Humans, the Short End of the Time Scale

The long-winded history of the Great Plains is recorded in the geological features we see today. The Precambrian shows itself in outcrops of the pink Town Mountain granite, the Packsaddle schist and Valley Springs gneiss. These rocks tell a story of massive chambers of boiling-hot magma being pushed to the surface to cool, and surrounding rocks being metamorphosed by intense heat and pressure. In the Paleozoic and later in the Cretaceous, ancient shallow seas covered the inner continent and produced carbon-rich rocks. Limestones, shales, and fossilized reefs are scattered throughout the Great Plains and nearby areas, evidence that the area was not always the ‘Great American Desert’. Decaying plant matter built up and compressed over time resulted in coveted coal deposits. When the waters retreated, the temperatures started going down, too.

Now, the Great Plains are dusted by a layer of younger sediments—sand and gravel and soil—eroded from the Rocky Mountains on the western border. These sediments help trap water underground in aquifers, supplying the region and its inhabitants. It is no surprise that pockets of water have been attracting all sorts of living beings for thousands of years, and early humans were no exception.

The common consensus among archaeologists is that humans began living on the Great Plains at least 11,000-11,500 years ago, based on carbon dating of various artifacts like bones, stone flakes and tools. This time overlaps with the last Ice Age, and the time of giant creatures like mammoths and saber-tooth cats (see Miocene and Mammoths). In 2005, a study took advantage of some broken mammoth bones that had been on display at the Denver Museum of Nature and Science for nearly 30 years. The bones appeared to have been broken by humans rather than by natural means, and were carbon dated at about 12,200 years old. Many scientists are drawn to the significance of discovering the oldest site with clear evidence of human habitation, and so research continues.

Humans have been fascinated by the challenges and opportunities offered by life on the Great Plains for a very long time, whether because of water and food resources, the hunt for gold and precious materials, agriculture, or an adventure. This curiosity is prominently realized in the mid-1800s, when Americans were surveying the Territories and some people thought that rain would follow the plow.

 

Featured photo courtesy of U.S. National Archive:

 

See the following sources for more info:

http://geology.teacherfriendlyguide.org/index.php/rocks-sc/rocks-region4-sc

https://www.geosociety.org/documents/gsa/timescale/timescl.pdf

Denver Post Staff Writer. “Museum’s Mammoth Bones Exhibit New Life After Nearly 30 Years on Display, Fossils Found in Kansas Are Causing Scientists to Re-examine When Humans Arrived on the Great Plains. (DENVER AND WEST).” The Denver Post (Denver, CO), 2005.

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Clean Burning Coal

When studying coal formation, origins usually point to the Carboniferous period in geologic history, 359-299 million years ago. Shallow inland seas, like the Western Interior Seaway discussed in the last post, were intermixed with thick trees and plant life, creating the perfect swampy wetlands where coal is formed. Decaying plant matter, buried and squeezed by mud, retains a lot of carbon. Over millions of years, the layers of dead plants undergo a process of pressure called carbonization.

The deeper the burial, the better the coal; higher carbon concentrations in the rock burn better and cleaner. Carbonization creates four main types of coal, from lowest to highest grade: lignite, sub-bituminous, bituminous, and anthracite.

Coal is formed on all continents, and the U.S. is among the biggest sources. While most U.S. coal comes from the East Coast, most famously from Pennsylvania and the Appalachian Region, a significant amount comes from the ‘Western Coal Region’, essentially the Great Plains. Coal from the western United States tends to be Cretaceous in age (see the post The Cretaceous Interior Seaway), corresponding with the dinosaurs, and more importantly the Western Interior Seaway, which provided the wet environment and flourishing plant life needed to form coal.

“Coal is the largest source of energy for generating electricity in the world, and the most abundant fossil fuel in the United States.”

Nine major coal-producing regions exist within the Great Plains, including some resources in Canada, and Wyoming is by far the top producer. The majority of these locations produce low-grade coal, of the lignite and sub-bituminous types. These sources supplied early explorers, farmers, and railroads, but after World War II, mining and production of coal took a nose dive. The need for energy did not decrease. In fact, it exploded, and desire for fuel has only increased since the 60s. The government also began setting stricter emissions standards at this time, and as a result, many hopeful surveyors set out to find their fortune in clean-burning coal.

 

Featured image courtesy of U.S. National Archive:

 

See the following sources for more info:

http://plainshumanities.unl.edu/encyclopedia/doc/egp.ind.014

https://www.nationalgeographic.org/encyclopedia/coal/

https://www.geosociety.org/documents/gsa/timescale/timescl.pdf

Roberts, Laura N. Robinson, Laura N. Robinson. Kirschbaum, Kirschbaum, Mark A., and Geological Survey, Issuing Body. Paleogeography of the Late Cretaceous of the Western Interior of Middle North America: Coal Distribution and Sediment Accumulation. U.S. Geological Survey Professional Paper; 1561. Washington: Denver, CO: U.S. G.P.O.; U.S. Geological Survey, Information Services, 1995.

The Cretaceous Interior Seaway

Jurassic Park helped to give dinosaurs their fame, but this really wasn’t when dinosaurs ruled the Earth. The Cretaceous period, starting about 145 million years ago, was the real heyday of our giant mesothermic friends (most dinosaurs were not ectothermic, or cold-blooded!). Until their extinction around 66 million years ago, dinosaurs were spread across the globe, including in the Great Plains region. At this point, Pangea had broken apart and North America was starting to look like the massive continent we know today.

