The Washington State scablands........Lake Missoula glacial dam breach and the massive flood and its geological effects.
J Harlen Bretz
And The Great Scabland Debate
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Introduction
One of the most interesting debates in the history of geology has to do with the origins of the Channeled Scabland region in eastern Washington State – so named by J Harlen Bretz because of the region’s distinctive channels with intervening “scabs” of loess or soil covering the underlying basaltic rock. But how, exactly, were these channels and scabs formed? Were they formed over millions of years of time by process of erosion currently active in the region or were they formed by some other means?
By the time of the early twentieth century, the most prominent scientists of the day were decidedly “uniformitarian” in their thinking.1,2 That is, they believed that the regular observed processes of usual geologic events acting over vast periods of time were able to explain most if not all of the observed geologic record. J Harlen Bretz, who earned his Ph.D. in geology from the University of Chicago, was the first geologist to seriously challenge this notion, but it was by no means an easy. The process to change the prevailing dogma of the day was a tremendous struggle for Bretz despite his use of a great deal of very good evidence – and that is what is most interesting about this story.
The Evidence for a Catastrophic Flood
Many people think that scientists are dispassionate in their investigations, conclusions and their general search for truth. As we will soon discover, most scientists have always been very passionate people who, just like most of the rest of us, do not like to admit a long-held error even in the face of otherwise overwhelming evidence.
Bretz’s interest in the Scablands was first aroused in 1910 by the newly published Quincy topography map of the area. This map clearly revealed great potholes now known as the Potholes Cataract. During this same year, Joseph Thomas Pardee published a paper describing the geomorphological evidence for a great glacial lake occupying the intermountain basins of western Montana during the late Pleistocene. He described the prominent horizontal shorelines or “strandlines” previously noted by T. C. Chamberlin. This lake, which was to eventually play a prominent role in this story, was named for Missoula Montana, where its strandlines were particularly prominent. 2
Bretz began the field research of the Scablands in 1922 with the help of a few advanced geology students. He continued these summer outings over the course of seven years, traveling largely byfoot. What he saw was truly remarkable. For example, the cliffs of Dry Falls are 3.5 miles wide and drop some 400 to 600 vertical feet.1,4 By comparison, Niagara Falls is only a measly 1.5 miles wide and drops just 165 vertical feet. Bretz took note of the very steep sides of the channels and their relatively straight pathways as well as the presence of very large gravel bars deposited by water. Also, throughout the scablands Bretz saw huge islands of land protruding from the surrounding landscape with streamlined features as if they were carved by massive torrents of water. 2
Bretz first presented his initial observations in 1923 to the Geological Society of America. In that first paper he simply described what he saw on his various field trips. He deliberately took special care not to present any sort of explanation or interpretation for his observations. He did note, however, that the observed channel erosion required large non-specified quantities of water. On the other hand, in his second 1923 paper Bretz decided to stir up his fellow geologists just a little bit. In the second paper Bretz presented his theory that a truly huge catastrophic flood was in fact the creator of the most prominent features of the Scabland region. 2
Uniformitarian Bias Blinds Scientists
Of course this conclusion was less than enthusiastically received by Bretz’s fellow geologists. In fact, Bretz was openly and vigorously ridiculed for presenting such a ludicrous notion as a flood model for the scablands since this region had obviously been carved out over millions of years by uniformitarian processes. In support of this derision, Pardee’s brief 1922 paper concerning the scabland region near Spokane, Washington (the Cheney-Palouse Scabland Tract) was used to discredit Bretz. In that paper Pardee proposed that unusual glaciation, acting over very long periods of time, created the Scablands.
However, when Bretz went to visit this area a couple years later he found that Pardee’s “glacial” deposits were actually flood bars. What is even more interesting is that, after hearing of Bretz’s ideas, Pardee seemed to change his mind. He actually wrote to Bretz in 1925 suggesting that Bretz consider the draining of a glacial lake as a possible source for his suggested cataclysmic flood. In reference to this communication, Bretz wrote the following to J. C. Merriam:
Mr. Pardee of the Federal Survey, who has seen much of the scablands, has suggested that his glacial Lake Missoula might have afforded the water for these enormous rivers if it were suddenly drained out across the plateau. This comment indicates that his former view of the scablands by land ice and concomitant subglacial drainage under ordinary climatic melting has been abandoned. Even our ultraconservative in Pleistocene geology, Dr. Alden, wrote that the phenomena I describe certainly appear to be river work “if you could only show where all the water came from in so short a time.” 2
Later, in a 1943 correspondence with Hobbs, Pardee himself wrote:
The “drift” referred to in the article Science consists of bouldery deposits which at that time (1922) I interpreted as a gravelly till transported and deposited by glaciers that extended far over the Columbia Plateau. The principal feature of the deposits that suggests glacial action is the presence of large boulder, some of them of foreign origin. From information of the region that has been made available since 1922, however, I have concluded that the deposits are more likely the work of flood waters, such as postulated by Bretz, rather than of glacial ice. That is — I do not regard them as conclusive evidence of glaciation. On the other hand the deposits are indirectly, if not directly, related to glaciation and may have been formed by streams that gouged out the channels and basins under an ice cover as you suggest.2
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Sometime before 1927 geologists were catching on to the seriousness of what Bretz was suggesting. If true, Bretz’s theory would undermine the very foundation of Uniformitarianism. Just as anticipated, the general outcry against any hint of a catastrophic model was very loud indeed. In fact, there was a very strong desire to publicly discredit and humiliate Bretz. So, to this purpose, Bretz was asked to present his ideas in public forum to the Geological Society of Washington. Bretz himself was rather unaware of the underlying purpose of this gathering or just how hostile his audience actually was to his ideas. Unawares to Bretz, six “challenging elders”, as Bretz later referred to them, were chosen to counter Bretz’s claims and beat him in public debate.6
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As Long as it’s Not Noah’s Flood
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Bretz Vindicated
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Bretz’s remarkable work was built painstakingly over many years, but he had to fight great opposition for many decades for its final acceptance. Finally, in 1979, the geological establishment publicly acknowledged Bretz’s work by awarding him the prestigious Penrose Medal – the most prestigious honor in the field of geology.3 Bretz was in his late 90s, and had been holding the line for more than 50 years before finally realizing general acceptance of his “insane” catastrophic model for the formation of the Channeled Scablands of eastern Washington State.
References
- Allen, J. E., Burns, M., Sargent, S. C., Cataclysms on The Columbia, Timber Press, (1986),Samuel Strok book review for Geology 103 at Bellevue Community College – Winter, 2003 (http://scidiv.bcc.ctc.edu/rv/103/reviews/docs/Strok.ncl )
- Baker, V., Joseph Thomas Pardee and the Spokane Flood Controversy, GSA Today, 5:(9), September 1995 (http://gsahist.org/gsat2/pardee.htm )
- Helfferich, C., Boulders, Braids, and J Harlen Bretz, Alaska Science Forum, Article #1160, November 17, 1993 ( http://www.gi.alaska.edu/ScienceForum/ASF11/1160.html )
- Spokane Astronomical Society, 1998 (http://www.webmaker-nw.com/bustomars/mars-dry-falls-1.html )
- Kids Cosmos, 2001 (http://www.kidscosmos.org/kid-stuff/mars-trip-scablands.html )
- Newman, J., Missoula Floods, Oregon Field Guide, Episode 1001, 2002-2004 (http://www.opb.org/programs/ofg/episodes/1001/missoula/index.php )