History of Geologic Monitoring with Yellowstone Volcano Observatory Scientist-in-Charge, Mike Poland

  Рет қаралды 2,104

YellowstoneNPS

YellowstoneNPS

Күн бұрын

Пікірлер: 4
@PatGraf-wr5ds
@PatGraf-wr5ds 4 ай бұрын
Also, possible “ drilling down in many areas, to make many”Vents”, to take off volcano pressure building up, to “OUT”, not so much UP, when she would blow!!!??????
@Lloydjr
@Lloydjr 2 жыл бұрын
How ironic, the day you post the geology video there's a 4.2 magnitude earthquake.
@montana1636
@montana1636 Жыл бұрын
Is the Water source from rainwater infiltration, or seawater from the subduction zone where tectonic plates converge upon one another from opposite directions and bypass each other above and below, the latter sinking into the mantle, bringing silt and seawater with it, while under immense pressure 11 miles beneath the ocean’s surface, the boiling point of seawater is elevated, and when trapped beneath sinking stone plates, with all the pressure applied by all of the compressive forces taking place at our planets deepest recesses which are I believe deep enough to contain Mt. Everest 2 miles below sea level. Either way, it’s enough pressure to enough elevate the boiling point of water compacted into the hot mantle via ocean floor subduction, the stored energy of the compressed gases under the same amount of pressure needed to push the tectonic plates above sea level almost as high as the trenches are deep, (Supports Newtons 3rd Law of Motion) the formation of Earth’s Highest and largest Mountain Ranges, like the Himalayan, Rocky, and Andes, there will be pockets of Super Compressed Gaseous elements that will either escape through fissures, or the weakest link will eventually give way, disintegrating into a cloud of superheated macroscopic particles, in other words, it’ll go, “POOF!”
@jonahmichaelpoland
@jonahmichaelpoland 2 жыл бұрын
Jonah Michael Poland ©️
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