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Waynesboro Formation

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Journal Article
Journal: Geosphere
Published: 01 June 2012
Geosphere (2012) 8 (3): 685–702.
... is interpreted as being above the Salina (salt) décollement. This magnitude of shortening is 14 km greater than the amount of displacement on the Nittany Anticlinorium, the northernmost structure of the fold-thrust belt that cuts upsection from the Cambrian Waynesboro Formation to the Silurian Salina décollement...
FIGURES | View All (13)
Series: Memoir, Memoir
Published: 01 January 2012
DOI: 10.1306/13331499M980271
EISBN: 9781629810201
... 1 (Lower Cambrian Chilhowee Group fluvial rift clastics grading up into shelf siliciclastics) underlies the passive margin carbonates. Supersequence 2 consists of the Lower Cambrian Shady Dolomite–Rome-Waynesboro Formations. This is a shallowing-upward ramp succession of thinly bedded to nodular...
FIGURES | View All (14)
Series: Memoir, Memoir
Published: 01 January 2012
DOI: 10.1306/13331500M983500
EISBN: 9781629810201
... coincided with the development of a rimmed platform that would persist throughout much of the Cambrian and Early Ordovician. At the end of deposition of the Waynesboro Formation, the platform became subaerially exposed because of the Hawke Bay regression, bringing the Sauk I supersequence to an end...
FIGURES | View All (22)
Journal Article
Journal: GSA Bulletin
Published: 01 November 2004
GSA Bulletin (2004) 116 (11-12): 1499–1514.
... by the removal of salt. The trend of the central and northern synclinorium reflects the location of Upper Silurian Salina salt. In the southern synclinorium, the salt-collapse structure translated northwestward over a thrust ramp joining detachments in the Cambrian Waynesboro Formation and the Salina Group...
FIGURES | View All (12)
Journal Article
Journal: AAPG Bulletin
Published: 15 November 2020
AAPG Bulletin (2020) 104 (11): 2379–2399.
.... These structures allow us to interpret a pathway of triangle zones (a combination of two thrusts with the same detachment and with opposing vergence such that they form a triangular zone) that transfer slip from the basal decollement in the Cambrian Waynesboro Formation to the overlying Ordovician Reedsville...
FIGURES | View All (13)
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1986
AAPG Bulletin (1986) 70 (11): 1674–1684.
... and an increase in displacement of thrust sheets floored in the Waynesboro Formation. However, the Massanutten-Blue Ridge and Pulaski sheets, seated primarily in incompetent Ordovician strata and bounded by the North Mountain and Pulaski fault systems, respectively, extend through the trend change zone...
FIGURES | View All (17)
Series: GSA Memoirs
Published: 01 September 2010
DOI: 10.1130/2010.1206(21)
... a more NW-directed shortening and resulted in rapid loading of the Paleozoic section in the footwall by 7–10 km of rock that extended 20–30 km toward the hinterland from the North Mountain thrust ramp. The loading of the Paleozoic section resulted in overpressuring of Cambrian Waynesboro décolle-ment...
Series: GSA Field Guide
Published: 01 January 2017
DOI: 10.1130/2017.0047(01)
EISBN: 9780813756479
.... Figure 6. Bedrock geologic map of the northern portion of the Blue Ridge Parkway, from near Waynesboro, Virginia, at the northern end of the Blue Ridge Parkway to the James River (~MP 64), showing fi eld-trip stops along the route. Abbreviations: c —location of columnar jointing in Catactin Formation...
FIGURES | View All (36)
Journal Article
Journal: Economic Geology
Published: 01 September 1958
Economic Geology (1958) 53 (6): 722–736.
...Edmond George Otton; Claire Alice Richardson Abstract Limestone rocks are an important source of ground water in the Piedmont and Appalachian areas of Maryland. The major limestone aquifers are the Cockeysville and Wakefield marbles and the Silver Run, Tomstown, Frederick, Grove, Waynesboro...
Journal Article
Published: 01 December 1993
Bulletin of Canadian Petroleum Geology (1993) 41 (4): 373–388.
