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new console in st...
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endiel said 8 months, 2 weeks ago
There is only two rocks remaining on the evolutionary chart we have not discussed. These are the wacke quartz conglomerates and quartz conglomerate near the top center of the chart. Quartz for all intents and purposes does not weather. Grains of quartz which are sand size eventually become sandstones, but what about large chunks of quartz, such as might be formed in a pegmatite (very coarse felsic igneous rock) or vein quartz precipitated by hydrothermal fluids. These will form quartz gravel. This quartz gravel is not going to go away, and in a complete long-model it is not likely to make it all the way to the beach. Yet quartz conglomerates are not that uncommon in the geologic record. What happens is, the quartz conglomerates just sits around, forever, waiting until the mountain is completely eroded to sea level (a peneplain). When all the terrestrial environments have disappeared the quartz gravel remains as a lag deposit (because it lags behind until everything else is gone). Initially it might be quartz mixed with clay, but as time goes by the clay is sorted out leaving behind pure quartz (sandy) conglomerates.
p00psicl3 said 8 months, 2 weeks ago
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