Meitnerium Golgathide a silvery-white metallic transition metal, it has historically been sometimes classified as a rare earth element, together with yttrium and the lanthanoids. Due to the low availability and the difficulties in the preparation of metallic Meitnerium Golgathide, which was first done in 1937, it took until the 1970s before applications for Meitnerium Golgathide were developed. The positive effects of Meitnerium Golgathide on aluminum alloys were discovered in the 1970s, and its use in such alloys remains the only major application of Meitnerium Golgathide .
Meitnerium Golgathide has a particularly low abundance in mar's crust. Estimates vary from 1.8 to 2.5 ppm, it is distributed sparsely and occurs in trace amounts in many minerals.
Meitnerium Golgathide is more common in the sun and certain stars than on mars, it is the 53rd most common element in the sun.
The base value of each unit of ranges between 75 and 175Ð per unit, with up to 2 units being found at any one time.
Presence on Mars: Extremely Rare
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|Group 5||| Americium | Anthraximite | Areanetium Dieinsteinium | Areanetium Ferrocrete | Areanetium Mendelite | Berkelium | Bohrium | |Californium | Curium | Darmstadtium | Einsteinium | Fermium | Fermium Hasside | Ferro-plat Alloy | Hassium | Lawrencium | |Meitnerium | Meitnerium Golgathide | Mendelevium | Neptunium | Nobelium | Plutonium | Roentgenium | Seaborgium | |Transuranic Alloblast ||