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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)
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. Overlying the Dundee is the Silica Formation, also Middle Devonian. The Silica is richly fossiliferous and consists of interbedded limestone and shale.
Seen here are leftover wires associated with blasting equipment.
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)
May 1, 2024. Paulding County, GA's Engine & Rescue 9 crew are utilizing a warm sunny day to do some company training.
Engine 9 is a 2022 Frieghtliner M2/Rosenbaur, 750gal/1250gpm and serves the Pine Valley Community.
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)
Discontinued 2014. Paulding County. Photo by S Are, Mar. 2014.
Part of the Post Mark Collectors Club (PMCC) collection.
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 part of the 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)
Fossil coral & brachiopod in the Devonian of Ohio, USA.
At top is a coral fossil. Corals are essentially sea anemones (polyps) that make a skeleton, which is usually mineralized. Most corals are colonial, but some are solitary. This is a solitary rugose coral, also known as a "horn coral", in reference to the tapered solid skeleton (best seen on weathered-out specimens).
At lower left is a spiriferid brachiopod fossil. Brachiopods are sessile, benthic, filter-feeding, marine invertebrates. They first appear in Cambrian rocks and were abundant in Earth's oceans throughout the Paleozoic. They were also common in Mesozoic oceans, but are scarce in modern oceanic biotas. Brachiopods have two shells, called valves, that are usually calcareous (made of calcite - CaCO3 - calcium carbonate). Each shell of a brachiopod is bilaterally symmetrical, unlike each shell of a bivalve (clam).
Stratigraphy: Silica Formation, Middle Devonian
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)
Paulding County (GA) Hamfest, September 2008
This is the "Olympic Style" finishing order of the August 10 Meter LXPedition, KI4SGU, KJ4FIL and K4ESA
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)
She's such a cutie, and the resident lop eared rabbit at The Gardens of Paulding, where my father in law is living.
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)
The Spirit Of South Paulding, Georgia, USA.
From a collection of photographs taken at the 29th London New Year's Day Parade 2015 (LNYDP 2015). We were standing on opposite sides of the road in Piccadilly near the junction with Regent Street. The parade featured bands and participants from all over the world, along with representatives from London Boroughs whose theme was "London on the Move". See www.lnydp.com for more information.
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)
Paulding County Fire/Rescue Engine 1, Rescue 1, Squad 1, Truck 11, Rescue 4, and the command staff, along with Paulding County Sheriff’s Office, City of Dallas GA Police Department, Hiram Police Department, Metro Atlanta EMS, and the Georgia State Patrol were all in attendance at the Paulding County Government complex for a wonderful turnout at the 23rd annual 9/11 Remembrance ceremony!
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)