By Steven A. Goldberg, J. Robert Butler(auth.)
About The Product
Published via the yank Geophysical Union as a part of the Field journey Guidebooks Series.
This box journey is meant to illustrate the foremost lithologic sequences and the most tectonic and metamorphic positive factors in a phase of the Blue Ridge geologic province in northwestern North Carolina and adjoining components of Tennessee and Virginia. a few of the box destinations selected for the six-day box journey emphasize geological features universal to a lot of the southern and significant Appalachians. many of the localities to be visited are within the Blue Ridge, with a few within the Valley and Ridge province to the northwest and the Brevard sector and internal Piedmont to the southeast. The journey presents an summary of the anatomy and evolution of terranes subjected to the subsequent tectonic episodes: past due Proterozoic rifting, the advance of oceanic lithosphere, the following closure of this ocean, and additional amendment via a number of episodes of Paleozoic deformation and metamorphism.
Read Online or Download Geological Cross-Section Through Part of the Southern Appalachian Orogen: Inner Piedmont to Valley and Ridge (North Carolina, Tennessee and Virginia), July 20-26, 1989 PDF
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Additional info for Geological Cross-Section Through Part of the Southern Appalachian Orogen: Inner Piedmont to Valley and Ridge (North Carolina, Tennessee and Virginia), July 20-26, 1989
C~brian ffi • precambrian (3 IIIII hady Fm" Chilhowee Grp" II D  Grandfather Mountain Window: Precambrian basement and late'Precambrian metasedimentary and metavolcanic rocks" ::~:~*~~::::::::~ Boundary between Pumpkin Patch and Beech Mountain thrust sheets, Beech Granite Fluorite-Alkali Granite Bakersville Gabbro Precambrian Crystalline Basement FIGURE 15 Geologic map of area northwest of the Grandfather Mountain window, western North Carolina.
Fiamme have been recognized in thin section from this unit. Roadlog Return to US 58, and travel west. The route traverses Precambrian basement until the community of Haw Orchard, where the unexposed contact between basement and Mount Rogers Formation ·occurs [Rankin, 1967]. From the contact near Haw Orchard westward towards the intersection of US 58 and VA 600 (turnoff to Whitetop Mountain), roadside exposures will be mainly greywackes, conglomerates, and siltstones of the lower Mount Rogers Formation.
9 miles into Jefferson to the Eldreth motel. DAY 3 Roadlog Leave Eldreth Motel and tum right on US 221. 7 mile to intersection with Blue Ridge Parkway. 4 miles to intersection with US 221-321 near Blowing· Rock. Overlooks along this part of the Parkway· have good views eastward across the Blue Ridge front and the distant Piedmont. 6 mile to large outcrop on east side of highway. Stop 3-1: Blowin2 Rock Gneiss Be extremely careful of the traffic- this is a busy highway! This large outcrop is Blowing Rock Gneiss cut by quartz veins, pegmatite dikes, and mafic dikes.