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This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone.
The upper quarry wall seen here consists of interbedded fossiliferous limestones and shales of the Middle Devonian Silica Formation. The fossils are typical mid-Paleozoic marine invertebrates such as brachiopods, bryozoans, corals, crinoids, and trilobites. Below the Silica is the Dundee Limestone, which lacks interbedded shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone.
The upper quarry wall seen here consists of interbedded fossiliferous limestones and shales of the Middle Devonian Silica Formation. The fossils are typical mid-Paleozoic marine invertebrates such as brachiopods, bryozoans, corals, crinoids, and trilobites. Below the Silica is the Dundee Limestone, which lacks interbedded shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
Taken from many sources, and facebook photos, these are photos from the fire that took place in Paulding, Ohio. Jan 15, 2012. Demolishing the Hotel Barnes, Paulding Ohio
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone.
The upper quarry wall seen here consists of interbedded fossiliferous limestones and shales of the Middle Devonian Silica Formation. The fossils are typical mid-Paleozoic marine invertebrates such as brachiopods, bryozoans, corals, crinoids, and trilobites. Below the Silica is the Dundee Limestone, which lacks interbedded shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone.
The upper quarry wall seen here consists of interbedded fossiliferous limestones and shales of the Middle Devonian Silica Formation. The fossils are typical mid-Paleozoic marine invertebrates such as brachiopods, bryozoans, corals, crinoids, and trilobites. Below the Silica is the Dundee Limestone, which lacks interbedded shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone.
The upper quarry wall seen here consists of interbedded fossiliferous limestones and shales of the Middle Devonian Silica Formation. The fossils are typical mid-Paleozoic marine invertebrates such as brachiopods, bryozoans, corals, crinoids, and trilobites. Below the Silica is the Dundee Limestone, which lacks interbedded shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone. Seen here is the Dundee in the lower part of the working quarry wall. Overlying the Dundee at this locality (not visible in the picture) is the Silica Formation (also Middle Devonian), which consists of interbedded fossiliferous limestones and shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone.
The upper quarry wall seen here consists of interbedded fossiliferous limestones and shales of the Middle Devonian Silica Formation. The fossils are typical mid-Paleozoic marine invertebrates such as brachiopods, bryozoans, corals, crinoids, and trilobites. Below the Silica is the Dundee Limestone, which lacks interbedded shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone.
The upper quarry wall seen here consists of interbedded fossiliferous limestones and shales of the Middle Devonian Silica Formation. The fossils are typical mid-Paleozoic marine invertebrates such as brachiopods, bryozoans, corals, crinoids, and trilobites. Below the Silica is the Dundee Limestone, which lacks interbedded shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone.
The blast rubble seen here is principally derived from the Silica Formation, which overlies the Dundee Limestone. The Silica Formation is also Middle Devonian and consists of richly fossiliferous interbedded limestones and shales. The fossils are typical mid-Paleozoic marine invertebrates such as brachiopods, bryozoans, corals, crinoids, and trilobites.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone.
The upper quarry wall seen here consists of interbedded fossiliferous limestones and shales of the Middle Devonian Silica Formation. The fossils are typical mid-Paleozoic marine invertebrates such as brachiopods, bryozoans, corals, crinoids, and trilobites. Below the Silica is the Dundee Limestone, which lacks interbedded shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone.
The upper quarry wall seen here consists of interbedded fossiliferous limestones and shales of the Middle Devonian Silica Formation. The fossils are typical mid-Paleozoic marine invertebrates such as brachiopods, bryozoans, corals, crinoids, and trilobites. Below the Silica is the Dundee Limestone, which lacks interbedded shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone.
The upper quarry wall seen here consists of interbedded fossiliferous limestones and shales of the Middle Devonian Silica Formation. The fossils are typical mid-Paleozoic marine invertebrates such as brachiopods, bryozoans, corals, crinoids, and trilobites. Below the Silica is the Dundee Limestone, which lacks interbedded shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone.
The upper quarry wall seen here consists of interbedded fossiliferous limestones and shales of the Middle Devonian Silica Formation. The fossils are typical mid-Paleozoic marine invertebrates such as brachiopods, bryozoans, corals, crinoids, and trilobites. Below the Silica is the Dundee Limestone, which lacks interbedded shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone.
The upper quarry wall seen here consists of interbedded fossiliferous limestones and shales of the Middle Devonian Silica Formation. The fossils are typical mid-Paleozoic marine invertebrates such as brachiopods, bryozoans, corals, crinoids, and trilobites. Below the Silica is the Dundee Limestone, which lacks interbedded shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone.
The upper quarry wall seen here consists of interbedded fossiliferous limestones and shales of the Middle Devonian Silica Formation. The fossils are typical mid-Paleozoic marine invertebrates such as brachiopods, bryozoans, corals, crinoids, and trilobites. Below the Silica is the Dundee Limestone, which lacks interbedded shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
At the site of the Battle of New Hope Church in the War Between the States, Paulding County, Georgia.
The North Paulding Cheerleading Bleacher Club takes the field accompanied by the big girls!
Young Miss Borders in the group
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone. Overlying the Dundee is the Silica Formation, also Middle Devonian. The Silica is richly fossiliferous and consists of interbedded limestone and shale.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone.
The upper quarry wall seen here consists of interbedded fossiliferous limestones and shales of the Middle Devonian Silica Formation. The fossils are typical mid-Paleozoic marine invertebrates such as brachiopods, bryozoans, corals, crinoids, and trilobites. Below the Silica is the Dundee Limestone, which lacks interbedded shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
Rue Anemone (Thalictrum thalictroides). Pickett's Mill State Historic Park, Paulding County, Georgia.
This statue is located in Oakwood Cemetery, to the southwest of the intersection of Monroe Street and West Michigan Avenue in Saline.
For more information regarding this statue please follow this link: en.wikipedia.org/wiki/John_Paulding_(sculptor)
Saline, Michigan is a small town located to the south of Ann Arbor in southern Washtenaw County.
PAULDING COUNTY AIRPORT, November 8, 2015. - During the transfer of authority ceremony, commanders of the 165th QM and H Co. LRS along side of their guidon salute the American flag during the playing of the national anthem.
Georgia Army National Guard photo by Cpt. William Carraway | released
The North Paulding Cheerleading Bleacher Club takes the field accompanied by the big girls!
Young Miss Borders in the group
Yellow Stargrass (Hypoxis hirsuta), also called Common Goldstar. Pickett’s Mill Battlefield State Historic Site, Paulding County, Georgia.
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone. Seen here is the Dundee in the lower part of the working quarry wall. Overlying the Dundee at this locality (not visible in the picture) is the Silica Formation (also Middle Devonian), which consists of interbedded fossiliferous limestones and shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)
#NWGA #News #NorthWestGA #NorthwestGeorgia Teen found on Paulding roadside likely suicide, hands not tied: spokesman t.co/jHCyBihzap — Paulding Neighbor (PauldingNews) March 13, 2018 (via Twitter twitter.com/RedneckGremlin/status/973611745188171776)
This is the Paulding Quarry in far-northwestern Ohio. The quarry opened in 1949 and the rocks are used to make cement on-site. The target unit is the Middle Devonian Dundee Limestone.
The upper quarry wall seen here consists of interbedded fossiliferous limestones and shales of the Middle Devonian Silica Formation. The fossils are typical mid-Paleozoic marine invertebrates such as brachiopods, bryozoans, corals, crinoids, and trilobites. Below the Silica is the Dundee Limestone, which lacks interbedded shales.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 57.96" North latitude, 84° 37' 21.23" West longitude)