Kerr Watch

Elapsed time since Richard Kerr failed to inform his Science readers of the confirmation of nanodiamonds at the YDB: 6 years, 2 months, and 2 days

Recent papers critical of the Younger Dryas Impact Hypothesis: Daulton and Scott

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Problem solved: Carolina Bays are shock liquefaction impact features from hypersonic ice boulders launched from the glacial ice sheet by a cosmic impact at the Younger Dryas

A. Zamora

The Tusk was absolutely thrilled to see the publication last week of a paper concerning Carolina Bays in the distinguished journal, Geomorphology. Other than a brief role for the Carolina bays in the early papers of the Comet Research Group, and a much longer series of Geological Society of America posters laboriously researched and determindly published by Michael Davias et. al, Zamora’s A Model for the Geomorphology of Bays is the only peer-reviewed and published ‘ET origin’ work on bays in the last two decades — and it is a doozy.

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Zamora builds on the work of Willam Prouty and Melton and Schriver in the first half of the 20th century, with an assist from Eyton and Parkhurst in the 70’s, and finally Davias and Kimbel’s efforts in recent years. Each of the researchers maintained that the bays were formed at once by a barrage of material from the midwest. But, just as the early researchers ultimately decided, those around today also dismiss bays as the direct impacts of ET fragments of a comet or asteroid, and consider them to be the remnant features of secondary impacts from the ejecta and ballistic shockwaves of a northerly catastrophe. They are wise to do so.

The correct theory must account for ALL the easily observed, unique characteristics of bays. [See list of 16 from Eyton and Parkhurst here] The “wind and wave,” gradual formation, theories that continue to hold sway in classrooms, and publications from Ivestor and Brooks, fail miserably to account for all the observed phenomena. Zamora checks each off with ease. When time permits I hope to address them one by one.

Significantly, Zamora’s work is multidisciplinary and, like Davias, assisted by geometry as well as geology. Here is a sample:

Ellipses are mathematical conic sections formed by the intersection of a plane and a cone. The elliptical geomorphology of the Carolina Bays and the Nebraska Rainwater Basins can be explained if the bays originated from slanted conical cavities that were later remodeled into shallow depressions by geological processes. A width-to-length ratio of 0.58 corresponds to a cone inclined at 35° using the relationship sin(θ) = W/L. The proposed conical cavities could have been made by impacts of material ejected at approximately 35° in ballistic trajectories from the point of convergence in the Great Lakes Region. The small variations of the width-to-length ratio correspond to slightly different angles that are consistent with possible ballistic trajectories

The bay rims to Zamora are the result of a complex mathematical equation. They are the final surface expression of thousands of conical, inclined ballistic shock cones, each traveling with a giant ice fragment blown from the ice sheet in a nine-minute supersonic arc from the frigid north to the Carolina coast. (I will work on that sentence but you get the idea). These icebergs from space slammed into the supersaturated unconsolidated clayey sands of the coastal plain and left behind the shock “ripples” and “flaps” that we recognize today as bay rims. Zamora even provides an equation relating the perfection and ellipticity of bays to the degree of unconsolidated sediments encountered by the ice bullets:

The LiDAR images also reveal that some terrains do not have elliptical bays. Davias and Harris (2015) describe six archetype bay shapes that may be determined by the geological characteristics of the terrain. The thickness of the layer of unconsolidated material required to produce an elliptical bay can be estimated by the formula tan(θ) × L/2, where L is the length of the major axis and θ is the angle of inclination. A conical cavity inclined at 35° corresponding to a bay with a major axis of 400 m would require a layer of unconsolidated material with a depth of approximately 140 m.

That makes sense to me, and accounts for the “classes” of similar bays, an aspect unexplained by wind and water enthusiasts, but first investigated and catalogued by Davias.

In addition to the present journal publication, Zamora makes his case in detail in a recently published book available from Amazon: Killer Comet: What the Carolina Bays tell us. I am reading it now and will update this post accordingly.