... Canada (Hoffman, 1975; Grotzinger, 1986); the Lower Cambrian Monkton, Waynesboro and Rome format ions of the Appalachians (Colton, 1970; Read, 1989); the Upper Cambrian Nol ichucky Formation of the southern Appalachians (Markello and Read, 1981); and the Lower to Middle Cambrian Carrera Formation...
Series: Memoir, Memoir
Published: 01 January 2012
DOI: 10.1306/13331502M983502
EISBN: 9781629810201
... Dolostone (Figure 2 ), Hardyston, Waynesboro, and Rome Formations, which occur in the western Appalachians from western Newfoundland to Georgia. The upper Lower Cambrian of the New York promontory shows a cumulative eustatic rise (Cheshire– Dunham Formations) before the Hawke Bay regression, which...
FIGURES | View All (7)
Image
Karst feature locations (green centroids) documented during the current stu...
Published: 01 February 2016
; wb = Waynesboro Formation; wbt = Waynesboro & Tomstown Formations; e = Elbrook Formation; O co = Conococheague Formation; Ob = Beekmantown Group; Oeln = New Market, Lincolnshire and Edinburg Formations; DSu 5 Silurian-Devonian Carbonates, undivided.)
Image
Karst feature locations (green centroids) documented during the current stu...
Published: 01 February 2016
; wb = Waynesboro Formation; wbt = Waynesboro & Tomstown Formations; e = Elbrook Formation; O co = Conococheague Formation; Ob = Beekmantown Group; Oeln = New Market, Lincolnshire and Edinburg Formations; DSu 5 Silurian-Devonian Carbonates, undivided.)
Image
Karst feature locations (green centroids) documented during the current stu...
Published: 01 February 2016
; wb = Waynesboro Formation; wbt = Waynesboro & Tomstown Formations; e = Elbrook Formation; O co = Conococheague Formation; Ob = Beekmantown Group; Oeln = New Market, Lincolnshire and Edinburg Formations; DSu 5 Silurian-Devonian Carbonates, undivided.)
Image
Karst feature locations (green centroids) documented during the current stu...
Published: 01 February 2016
; wb = Waynesboro Formation; wbt = Waynesboro & Tomstown Formations; e = Elbrook Formation; O co = Conococheague Formation; Ob = Beekmantown Group; Oeln = New Market, Lincolnshire and Edinburg Formations; DSu 5 Silurian-Devonian Carbonates, undivided.)
Image
Karst feature locations (green centroids) documented during the current stu...
Published: 01 February 2016
; wb = Waynesboro Formation; wbt = Waynesboro & Tomstown Formations; e = Elbrook Formation; O co = Conococheague Formation; Ob = Beekmantown Group; Oeln = New Market, Lincolnshire and Edinburg Formations; DSu 5 Silurian-Devonian Carbonates, undivided.)
Image
Karst feature locations (green centroids) documented during the current stu...
Published: 01 February 2016
; wb = Waynesboro Formation; wbt = Waynesboro & Tomstown Formations; e = Elbrook Formation; O co = Conococheague Formation; Ob = Beekmantown Group; Oeln = New Market, Lincolnshire and Edinburg Formations; DSu 5 Silurian-Devonian Carbonates, undivided.)
Image
Karst feature locations (green centroids) documented during the current stu...
Published: 01 February 2016
; wb = Waynesboro Formation; wbt = Waynesboro & Tomstown Formations; e = Elbrook Formation; O co = Conococheague Formation; Ob = Beekmantown Group; Oeln = New Market, Lincolnshire and Edinburg Formations; DSu 5 Silurian-Devonian Carbonates, undivided.)
Image
—Stratigraphy of Middle and Upper Cambrian sediments from central Pennsylva...
Published: 01 August 1948
group, and Mines likewise has been so classed by some authors. Waynesboro formation may be Lower Cambrian throughout.
Series: GCSSEPM, GCSSEPM
Published: 01 June 1991
DOI: 10.5724/gcs.90.11.0141
EISBN: 978-0-9836097-2-8
... deposits, with the Byram consisting largely of fossiliferous shelf sands and the Bucatunna consisting of sparsely fossiliferous estuarine clays. A fluvial channel sand, the Waynesboro Sand, occurs within the Bucatunna Formation of eastern Mississippi (Wayne County), where it cuts through the Byram...