Pillar To Post
Suppose Genghis Khan had been a convert to Judaism and his horde had fought for a different cause than in our universe? What if the Second Punic War got even weirder than it did in our history-- which, considering what really happened, ain't easy?
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These and more alternate realities are explored as Hugo Award-winner Harry Turtledove and his colleagues turn the past upside down and inside out, and the possibilities are endless. Alternate Generals III. Reviews from Goodreads.
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Dec Rookhouse Books eBook Kindle. The NPS Geodiversity Atlas delivers information in support of education, Geoconservation , and integrated management of living biotic and non-living abiotic components of the ecosystem. Established in , Appomattox Court House National Historical Park covers ha 1, ac in Appomattox County, Virginia, and preserves the village of Appomattox Court House and the surrounding farm, forest, and meadow lands.
The purpose of the park is to commemorate the surrender of the Confederate Army of Northern Virginia to the Union Army on April 9, , the strategic act that effectively ended the American Civil War. The park preserves many cultural resources, including the site of surrender at McLean House, the historic village at Appomattox, and the site of the Battle of Appomattox Court House.
The park lies within the western Piedmont physiographic province, which is underlain by hard crystalline igneous and metamorphic rocks such as schists, phyllites, slates, gneisses, and gabbros. This portion of the Piedmont physiographic province contains numerous belts of rocks that accreted onto the North American continent during repeated continental collisions and orogenic events, culminating in the formation of the Appalachian Mountains. This geologic history spans more than million years through the present regime of weathering, erosion, and anthropogenic land use patterns.
Rolling hills and narrow eroded stream valleys characterize the landscape at Appomattox Court House National Historical Park.
Appomattox Court House Landscape (U.S. National Park Service)
The elevation in the park ranges from m ft above sea level at the highest hills to m ft above sea level at the eroded Appomattox River valley. The Appomattox River and several tributaries, including Plain Run Branch, traverse the park, which protects over 13 km 8.
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The Appomattox River is a major tributary to the James River. The two rivers meet in Hopewell, Virginia.
The gentle landscape and topography at Appomattox Court House National Historical Park are defined by the local geology and hydrology. This setting historically dictated the placement of towns, strategies and encampment of troops, escape routes, river crossings, and railroads, as well as the development of outlying areas. In many Civil War maneuvers, an advantage was held by those familiar with the terrain; the ability to utilize the natural features of the area and manipulate the focal points, gaps, ravines, cuts, hills, and ridges could determine the outcome of a battle. In addition to influencing battles, the landscape and topography also affected how troops and supplies were transported during the Civil War.
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Geologic Structures The rocks of the area have a complex deformational and metamorphic history with at least four distinct periods of folding Marr and Sweet Large-scale regional folds include the Whispering Creek anticline and the Long Island syncline, both located east of Appomattox Marr Recent mapping south of Appomattox Court House National Historical Park revealed a northern extension of the Carolina Slate Belt along a simple upright northeast-trending isoclinal syncline called the Dryburg syncline.
It is part of the Virgilina synclinorium complex that stretches south into North Carolina and contains greenschist facies, metamorphosed volcanic, volcaniclastic, and sedimentary rocks Hackley et al. Folding and metamorphism of this structure likely occurred during the Alleghanian Orogeny. Appomattox Court House National Historical Park sits atop bedrock that includes the Fork Mountain Formation; the bedrock contains porphyroblastic aluminosilicate mica schist, garnet-bearing biotite gneiss, and amphibolite, as well as a band of greenstone and amphibole gneiss, with an interlayered belt of felsic metatuff, mica schist, and gneiss Virginia Division of Mineral Resources Permeating through the regional rock units are small-scale faults, fractures, mylonite zones, foliation, and other deformation features.
Foliation is commonly wavy, defined by thin alternating dark and light mineral bands Nelson et al. Small-scale joints and fractures are ubiquitous in the rocks beneath the park. Most deformation fabrics follow the northeast-southwest regional structural trend. Geologic Processes and the Historic Landscape Maintaining this Civil War landscape often means resisting natural geologic changes, and this presents several management challenges. Geologic processes such as chemical weathering, seismicity, and slope erosion are constantly changing the landscape at the park.
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