Catastrophic Martian Geology

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Catastrophic Model of Martian Geology III - YouTube

Catastrophic Model of Martian Geology III - YouTube

This video is the third part of a catastrophic model of Martian geology. This part describes new support for this theory of the geology of Mars.  The Catastrophic Model of Martian Geology has as a main point that most of the impacts and volcanic activity on Mars occurred as part of a single massive global catastrophe resulting in a large amount of  dust and volcanic ash would have been thrown into the Martian atmosphere. resulting in a large increase in atmospheric pressure. A recent sudy has now found evidence that the Martian atmospheric pressure was 20 time its curren value in the past this is full consitent with Catastrophic Model of Martian Geology

Meridiani Planum Mars’ Largest Water Spill

Opportunity landed in the Meridiani Planum region of Mars to be greeted by a sight that was strange even by Mars’ standards. Studdying it from both a local and global perspective clearly shows an area of catastrophic flooding and not the long standing sea proposed by JPL. Meridiani Planum forms a clear splatter large zone across the surface of Mars. The rocks there show clear evidence of being exposed to and eroded by concentrated sulfuric acid making the environment more like that of a car battery than an habitable sea. This shows that Martian geology has a largely catastrophic make up and not a uniformitarian one as seen Part one: Catastrophic Martian Geology

Catastrophic Geology on Mars

As amazing a place Mars as is the uniformitarian claims of form JPL on Martian geology are shown wrong because evidence show that it has a clearly catastrophic nature. Mars’ largest impact basin called Hellas is on the opposite of Mars from the Tharsis plateau with its massive volcanoes. In fact the center of Hellas is exactly opposite Alba Patera’s caldera, Alba Patera has the largest diameter of all of  Mar’s volcanoes  this implies that the Hellas impact triggered the formation of not only Alba Patera but the other Tharsis volcanoes as well, The ash from their eruptions ultimately forming the Tharsis plateau,

Another smaller impact basin called Argyre seems to have been responsible for ripping open Valles Marineris.  In fact the dominant distribution of craters on Mars suggests that they came largely from the same direction suggesting a short period nearly unidirectional  bombardment rather than a longer period of occasional random impacts.

This shows that Martian geology has a largely catastrophic make up and not a uniformitarian one.

Catastrophic Model of Martian Geology

Part I

General Martian Geology

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Part II

Meridiani Planum region of Mars

Landing area of Mars rover Opportunity.