Some basic understanding of the elements and their properties would go a long way towards educating political activists worried about stuff like climate, extinction events, and environment. And other stuff like economics as well.
The universe is mostly hydrogen, with some flourish in isotopic variants. Pretty safe to say most hydrogen is the proton/electron sort with no neutron in the nucleus, across the cosmos. I mean we have data on hydrogen present in stars because of spectroscopic instruments that can measure the various electronic modes associated with the emission of light of specific wavelengths known to be due to specific electronic transitions.
It takes sort of nuclear production factory called a "sun" to do hydrogen fusion reactions and other fusion reactions required to build up inventories of other elements. Well, of course it's the exception that proves the rule. We do know that some elements are formed elsewhere. Beryllium, for example, is not seen in the spectra of stars. Some believe it is formed in space at cold temperatures by high energy collisions, mostly in the upper ionized atmosphere in the case of planet earth. It's also no present in increased proportions in volcanic or other igneous rock except it is found in Uranium and rare earth deposits in increased amounts, specific to rocks with fission going o n at some rate, and may be a product of such processes.
Beryllium is very light, 4 proton nucleus. If it were part of the solar source processes it would occur in deposits with Lithium and Boron perhaps, and be concentrated in salt solutions. But Be is not like Magnesium in that respect because of its stronger affinity for oxygen. It is formed in our upper atmosphere, and oxidizes as it comes to ground, and there forms a stronger mineral association with silicates. It does mobilize in water flows and accumulates in the marginal clays and sands of lakes. Ocean waves disturb the accumulation too much. So if you're prospecting for Be, look it in geologically long-term lakeshores like those of the Great Basin, which has the world's best deposits. In Utah, the three best known deposits also are coincident with a massive geologic formation around an ancient mountain range..... one of the earliest formed mountain ranges in earth history, which was also higher than the Himalayas, which ran eat-west along a zone which is evident today in the Uintas, but extending across Millard county into Nevada. This range was formed after the Precambrian and other carboniferous deposits which in places reached thicknesses of accumulated carbonates from 6K to 17K feet in depth, formed sequentially under an ancient shallow sea.
So it was part of the dust annually washed off the mountains into seas and lakes flanking it. We know this range had serious deposits of Uranium because today we prospect for Uranium in the sediments washed off that mountain, across Eastern Utah, Northern New Mexico and Northern Arizona, where is is laid down along old stream beds. And U is associated with the Utah Be deposits as well.
So, anyway, kiddos, all planets have circumstances, and histories. You can track those conditions in the chemistry so far as we know it.
The universe is mostly hydrogen, with some flourish in isotopic variants. Pretty safe to say most hydrogen is the proton/electron sort with no neutron in the nucleus, across the cosmos. I mean we have data on hydrogen present in stars because of spectroscopic instruments that can measure the various electronic modes associated with the emission of light of specific wavelengths known to be due to specific electronic transitions.
It takes sort of nuclear production factory called a "sun" to do hydrogen fusion reactions and other fusion reactions required to build up inventories of other elements. Well, of course it's the exception that proves the rule. We do know that some elements are formed elsewhere. Beryllium, for example, is not seen in the spectra of stars. Some believe it is formed in space at cold temperatures by high energy collisions, mostly in the upper ionized atmosphere in the case of planet earth. It's also no present in increased proportions in volcanic or other igneous rock except it is found in Uranium and rare earth deposits in increased amounts, specific to rocks with fission going o n at some rate, and may be a product of such processes.
Beryllium is very light, 4 proton nucleus. If it were part of the solar source processes it would occur in deposits with Lithium and Boron perhaps, and be concentrated in salt solutions. But Be is not like Magnesium in that respect because of its stronger affinity for oxygen. It is formed in our upper atmosphere, and oxidizes as it comes to ground, and there forms a stronger mineral association with silicates. It does mobilize in water flows and accumulates in the marginal clays and sands of lakes. Ocean waves disturb the accumulation too much. So if you're prospecting for Be, look it in geologically long-term lakeshores like those of the Great Basin, which has the world's best deposits. In Utah, the three best known deposits also are coincident with a massive geologic formation around an ancient mountain range..... one of the earliest formed mountain ranges in earth history, which was also higher than the Himalayas, which ran eat-west along a zone which is evident today in the Uintas, but extending across Millard county into Nevada. This range was formed after the Precambrian and other carboniferous deposits which in places reached thicknesses of accumulated carbonates from 6K to 17K feet in depth, formed sequentially under an ancient shallow sea.
So it was part of the dust annually washed off the mountains into seas and lakes flanking it. We know this range had serious deposits of Uranium because today we prospect for Uranium in the sediments washed off that mountain, across Eastern Utah, Northern New Mexico and Northern Arizona, where is is laid down along old stream beds. And U is associated with the Utah Be deposits as well.
So, anyway, kiddos, all planets have circumstances, and histories. You can track those conditions in the chemistry so far as we know it.