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.
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.
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.
The words "burst forth" correspond to the words "were opened" and the expression "the fountains of the great deep" corresponds to the "windows of the heavens." This chiastic parallelism indicates that the waters below the ground came forth as the waters above the ground broke loose. Published in Origins v. 1, n. 2.
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.
This is an update of "The Ginkgo Petrified Forest" Origins 1(2):101-103 (1974)
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.
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.
This article is an update of the article, Famous Fossils on a Mountaintop (Origins v. 1, n. 1)
