FrograilStanly County, North Carolina, and it's Railroads
Geology and Geography. Truly, the history of Stanly County's railroads began millions of years ago. Two events happened over geologic time which had profound influence on the county's railroads: On the eastern edge of the county, and extending maybe 30 miles further east, a series of volcanoes commenced to do their thing, leaving behind a fairly large area including what are now Morrow Mountain State Park and the Uwharrie National Forest. These are wonderful places to hike and enjoy nature, but they are terrible places to build railroads. Just to the north (today's I-85 corridor), and just to the south (today's US-74 corridor), there are much better, more logical routes. Further to the east, the rocky "fall line" abruptly separates the piedmont from the coastal plain. This is no mere curiosity, as the plain goes all the way to, and quite a ways out into, the ocean. Again, this makes for great hiking, swimming, beer drinking, etc., but it makes for lousy deep sea ports. Compared to Boston, New York, Philadelphia, Baltimore, Savannah, Norfolk (especially), and to a lesser extent Wilmington and Charleston, the eastern North Carolina ports of New Bern, Morehead City and Beaufort were simply not created equal, and railroad activity to and from these latter secondary ports paled behind that of traffic to the great natural ports of the east coast. There are other North Carolina geological features which have a fairly minor impact on Stanly County's railroading history: Obviously, the mountains to the west precluded any efficient, easily constructed east-west route across the state. There are some pretty dramatic rivers in the state, and crossing them required routes which took advantage of the most logical crossing points. Chief rivers which bore an indirect effect on Stanly County's eventual railroads were the Roanoke (a real beast, and its crossing location pretty much dictated the railroad map in the state for many, many years), and the Yadkin/Pee Dee (a big river, which, before a series of dams was constructed, was one big-time tough cookie. This river forms the eastern boundary of Stanly County, and is really an after effect of the volcanic period mentioned above.). Because of the above, there were three fairly logical, relatively easy places to build railroads in the state:
All three routes were actually built, although the NE-SW route was more politically than geographically dictated, and today's rather strange-looking "North Carolina Railroad" is the result.
As a general comment, most historians dealing specifically with the Stanly County region seem to regard the coming and development of the railroad as one of those things to be taken for granted; the authors of Stanly County's definitive history are no exception. While devoting an incredible 108 pages to the origin, development and status of the various churches in the county, Sharpe and Pepper devote a grand total of 8 paragraphs to the county's railroads!! However, they indicate they do realize the tremendous effect the railroads had on the county:
It seems obvious that a pretty large percentage of the churches Sharpe and Pepper detail so meticulously would never have been in existence had not the coming of the railroads so broadly increased the standard of living in the county. Likewise, Sharpe and Pepper devote 20 pages to the development of Pfeiffer College (very interesting reading, by the way), but fail to mention the obvious connection between the school (actually now a full university) and the railroad. When the school (them Mitchell Home) was relocated from Lenoir to Misenheimer in 1910, certainly one of the most important considerations to the school's leaders must have been the fact that the town of Misenheimer was directly on the railroad line from Salisbury to Albemarle. It would have been difficult, indeed, for the school and subsequent college to grow without that vital connection to the outside world. To read about the history of the railroads themselves, go to the Frograil Stanly County Railroad History page, which is here. | ||||||||