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The Organic Levels of the Yellowstone Petrified Forests

The normal accumulation of organic debris and the subsequent formation of humus and true soil which proceeds relentlessly on modern growth surfaces does not readily account for several of the phenomena seen in the organic levels of Yellowstone. Published in Origins v. 6, n. 2.

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Precambrian and Paleozoic Glaciation?

The effects of glaciers are well-dccumented in modern and Pleistocene sediments. Some Precambrian and Paleozoic sediments show some features similar to those of modern glaciation, but there is some controversy over whether the features are the result of glaciers, submarine landslides, lahars, turbidity currents, etc. Published in Origins v. 6, n. 1.

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Footprints in the Grand Canyon

The Coconino Sandstone has traditionally been interpreted as wind-deposited, but fossil trackways in this formation point to underwater deposition. Published in Origins v. 5, n. 2.

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How Rapidly Can Wood Petrify?

Experimental evidence shows that wood can petrify in a few years or less when immersed in mineral-rich water. Published in Origins v. 5, n. 2.

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Megabreccias: Evidence for Catastrophism

The presence of various kinds of megabreccias in the geologic column, showing in some cases the transport of extremely large clasts, indicates energy levels on a scale that staggers our imagination. Published in Origins v. 5, n. 1.

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A New Journal on Catastrophism

A new journal, Catastrophist Geology, has begun publication. Published in Origins v. 4, n. 2.

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Clastic Dikes

Clastic dikes form when unconsolidated sediments are forced upward into overlying sediments by the weight of the accumulating sediments. Some clastic dikes intrude into layers supposedly many millions of years younger, indicating that the underlying sediments remained unconsolidated for unexpectedly long periods of alleged time. Such features challenge the conventional geologic time scale. Published in Origins v. 4, n. 1.

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Anomalous Ages for Meteorite Impacts and Tektites

Major tektite falls in Australia in strata as young as 5700 years old according to radiocarbon dating have called in question both the fission-track and the K-Ar methods of dating which assign these identical tektites an age of about 700,000 years. Published in Origins v. 3, n. 2.

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Geological Changes and Time

A review of two articles: On the Survival of Paleoforms, and The Tempo of Geomorphic Change. The scientific data of both papers indicate that much greater caution is warranted in approaching questions regarding the length of time involved in the past history of the earth. Published in Origins v. 3, n. 2.

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Dinosaur Tracks and Giant Men

The Glen Rose region of the Paluxy River does not provide good evidence for the past existence of giant men, nor does it provide evidence for the coexistence of such men and the giant dinosaurs. Published in Origins v. 2, n. 2.

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Old Traditions on Trial

A review of the book, The Nature of the Stratigraphical Record. The geologic record can be described as long periods of relative calm punctuated by brief catastrophic events. Numerous geologic features can be traced over large portions of the earth's surface. Published in Origins v. 2, n. 2.

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Turbidites

This new concept indicates that some events in the past history of the earth may have proceeded much more rapidly than was previously believed. Published in Origins v. 2, n. 2.

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The Spirorbis Problem

A tiny marine worm, Spirorbis, constructs a calcareous tube, and is often found attached to shells and debris in the ocean. Fossil Spirorbis are sometimes common in coal beds. Some have suggested Spirorbis lived in fresh-water habitats in the past, but this is highly unlikely. It is more likely that coal formed in marine waters during the Flood. Published in Origins v. 2, n. 1.

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The Ginkgo Petrified Forest

The Gingko Petrified Forest in western Washington state contains a large variety of petrified plant species, more than any other site known. The plants represent a mixture of tropical and temperate species that appear to have been transported and not grown in situ. Published in Origins v. 1, n. 2.

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Fossil Tree Orientation in the Chinle Formation

Trees were measured at nine locations in two general areas in Arizona and Utah. Preliminary data show very strong orientation of logs at most sites. Published in Origins v. 1, n. 1.

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Famous Fossils From a Mountaintop

Thousands of well-preserved Cambrian fossils are found in the Burgess Shale of Alberta, Canada. These Cambrian fossils are complex and diverse, in contradiction to the expectations of evolutionary theory. Published in Origins v. 1, n. 1.

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Unusual Fossils From a Mountaintop

This article is an update of the article, Famous Fossils on a Mountaintop (Origins v. 1, n. 1)

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