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"Dinosaur tracks preserved in sandstone, knobs of granite rising from the plains, and springs cascading down limestone cliffs are just a few of the fascinating geologic features discussed in Roadside Geology of Oklahoma, a guide to more than 35 roads that crisscross the Sooner State. Longtime Oklahoma Geological Survey geologist Neil Suneson tells you what to look for along the roads, points you in the direction of nearby parks with interesting rocks and crystals, and recounts historical gems about radium mineral baths, coal mines, fossil excavations, and the early days of petroleum extraction, not to mention the rush for nonexistent gold in the Wichita Mountains. And lest you think nothing has happened recently, geologically speaking, in this Great Plains state, you'll learn about a fault that broke the land surface a meer 1,250 years ago and is capable of generating a 7.0 magnitude earthquake. Suneson also gets you up to speed on more modern considerations such as groundwater depletion, petroleum fracking, and strip mine reclamation. Take this book along for a ride as you roll across the red plains east to the Ozark Plateau, west to the Panhandle, or south to the Ouachita, Arbuckle, and Wichita Mountains"--
Located along the Atchison, Topeka & Santa Fe Railroad, at a stop known as Oklahoma Station, Oklahoma City was born on April 22, 1889, at 12 noon. By 6:00 p.m., she had a population of around 10,000 citizens. As with any birth, there were many firsts in the newly opened territory, and many of these landmark events have been captured and preserved in historic photographs. With images culled from the archives of the author‚'s own vast personal collection as well as the Oklahoma Historical Society and other collections, the stories of prosperity and development of the area‚'s first settlers are told through Statehood. In light of this perseverance, it is no wonder that Theodore Roosevelt announced, ‚"Men and Women of Oklahoma. I was never in your country until last night, but I feel at home here. I am blood of your blood, and bone of your bone, and I am bound to some of you, and to your sons, by the strongest ties that can bind one man to another.‚"
A photographic guide to Oklahomas Devonian trilobites. The geological history of Coal County, Oklahoma. Descriptions of rock formations where trilobites are found. Excavation and restoration of trilobites. A photographic atlas of the Lower Devonian trilobites of Oklahoma, with helpful information to aid in their identification. Trilobites are a well-known fossil group, possibly second most famous only to dinosaurs. With their easily fossilized exoskeleton, they left an extensive and diverse fossil record. They began a drawn-out decline to extinction during Late Devonian time, when all but one of the trilobite orders died out. This meticulously researched reference guide is a photographic atlas and descriptive compendium on the trilobites of Coal County, Oklahoma. The species described lived during the Lower Devonian in a shallow tropical ocean that had advanced over the landscape of North America. More than twenty species are exquisitely preserved in Oklahomas limestone rocks. Each species is carefully illustrated, including thorough descriptions, so that those familiar and unfamiliar can understand and appreciate these amazing creatures. The most current scientific research on these trilobites is also included. For those wishing to pursue a deeper interest in trilobites, a comprehensive bibliography lists hundreds of sources of information for further study.
Geologic maps supply a wealth of information about the surface and shallow subsurface of the earth. The types of materials that are present in a location and the three-dimensional structure of the bedrock both can be gleaned from a clearly prepared geologic map. Geologists, civil and environmental engineers, land-use planners, soil scientists, and geographers commonly use geologic maps as a source of information to facilitate problem solving and identify the qualities of a region. Maps reveal the position of many types of natural hazards, indicate the suitability of the land surface for various uses, reveal problems that may be encountered in excavation, provide clues to the natural processes that shape an area, and help locate important natural resources. Suitable for lab courses in structural geology as well as field geology work, Spencer describes representative examples of features found on geologic maps and outlines procedures for interpretation and projection. Geometric techniques are explained using a step-by-step approach. Coverage of mapping methods includes tools that provide necessary data, such as Google Earth, GPS, GIS, LiDAR maps, drones, and aerial photographs. Challenging and engaging exercises throughout the text involve students in the mapping process and stimulate an appreciation of the extent and precision of information presented in geologic maps. Regional geology is an important component of lab and field mapping projects. As such, the Third Edition includes new maps of the Gulf of Mexico Coastal Plain, Rocky Mountain Front Range, Yellowstone region, Moab, Utah, Shenandoah National Park, and Hawai’i. A new chapter devoted to tectonic maps also broadens students’ exposure. Ed Spencer brings over 45 years of teaching experience to the text along with valuable insight and clarity into the interpretation and preparation of geologic maps.
Author Charlie Spencer shows you around the state from the flat, glaciated plains in the north to the knobs of rhyolite in the St. Francois Mountains in the south, and from the earthquake-formed sand boils on the Mississippi floodplain in the southeast to the layers of coal, shale, sandstone, and limestone on the Springfield Plateau and Osage Plains in the west.
An introductory chapter briefly reviews Texas' geology followed by a series of road guides with the local particulars. The authors tell you what the rocks are and what they mean. Useful graphics and charts supplement the text and help you to understand