On the shoulders of genius, Zamora has provided defensible and superior answers to the many questions provoked by the appearance and distribution of Carolina bays. The geological community will largely ignore this paper, of course, but some will take note. And there is always reason for hope as the class of geologists who reject recent catastrophic explanations out-of-hand continue their long march from the tenured defense of the known, to retirement, and finally to death. I note that in closing Zamora gives a shout-out to his editor, Professor Andrew J. Plater of the University of Liverpool, clearly an enlightened man, who tweets here as @GeomorphologyDr if you care to thank him.

 

 

Comet Research Group responds to Robert Schoch

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Robert Schoch

Dr. Robert M. Schoch, Ph.D., of Boston University, is a thought provoking scientist with an open-minded approach to new ideas. Unfortunately his interest in disruptive theories has never extended itself to the Younger Dryas Boundary hypothesis, as he details on his webpage in a critique titled “Controversies Concerning the End ofthe Last Ice Age.”

His objection to the published science and data of the Comet Research Group is curious, since our work validates much of his unpublished speculation concerning catastrophe at the Pleistocene-Holocene transition. This dynamic is disappointing because those working to reveal the true record should find some common cause. Unfortunately, Schoch has never reached out to our researchers in order to work through and address his criticisms.

So, the CRG is taking the opportunity here on the Tusk and elsewhere to rebut Dr. Schoch’s critique in the hope that he will carefully re-consider his position, which seems entirely based on the on the faulty work of our critics — which are his too.

Comet Research Group: Rebuttal to “Controversies Concerning the End of the Last Ice Age” 

The Younger Dryas impact hypothesis proposes that a massive swarm of fragments from a giant comet hit Earth approximately 12,800 years ago, triggering bitterly cold ice-age conditions, while contributing to the extinction of millions of animals and to a human population decline across the Northern Hemisphere. The debris from the multiple comet impacts created the Younger Dryas boundary layer (abbreviated as “YDB”), which contains more than a dozen items, called “proxies,” all of which have been found in previously known impact events. These proxies include melted iron spherules, melted glass spherules, high-temperature chunks of melted glass, nanodiamonds, carbon spherules (some containing nanodiamonds), iridium, osmium, platinum, charcoal, and aciniform carbon, a form of soot. Although many of those individual proxies, such as charcoal and soot, can be produced by normal terrestrial processes other than impacts, the entire suite of proxies listed above is only known to occur in cosmic impact events, and cannot be produced in any other natural way. That is an important distinction to remember. To repeat, individual proxies may have other sources than impacts, but there is no evidence of any kind that all of those proxies together are produced at one time by anything other than a cosmic impact. For more information on the impact hypothesis and these proxies, see our website at www.CometResearchGroup.org

Continue reading Comet Research Group responds to Robert Schoch

Grab an oar: Comet Research Group crowd appeal goes live on Indiegogo

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Hey folks, I will make this short and expand and update in the future. The newly formed Comet Research Group crowd appeal for funding ancient impact research is on the air — and your help is desperately needed. Now is the time for all good men to come to the aid of the Tusk. And the sooner the better. We only have 30 days remaining and funding of this type requires early enthusiasm to thrive.

There are three pages you should visit in order to give, learn, and share your interest in the effort.

Give: Indiegogo

Learn: Comet Research Group

Share: Facebook

Many of you, like me, have devoted countless hours to this obscure subject. Others who visit this blog maintain a strong interest, if not the obsession of others. But each and every person who has visited cosmictusk.com more than once, and wonders “what the hell did happen 13,000 years ago?” has a good reason to donate to continue and expand the investigation to provide the answer.

Small contributions are particular important. Small donations raise the visibility of the effort just as much as large ones. 5$ 10$ $100 or more is deeply appreciated.

Thank you for donating and sharing the effort on social media. Please let me know if you have “grabbed an oar” in the comments below!