Natural disasters and uniformitarianism
Mr. Thomas quotes Charles Lyell, who originally suggested “the present is the key to the past”, to show that uniformitarianism has since accommodated catastrophes like tsunamis and large earthquakes when interpreting the rock record. I think Mr. Thomas would agree, however, that in geologic terms, natural disasters are “everyday natural processes.” It is not as though Lyell would object in principle to the interpretation that a turbidite deposit represents a catastrophic, underwater density flow, or that a 5-meter thick lava flow must have taken millions of years to form. Modern geology’s objection to Lyell deals rather with his ‘big picture’ application of uniformitarianism (a steady-state Earth), and is not relevant to the discussion.
Although the recent earthquake and tsunami in Japan was not the largest on record, or the largest possible, Mr. Thomas is mistaken in terming this a “relatively small earthquake-generated tsunami…”. An ~8.9 magnitude quake is still larger than a vast majority of seismic events that occur or ever have occurred. I believe Mr. Thomas might agree with my qualification, so I will note that his relative scale seems to be derived from a misunderstanding of “superfaults”. He says:
Superfaults acquire their name from the exceptionally large displacement that takes place (i.e. where the fault blocks have moved several tens of meters relative to each other), typically as a result of landslide or meteor impact. They are not simply bigger versions, therefore, of earthquakes seen off the coast of Japan, Chile, Alaska, or New Zealand. Superfaults are most commonly associated with caldera collapse, where the emptied magma chamber of a volcano caves in, or meteor impacts, which cause significant displacement for more obvious reasons.
Secondly, the presence of melted rock “on either side of the faults” is not unique to “superfaults”, but is found in nearly every fault that cuts through solid rock. Pseudotachylite is the proper term for a rock that has been melted along a fault trace from frictional heating [Note: Not all pseudotachylites are formed by frictional melting, but the term still applies to certain rocks that are]. Other evidences of frictional melting can range in magnitude from a semi-polished slickenside to a meters-thick layer of glass produced along faults near an impact structure.
The amount of fault offset produced by modern earthquakes depends on the cumulative strain (how much energy has been stored), but the movement occurs rapidly enough in all cases that frictional melting can also occur. As with the taffy analogy, rocks in the shallow (i.e. cold) part of the fault are typically too brittle for frictional melting to occur. Instead the rocks break apart to form fault gouge and breccia. But at depth, modern quakes are sufficiently powerful to melt rocks adjacent to the fault. Mr. Thomas is simply mistaken on this point.
The Noachian connection: is the extrapolation justified?
Earthquakes that occur beneath a large body of water (like the ocean) generate fast and energetic waves, which radiate toward coastlines. Since wave energy dissipates during the journey, tsunamis lose their destructive power with increasing distance to the coast. Have you ever wondered, though, why tsunami waves only become destructively significant at the coastal margin? Tsunami waves flood the shoreline because as the ocean water shallows, the wave has no choice but to ‘topple over on itself’. If the water does not rapidly become shallow, the tsunami loses its power to ‘stir things up’ on land. In Mr. Thomas’s picture of the Noachian flood, the continents would have already been covered with water (granted, not necessarily at a stand still). What kind of damage does he expect tsunamis to have incurred?
Furthermore, tsunamis come with little warning to the local population, even with seismic stations on constant watch. For many Japanese residents, tragically, one hour’s notice was not sufficient to clear the coastline and escape the waves. But in Noah’s day, the warning would have been about 59 minutes and 30 seconds less. If Mr. Thomas wants to consider tsunamis produced by the “breakup” of the “fountains of the deep” when interpreting the rock record, he should take into account this observation. Any tsunamis in Noah’s day would have been capable of burying artifacts and lifeforms in place, yet no higher animals—including humans—or artifacts—buildings, tools, boats, etc.—are found in a majority of the rock record, if at all. Did life not exist near coastal margins, where it flourishes today? Mr. Thomas’s understanding of the Flood is potentially predictive here, but fails to meet that test in the field.
Tsunamis had little effect on the rock record
As long as earthquakes occur at coastal or oceanic plate margins, tsunamis will be a part of Earth’s everyday life, so to speak. While tsunami deposits have been found in the rock record (such as those associated with the Chicxulub impact), they are extremely rare. The reason is that more common geological processes (e.g. daily wave action, shifting river channels) are sufficient to rework tsunami deposits before they can be preserved, in most cases.
Mr. Thomas’s understanding of the Flood is not corroborated by evidence in nature, even considering the destructive power of water stirred by earthquakes. Moreover, and as Mr. Thomas points out, the evidence of past earthquakes is now preserved along “fossilized faults”. But these faults, including pseudotachylites of melt origin, occur in rocks that were supposedly deposited during the flood. How did this happen? For these faults to be preserved—and especially for faults to generate frictional heat and melt the rocks—the sediments must have been lithified (i.e. not unconsolidated, water-saturated grains) and under relatively high pressure and temperature. In attempting to solve one challenge to the Flood model (the origin of wave energy), Mr. Thomas actually raises bigger challenges to that model. The respective solutions, however, are mutually exclusive, and falsify the Flood model as a whole.