![]() ![]() Donations can be made at Ashland County Community Foundation at 41 or mailed to Ashland County Community Foundation 300 College Ave Ashland, OH 44805 or a charity of one’s choice.Ī memorial service celebrating Dave’s life will be held at Saluda Shoals Park in Columbia, SC on Jat 11:00am. Downie Scholarship Fund furthering teacher education in Ashland, OH. Baugh and all the doctors and nurses at Advanced Heart Health clinic at Prisma Richland Hospital in Columbia, SC.įamily requests in lieu of flowers donations be made to the David III and Marlene F. ![]() Special thanks go to Prisma Health Hospice, also Dr. Dave was preceded in death by his wife of 47 years Marlene (Puni) Downie and his infant grandson David Downie V.ĭave donated his body to MUSC School of Medicine where two of his grandsons graduated medical school. He was the proud and loving grandfather of 9 and was a beloved great-grandfather of 18 as well as many nieces and nephews. Downie of Columbia, SC, son David Downie IV (Barbara) of Columbia, SC and his two daughters Diana Downie-Bristow (Mike) of Wickliffe, OH and Debra (Downie) Paden (Richard) of Wickliffe, OH. He was also an avid woodworker and enjoyed painting crafts for the family.ĭave is survived by his loving wife Peggy R. He loved people and always enjoyed a good party. Dave’s favorite times were times spent with his family. Dave was a member of the Dulcimores a musical group in Columbia, SC as well as a lifetime member of the Ashland, OH Elks. During this time, he received many awards including various local school district volunteer and community awards as well as South Carolina’s highest honor for volunteer and community service, “The Order of the Silver Crescent”. He spent 24 years teaching special needs children how to read, play chess and play the dulcimer. Dave embraced his Scottish heritage by being involved with Scottish Clan Grant #17 in Cleveland, OH.Īfter moving to South Carolina in 1987 Dave volunteered with Nursery Road Elementary School in Columbia, SC. He also volunteered with Camp Inspiration Hills Outdoor Education Program (Camp Nuhop) for 10 years. Dave graduated from high school in Ashland, OH and married his high school sweetheart, “Puni” in 1951.ĭave was involved with children throughout his entire life by volunteering with youth baseball, bowling and boy scouts. He was born on Januin Cleveland, OH to the late David Downie II and Mary Wallace Downie. ![]() Combined stratigraphic and structural cross section through Pettipiece Ridge which lithologically distinguishes it from unit 6.David Downie III, 91, passed away peacefully at his home in Columbia, SC on May 11, 2022. It contains calc-silicates, impure and graphitic marbles, quartzites, and minor pelites. The contact between units 6 and 7 (these units are referred to by British Columbia Hydro as "West" and "East Series" respectively) has been the focus of attention for a long time as it was interpreted as a faulted contact, with the fault following the trace of the river valley. However, our mapping just north of the slide and in adit 2 has shown that the contact is conformable but gradational over a distance of tens of metres. 4) the contact trends north parallel to the river, but swings westward and crosses the river somewhere near the centre of the slide and is exposed in the adit, implying stratigraphic continuity across this part of the Columbia River. An impure marble bed within unit 7 traced from the east bank to the vicinity of the adit and north to Fissure Creek (Fig. 4) confirms stratigraphic continuity across the Columbia River. The presence of graded grits in units 4,5, and 6, lack of repetition of stratigraphic units, and unfaulted and generally gradational contacts are evidence that units 3-7 comprise a right-way-up stratigraphic succession. Units 8,9, and 10 comprise a 600 m thick succession of quartzites, quartzo-feldspathic grits and Correlation with regional stratigraphy of Frenchman Cap confirms this interpretation (Brown and Psutka 1979 Brown 1980). The displacement of a large slow-moving landslide is accompanied by slope damage, such as fractures, tension cracks, and slope bulging. Studies of these features provide insight into the mechanisms responsible for the deformation. In this paper, we investigate slope damage at the Downie Slide, a very large landslide in British Columbia, Canada, that is slowly moving along two shear zones subparallel to the ground surface. Structural geology, and particularly the morphology of the lower shear zone, strongly controls the deformation and, in turn, the observed internal and surficial slope damage features. We use aerial and underground adit laser scanning and photogrammetry to characterize the geometry of the landslide. ![]()
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