Near the middle of the sea in what is now Kansas sediments were deposited at a fast rate creating about an inch of compacted chalk each 700 years. Some of the worlds finest fossils have been discovered here. The crinoid Uintacrinus and fish Ichthyodectes are two examples. (Fossilmuseum.net NP)
When other regions have such finds they are news, while the shelf and chalk deposit areas of the Western Interior Seaway boast finds nearly every digging season, by both hobbyists and professional scholars. While other scholars are quick to point out that marine fossils are abundant the vertebrate fossil record is relatively barren, this is likely due to the significantly fossil bearing conditions of the silt sea bottom and its storm driven record keeping system, where large silt deposits moved rapidly over large areas in short periods of time and created a relative recording of the living and dead creatures in its wake. (Baldridge 58)
The demise of the Western Interior Sea was again a result of regional shifts and changes that resulted in seaway becoming increasingly shallow, losing its connection to the oceans in both the northern and southern aspects of the region, due in part to land shifting as well as ocean recession. When this occurred fresh water lakes, rivers, swamps and streams filled the crevasses and valleys left by the seaway and massive formations of vegetation and other matter collected to create the coal deposits that we mine today and that serve as the majority of energy for nearly the whole of the Midwest and east coast of the U.S. (Brigham 400)
The fascinating history of the Western Interior Seaway is peppered...
" Hamilton explains that while Continental Lithosphere is as much as 93 miles thick, the "Oceanic Lithosphere" is much thinner - up to perhaps six miles. Indeed, the oceanic crust makes up only 0.099% of earth's mass, according to Hamilton. Oceanic lithosphere is a product of the volcanic magma that pushes up to force tectonic plates aside. As new oceanic lithosphere is actually formed the heat that comes up with the
In fact, the entire damage was caused by the tsunami itself along with other factors like the geology and geography of the region. The damage that the tsunami caused to mainland India, a seismically quiescent region, was concentrated mainly on the eastern coastline but some damage due to diffraction also occurred on the southernmost tip of the western coastline. A factor which played a major role in the scale
Summary of the Punic Wars The Punic Wars refer to the collective names of a series of three separate wars between Carthage and Rome, which took place from 264 to 146 BC. The wars were fought between the two strongest contenders for control over the central Mediterranean Sea of the time. These wars ended with the destruction of Carthage, thus ending the city's period as an independent power and an important
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