Class A; August 1969; West Virginia, McDowell County
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Well there you have it, drought and Bigfoot behavior in daylight documented. The creek had dried up, it was seen stooping at a spring. Her poor
sister, a little PTSD maybe?
sister, a little PTSD maybe?
Interesting. . .I believe this woman saw something out of the ordinary that day. Sounds like a credible story. With so little else to go on, I'm not sure what else to say (think).
Wow! Even today that area is very remote, wild, and rugged. A small town is in the area, but still sparsley populated and mountainous. I have no problem believing that something could be living up in those thar hills....
Interesting the grandmother knew about the BF.
QUOTE(georgerm @ Jul 19 2009, 11:22 AM) 
Interesting the grandmother knew about the BF.
I think a lot of our ancestors who lived out in the very rural and isolated areas of earlier times, probably either had a first hand experience with them or knew somebody who did. Of course they did not call it BF, but I suspect that the creature was known amongst the locals.
Odd that no mention of hurricane Camille, but perhaps the incident happened prior to the hurricane
McDowell county is shown as the southern most county is WV. Here is a map showing the location. I couldn't get it to post. http://www.city-data.com/county/McDowell_County-WV.html
Here is a map of hurricane Camille's path from NOAA
QUOTE
http://sciencepolicy.colorado.edu/about_us...lle/report.html
The Virginia Floods
Camille's remnants moved north-northeastward through central Kentucky and eastward through extreme southern West Virginia and southern Virginia. As Camille reached Kentucky, Tennessee, and Ohio, it encountered large masses of moisture-laden air and again became active (OEP 1969). Late Tuesday August 19, the tropical depression produced torrential rainfall that caused flash floods and landslides along the eastern slopes of the Blue Ridge Mountains and record flooding in Virginia's James River watershed (USACE 1970).
The heavy rains began about 7 p.m. on August 19 and continued without a decrease in intensity for the next eight hours. By 10 p.m., a band of rain and thunderstorms some 40 to 50 miles wide extended in a general east-west orientation from the vicinity of White Sulphur Springs, West Virginia, to Fredericksburg, Virginia (Figure 9). Around midnight, the low-pressure center intensified as it moved eastward into Virginia along a track south of Roanoke and Lynchburg (ESSA, 1969b). Rainfall to the north and east of the low-pressure center increased rapidly along the western slopes of the Blue Ridge Mountains, with more than 10 inches accumulating at Clifton Forge, Virginia. The rainfall continued to intensify on the eastern slopes of the Blue Ridge Mountains until it reached catastrophic proportions (ESSA, 1969b).
The rains, flash floods, and rain-induced landslides accompanying the storm's passage led to the worst natural disaster ever to strike Virginia (Figure 10). Most of the residents of the mountain hollows, hamlets, and towns were asleep during the fatal hours of the storm. Little warning was possible -- only one report of excessive rain was received by the Weather Bureau during the night from a cooperative observer (DeAngelis 1969). Rapidly rising streams and landslides caused by the rainfall not only destroyed homes as the occupants slept, but communication lines and roads were destroyed, preventing downstream inhabitants from being alerted. Large uprooted trees acted as battering rams, crashing through houses and overturning automobiles.
The Virginia Floods
Camille's remnants moved north-northeastward through central Kentucky and eastward through extreme southern West Virginia and southern Virginia. As Camille reached Kentucky, Tennessee, and Ohio, it encountered large masses of moisture-laden air and again became active (OEP 1969). Late Tuesday August 19, the tropical depression produced torrential rainfall that caused flash floods and landslides along the eastern slopes of the Blue Ridge Mountains and record flooding in Virginia's James River watershed (USACE 1970).
The heavy rains began about 7 p.m. on August 19 and continued without a decrease in intensity for the next eight hours. By 10 p.m., a band of rain and thunderstorms some 40 to 50 miles wide extended in a general east-west orientation from the vicinity of White Sulphur Springs, West Virginia, to Fredericksburg, Virginia (Figure 9). Around midnight, the low-pressure center intensified as it moved eastward into Virginia along a track south of Roanoke and Lynchburg (ESSA, 1969b). Rainfall to the north and east of the low-pressure center increased rapidly along the western slopes of the Blue Ridge Mountains, with more than 10 inches accumulating at Clifton Forge, Virginia. The rainfall continued to intensify on the eastern slopes of the Blue Ridge Mountains until it reached catastrophic proportions (ESSA, 1969b).
The rains, flash floods, and rain-induced landslides accompanying the storm's passage led to the worst natural disaster ever to strike Virginia (Figure 10). Most of the residents of the mountain hollows, hamlets, and towns were asleep during the fatal hours of the storm. Little warning was possible -- only one report of excessive rain was received by the Weather Bureau during the night from a cooperative observer (DeAngelis 1969). Rapidly rising streams and landslides caused by the rainfall not only destroyed homes as the occupants slept, but communication lines and roads were destroyed, preventing downstream inhabitants from being alerted. Large uprooted trees acted as battering rams, crashing through houses and overturning automobiles.
McDowell county is shown as the southern most county is WV. Here is a map showing the location. I couldn't get it to post. http://www.city-data.com/county/McDowell_County-WV.html
Here is a map of hurricane Camille's path from NOAA
Great point about Camille coming through that month. I suspect that this did happen before the hurricane. Seems like that would have been mentioned if the incident had occurred afterwards.
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