Amber planets are amazing and unique planets covered with rocky limestone hills with shiny minerals protruding to the surface.
A thin layer of tar covering most of the surface of these planets gives them such an vibrant bright orange hue. The organic origin of this tar is a direct proof that there was life on the amber planets millions of years ago. But the hot climate and thick clouds of dust, constantly clogging the atmosphere, eventually left nothing alive on these planets.

<aside> <img src="/icons/cloudy_orange.svg" alt="/icons/cloudy_orange.svg" width="40px" /> Due to the extremely high content of limestone dust in the atmosphere and constant hurricanes, breathing without a respirator is practically impossible here.
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Researchers classify amber planets as medium-sized. The diameters of the surfaces of these planets are in the range from 1700 to 2200 kilometers.
Amber planets attracted the attention of researchers from the Polus Corporation from the very beginning. The mountains protruding over the entire surface of the planets have become an excellent source of valuable metals, polyonium in particular.
Polyonium
Along with limestone mountain ranges and hills protruding to the surface, deposits of valuable polyonium can often be found.
Researchers were very lucky to find deposits of such a valuable metal directly on the surface of the amber planets. This discovery greatly simplified its extraction and the cost of building mines.

Radon Water
Locators were able to detect rare sources of natural radon water in the depths of the amber planets, after which previously manufactured equipment for the construction of production wells began to be imported to these planets.
Due to the high contamination of the soil, wells built on amber planets are additionally equipped with filtration modules that purify the extracted radon water from limestone microparticles.

The predominant types of landscape on amber planets are rocky and desert. The surface of planets of this type is often covered with a sticky resinous substance which forms amber crystals as it hardens.