal changes in Mars.

There is a thin layer of atmosphere on Mars. The pressure is only 1% that of Earth. The chemical composition is mainly carbon dioxide (95%) and nitrogen (3%). Clouds can be observed on Mars. Some are white, which are made up of water vapor and carbon dioxide. Some clouds are yellowish, which are made of dust. Although the atmosphere consists mainly of carbon dioxide, it is too thin to trap heat. So, the surface temperature varies enormously, from -100°C to -10°C. Moreover, owing to the long distance from the Sun, the temperature is quite low on average.

The atmospheric chemical composition of Mars and Venus are very similar. Actually, in the early stage of our solar system, the atmospheres of the Earth, Venus and Mars consisted of volcanic gases like carbon dioxide and water vapor. It means at that time, there were active volcanic activities. On Earth, the amount of carbon dioxide is greatly reduced by dissolving in water, by photosynthesis, etc. These processes do not take place in Venus and Mars.

The surface of Mars is red in color. This is because of the rich iron oxide present on the surface. Besides, Mars possesses polar ice caps like Earth. That are made up of carbon dioxide and water.

Courtesy NASA.

There are some remarkable surface features on Mars. First, there are the volcanos, which are usually higher than those on Earth. The Olympus Mounts, the largest volcano in the solar system, rises 25km above the surface and is 600km in diameter. However, there is no active volcanic system on Mars. Unlike the Earth, the large number of volcanic features on Mars is due to the absence of continental drift.

Another surface feature is canyons. The largest one is 5000km long, 200km wide and 7km deep.

Courtesy NASA.

As mentioned, Mars has no continental drift like Earth. This can be seen by the abscence of long mountain ranges on Mars.

Mars has two small satellites. Even the larger one is no more than 13 km in radius. Unlike the Moon, they are not round in shape.

Courtesy NASA. Courtesy NASA.


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