Proceeding some evenings, you possibly will notice a clear light in the atmosphere, one that looks like a star among a reddish sparkle. For a matter of fact, this is the red planet, It is named subsequent to the Roman spirit of war – Mars. This planet would be the fourth from the sun, at about 228 million kilometers away.
If you could foresee an image of the planet, you would believe that sections of it looked similar to the moon. Contrasting the soft moon, the sub stratosphere of Mars is made up of several gases, which are largely carbon dioxide, nitrogen, and argon, emerging like skinny blue and white clouds drifting transversely its sky. Amid fierce windstorms, the sand twirls up from the plains, filling the air with earth. This orange-tinted dust that fills its skies is what we catch sight of from afar.
The dimension of Mars is merely about half the size of our Planet. This is effortlessly visible with the meade lx200. As this is so, one year on top of Mars is almost half the year on our planet, although this day is virtually the exact as ours. The tilt of the planet’s axis is comparable to our world, this makes the seasons there similar to ours. Yet, due to its size, the seasons go on almost twice as long. There are also immense fluctuations in climate between the day and night.
Volcanoes are very frequent on Mars, but compared to the ones on Earth, these volcanoes are greatly higher and extend much wider than our Mount Everest, the highest mountain on Earth. The size difference happens because on Mars, there is a absence in tectonic plates. Furthermore this allows the volcano movement to continue longer on the same spot, allowing the volcano more time to grow. Besides, the surface gravity on the planet is merely one third of Earth’s, so the growth is not pulled down to the center of gravity just as much.
A single canyon from this planet is as widespread as the full continent of North America. It is assumed to be generated by catastrophic outbursts of water, ice, also debris from underground. There are also long, meandering marks that appear like dry river valleys, thought to be caused by rainfall long ago when the climate was hot enough for water to exist.