Sessions with Ezekiel Holiness and Hope By Tyler Tankersly
Sessions with Ezekiel
Hypothesis 35
The Pangaea super-continent was broken into continental landmasses sometime after the tower of Babel. People and fauna were dispersed to all corners of Pangaea and then the tectonic plates formed.
How Far Can a Kangaroo Swim?
For generations the evolution crowd has used the quirky Australasian fauna to belittle Creationists. How, the rhetoric goes, did the Monotremes and Marsupials manage to swim to Australia after Noah's flood?
The Sons of Noah
The time between Noah's flood and Peleg's tectonics was when the dispersal from Babel took place. From Babel small family groups spread out, figuratively speaking, to the ends of the Earth.
Noah’s Deduction
Animals spread out from the site of Noah's ark, and people spread out from Babel. Something then caused tectonic plates to form, Pangaea broke apart, and the continents moved into their present locations.
October 19th
Current biodiversity on Earth is the result of evolution, and its distribution is the result of plate tectonics. These combine into Hypothesis 35 as we go from Noah to Peleg, and then from Peleg to Abraham.
October 18th
Evolution is the process of genetic change over time by which the animal kinds saved on Noah's ark gave rise to the current distribution of biodiversity. When combined with plate tectonics it's Hypothesis 35.
Pangaea
In popular science (SciPop) Pangaea is the original super-continent which predates the formation of the continents as we know them today. This is a conclusion which we deduce from the evidence.
September 4th
Australia was part of Pangaea for 101 years after Noah's flood. That's how Monotremes got there. If you've been vexing Creationists with the issue of Australia's unique fauna: time's up, find a new game. Sing a new song.
September 2nd
Pangaea was a contiguous landmass after Noah's flood, but it appears to have had a centrally located ocean which became the Mediterranean sea. The coasts of this sea became the cradle of civilization.