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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 a combination cement-making plant and waste processing plant near Paulding in northwestern Ohio. The cement plant uses rocks that are quarried adjacent to the cluster of buildings. The Paulding Quarry opened in 1949.
Locality: Paulding Quarry (= Lafarge Paulding Quarry), north-northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 51.44" North latitude, 84° 36' 16.82" West longitude)
March 29, 2024. Truck 2, Rescue 2, and Rescue 9 along with Metro Atlanta EMS, and Hiram Police responded to an overturned vehicle near Wellstar Paulding Hospital.
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)
Built in 2006-08 using the designs of Facility Group of Smyrna, the Paulding County Courthouse is located on the southwestern edge of Dallas, 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.
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)
Every lighting inside and Out has been replaced with LED lighting. All of the fixtures were retrofitted and the outdoor wallpacks were completely replaced with new fixtures. They are saving well over %500 per month on electricity alone
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)
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 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 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)
#23, Rickey Paulding, Forward von den EWE Baskets Oldenburg in Aktion während des Derbys zwischen den EWE Baskets Oldenburg und den Eisbären Bremerhaven
Foto: Ulf Duda
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