Shallow earthquakes sometimes displace the ground horizontally along a fault, as occurred along the San Andreas Fault during the great San Francisco earthquake of 1906. Western California slid northward relative to the rest of North America. The San Andreas Fault has several prominent bends, so just as two interlocking pieces of a jigsaw puzzle cannot slip very far relative to each other, neither can both sides of the curved San Andreas Fault. Furthermore, if slippage has occurred along the San Andreas Fault for eons, friction should have greatly heated the sliding surfaces. Drilling into the fault has not detected that heat.This is an extremely important data point, and one which strikes a telling blow against the tectonic explanation. If it were the only data point that seemed to oppose the tectonic theory, it would not perhaps be so damaging, but in fact there are dozens of other powerful data points which are very damaging to the tectonic theory but which seem to support the hydroplate theory. Some of those which have been discussed in previous posts include the arc-and-cusp shape of deep ocean trenches, the unexpectedly low gravity readings scientists have measured over deep ocean trenches, and the difficulties the tectonic theory has in explaining the location of Antarctica (did it all move south on one plate, and if so then how to explain the severe sediment displacement found in the mountain ranges of Antarctica?), as well as the earthquakes far from boundaries mentioned above, and the bimodal depth distribution of earthquakes that Dr. Brown discusses in the passages linked above. The existence of Lake Vostok in Antarctica seems to pose some serious difficulties for the conventional tectonic theory as well.
If builders, owners, and officers of the Titanic were complacent and overconfident, they were simply reflecting the attitude of every shipping line in the North Atlantic trade. If the passengers believed that the Titanic was indeed unsinkable, it wasn't because they had succumbed to the blandishments of the shipping line's advertisements or the pronouncements of the experts: in the forty years prior to the Titanic's maiden voyage, only four lives had been lost on passenger ships on the North Atlantic trade. Imagine how blithely air travel would be regarded by present-day travelers, who usually seem to express little enough trepidation about the hazards of commercial flying, if the major airlines possessed a similar safety record. never had any form of transportation been so safe and hazard free. xi.As for the "terrain," so to speak, we now know that an extensive and dangerous field of ice stretched across Titanic's path, much further south than the captain anticipated (he had already adjusted his course ten miles further south based on warnings received, but not far enough).
After the flood, magma under the Pacific floor, but above the crossover depth, erupted onto the Pacific floor. (To a much lesser extent, eruptions continue today, so in those places, ocean temperatures rise temporarily, a phenomenon called El Niño.14) Magma below the crossover depth drains down into the outer core, so the outer core is slowly growing today! Simultaneously, melting is shrinking the total volume below the crossover depth, so the crust is compressing like the wrinkling skin of a drying (shrinking) apple. Also, the continents, thickened during the compression event, are still sinking into and laterally displacing the mantle. So the mantle is being squeezed downward from above and upward by the growing outer core. Mantle volume is also being lost primarily from the Pacific mantle by draining below the crossover depth and by eruptions above the crossover depth. Therefore, the mantle is shifting an inch or so a year, in general, toward the Pacific to replace that escaping volume. [See Figure 91 on page 165.] These movements and stresses produce earthquakes. Slowly shifting continents led to the mistaken belief that the entire solid mantle somehow circulates as if it were a liquid—and, over millions of years, drifted continents over the face of the earth. [To read this passage in Dr. Brown's book, go to this page, to a paragraph in the section entitled "Deep Movements During the Flood Phase"].These forces create frictional heating along faults. From there, Dr. Brown explains:
frictional heating along the fault melts the grain-sized minerals with the lowest melting temperatures, causing them to expand, because they were above the crossover depth. (Remember: Tiny movements at the extreme pressures deep in the earth create great heat and melting.) Minerals with higher melting temperatures remained solid, maybe for decades, thereby encasing and trapping the tiny droplets of melted rock.As more frictional heat “soaked” very slowly into the rock on both sides of the fault, the previously encased droplets of melt began to leak. Paths opened up for the expanding melt to escape upward buoyantly, allowing the highly compressed solid “scaffolding” (surrounding the focus and composed of the minerals with the highest melting temperatures) to become unstable and begin to collapse. Frictional heating instantly became extreme, so all nearby minerals suddenly melted. The result: a powerful earthquake. [To read this passage in Dr. Brown's book, go to this page].
So, Dr. Brown believes that most fault slippage occurs because the fault is unlocked due to the sudden liquification of rock along the fault due to frictional heat buildup over time. However, he notes that in addition to melted rock (magma) creating a fault movement, high-pressure water could do the same thing. In note 25 on this page of his book, he says:
Shallow earthquakes, in addition to the mechanism explained in Figure 88, may involve another phenomenon. Trapped subterranean water, unable to escape during the flood, slowly seeps upward through cracks and faults formed during the crushing of the compression event. (Seismographs on the Pacific Ocean floor have measured tremors from such seepings.)11 The higher this water migrates through a crack, the more the water’s pressure exceeds that in the walls of the crack trying to contain it. Consequently, the crack spreads and lengthens. (So, before an earthquake, the ground often bulges slightly, water levels sometimes change in wells, and geyser eruptions may become more irregular.) Simultaneously, stresses build up in the crust, again driven ultimately by gravity and mass imbalances produced by the flood. Once compressive stresses have risen enough, the cracks have grown enough, and the frictional locking of cracked surfaces has diminished enough, sudden movement occurs. Water acts as a lubricant. (Therefore, large temperature increases are not found along the San Andreas Fault.) Sliding friction instantly heats the water, converts it to steam at an even higher pressure, and initiates a runaway process, one type of shallow earthquake.
This explanation reveals the reason that the injection of high-pressure water deep underground by human activity can also create a similar result.
The immense bulk of the liner displaced an incredible volume of water in the narrow channel, creating a powerful suction in her wake. As she approached the entrance to the channel, the Titanic drew abreast of the small American liner New York, which was moored side by side to the White Star's Oceanic. Both ships had been immobilized by the coal strike, and neither had steam up. As the Titanic passed, the suction of her wake drew the two smaller vessels away from the dock where they were tied up. The strain on the six lines mooring the New York to the Oceanic grew too great, and with a series of loud cracks they parted in rapid succession as the New York was pulled helplessly toward the Titanic. For a moment a nasty collision seemed inevitable as the stern of the New York swung to within three or four feet of the bigger liner's hull. Quick thinking on the part of Captain Gale of the tug Vulcan and prompt action on the Titanic's bridge by Captain Smith averted an accident. 41.Mr. Butler recounts that one passenger, Renee Harris, the wife of an American theater producer, "suddenly found a stranger standing at her side, asking, 'Do you love life?'" When she answered in the affirmative, he told her, "That was a bad omen. Get off this ship at Cherbourg, if we get that far. That's what I'm going to do." According to Mrs. Harris, she laughed it off at the time, "but later she would recall that she never saw the man on board again" (Butler 42).
For most people, the difference between a fear and a premonition is that fears are vague and not unusual. Premonitions, on the other hand, seem to come spontaneously, and often with great force and clarity. In fact, for most people, the problem is not recognizing a premonition, but acting upon it.This is an important distinction. As someone who has made hundreds of skydives and participated in dozens of military tactical airborne operations (often at night with heavy gear and sometimes in atrocious weather conditions), I can report that I have had several occasions where I experienced what the paragraph above would describe as "vague and not unusual" feelings of general fear and unease prior to some jumps, but nothing ever came of them. They were not at all specific, spontaneous, or full of "great clarity." They were just ordinary fear, not premonitions (if true premonitions even actually exist).