Even more interesting, the North American landmass was home to a Cretaceous inland sea. The Western Interior Seaway was a result of incredibly high sea level, where a shallow ocean covered a massive part of the continent. “At its maximum extent, the seaway extended for 4,800 km from the North Slope of Alaska to northern Mexico and was approximately 1,620 km wide from central Utah to Minnesota,” according to a U.S. Geological Survey report. This includes much of the Great Plains region.

Evidence of this inland sea lies in the paleontology—the fossils—of the region. Geologists have found an incredibly diverse variety of marine fossils all over the landlocked states, even here in Arizona. The fossils found are not just shallow water creatures, though some extensive coral reef remains have been studied. Giant turtles, ammonites, crinoids, sharks and fishes have been discovered in areas that are now deserts and grasslands. On top of that, giant marine beasts resembling the Loch Ness monster, like Mosasaurs and Plesiosaurs who needed large expanses of salty ocean water to survive, have been found. Right along side these are the bones and tracks of dinosaurs who tromped on the muddy shores.

The rock that hosts the marine fossils also tells the tale of deep ocean covering North America. Chalk, limestone and dolostone are carbonate rocks, created when microscopic sea-critters died and accumulated on the ocean floor, eventually compacting into solid rocks.

By the end of the Cretaceous, the Rocky Mountains were beginning to form, and the Western Interior Seaway was retreating. The dropping sea level and receding inland sea led way to swampy environments, and later, the formation of coal.

 

Featured photo courtesy of U.S. National Archives:

 

See the following sources for more info:

http://geology.teacherfriendlyguide.org/index.php/fossils-sc/fossils-region4-sc

https://www.geosociety.org/documents/gsa/timescale/timescl.pdf

Roberts, Laura N. Robinson, Laura N. Robinson. Kirschbaum, Kirschbaum, Mark A., and Geological Survey, Issuing Body. Paleogeography of the Late Cretaceous of the Western Interior of Middle North America: Coal Distribution and Sediment Accumulation. U.S. Geological Survey Professional Paper; 1561. Washington: Denver, CO: U.S. G.P.O.; U.S. Geological Survey, Information Services, 1995.

The Great American Desert

What exactly are the Great Plains? Everyone has heard the name, at least in a history class at some point. Definitions of the region have changed over time, and continue to be murky even today. Officially, the Great Plains cover parts of 10 U.S. states, the Canadian provinces of Manitoba, Saskatchewan, Alberta, and bits of the Northwest Territories. Most people will consider the area west of the 100^th meridian line to the Rocky Mountains to be a part of the Great Plains—a space taking up nearly a third of the country.

The Great Plains are not as flat and boring as you may imagine. It is crisscrossed and mixed with rolling hills and valleys carved by raging rivers. Even mountains make an appearance, most famously in the Black Hills of South Dakota. Most of the area is characterized by the typical semi-arid grasslands one might expect, though there was a time that the Great Plains were considered a full out desert.

This worked both for and against people from all walks of life. The Great American Desert was a concept that settlers used to become heroes—only the bravest and most awesome people could drop everything to move out farther west and thrive as farmers in the desert. Obviously, those parties interested in selling the land for profit also used the desert label as a mark of success, hinging on the idea that ‘rainfall follows the plow’. By settling and plowing the earth of this mighty desert, people could increase rainfall and enjoy the fertility of this harsh environment.

While humans have been inhabiting the Great Plains Region for over 15,000 years, it wasn’t until the last couple of hundred years that attempts were made to survey the area. Boy, were they fascinated. In 1817, Lewis and Clark considered the area an incredible garden, ripe with agricultural prospects. Not everyone agreed, and just three years later, a scientific expedition led by Stephen H. Long observed the hot, dry expanses and expressed doubts whether people could ever settle the area. Both saw the wilderness differently, with very different motivations.

Regardless, flora and fauna have thrived in the Great Plains for longer than humans have even existed, from sagebrush and cacti and trees, to bison and rattlesnakes and wolves. People were eager to spread, despite the hesitance of explorer and scientists, egged on by naturalists and a heck of a lot of hope. Even today, residents embrace the desert culture, echoing the hardiness of their pioneer forerunners.

This blog will cover a brief timeline of events, even before humans enter the picture, deep into geologic time when prehistoric life roamed the Earth. Later, it will discuss the elephant in the room, and such big-name influencers like Charles Dana Wilber, Ferdinand Hayden, and others.

 

See the following sources for more info:

https://www.britannica.com/place/Great-Plains

Baltensperger, B. H. “Plains Boomers and the Creation of the Great American Desert Myth.” Journal of Historical Geography18, no. 1 (1992): 59-73. doi:10.1016/0305-7488(92)90276-f.

Dillon, Richard H. “Stephen Long’s Great American Desert.” Proceedings of the American Philosophical Society 111, no. 2 (April 14, 1967): 93-108.

Samson, Fred B., Fritz L. Knopf, and Wayne R. Ostlie. “Great Plains Ecosystems: Past, Present, and Future.” Wildlife Society Bulletin 32, no. 1 (2004): 6-15.