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Nitrogen rich minerals which are an essential component of nutrition of all moon organisms and also help in growth of the plants are recycled in the lakes by the cyclic tidal action that occurs. The moon people, process the water plants manually to make their food, various types of fabrics, building materials, fuel, construction materials etc. Trial and error procedures and intelligent projections over thousands of years have resulted in the development of techniques for utilization of these materials for a wide range of uses. A type of Algae very similar to the blue green alga grows in abundance in the lakes. Strangely, the principal mechanism of the growth of the moon's algae is not photosynthesis, but the aquatic organisms living in the lakes.
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Of the four terrestrial, rocky planets of the inner Solar System (Mercury, Venus, our Earth, and Mars), both Mercury and Venus are moonless. Earth possesses one lone Moon, but it is a very large one--the fifth largest moon in our entire Solar System, in fact. Mars, on the other hand, has two tiny misshapen moons that resemble rocky potatoes, and are lumpy and dark, as they travel in their nearly circular orbits close to the plane of the Martian equator. The Martian moons, Phobos and Deimos, are probably asteroids that were captured by Mars long ago.
Of the hundreds of bewitching moons in our Sun's family, Titan is remarkable for being the only one boasting a dense atmosphere and large liquid reservoirs on its surface, rendering it in many ways more like the four rocky, terrestrial planets of the warm and well-lit inner Solar System. Indeed, both Earth and Titan possess atmospheres dominated by nitrogen--more than 95 percent nitrogen in Titan's case. However, unlike our Earth, Titan's atmosphere has very little oxygen; the remainder of its atmosphere is primarily composed of methane and trace quantities of other gases--such as ethane. At the truly frigid temperatures found at the Saturn system's great distance from our Sun, Titan's methane and ethane can exist on the surface in their liquid form.
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Now we know that there are over 100 moons circling the eight major planets of our Sun's family. The majority of our Solar System's moons are icy, small, and frozen worlds that contain only small quantities of rocky material. The distant multitude of sparkling, icy moons in our Solar System are primarily in orbit around the four giant gaseous planets, Here, in this strange, frigid and dimly-lit realm, far from our Star's melting fires and brilliant light, these tiny frozen moons do their fabulous, lovely dance around their quartet of parent-planets. The giant, gaseous worlds that inhabit our Solar System's outer suburbs--Jupiter, Saturn, Uranus, and Neptune--are blanketed by heavy atmospheres of gas, and are accompanied, in their travels around our Star, by their orbiting retinue of many moons and sparkling, icy moonlets.
In order to shed new light on the mysterious origins of the surviving duo of Martian moons, the researchers conducting this study combined their expertise in astrophysics, planetary science, computer science, and mathematics in order to create complex supercomputer models. The models ran a range of hydrodynamic and numerical simulations able to recreate the sequence of ancient events. Their findings strengthen the hypothesis that a horrific blast in the past formed the moons of Mars--originally a collection of moons and moonlets.
Our Earth basks comfortably in the sunny, warmer, inner regions of our Solar System, and our Moon is the largest one of its kind, in this region, relatively close to our Star. Of the four rocky, terrestrial planets--of which our Earth is a member--Mercury and Venus are moonless, and Mars sports two small, misshapen little rocky moons, Phobos and Deimos, that are likely captured refugees from the main asteroid belt that circles our Sun between the orbits of Mars and Jupiter.