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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 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 statue is located in Pershing Park, next to the Sage Public Library in Bay City.
For more information regarding this statue please follow this link: en.wikipedia.org/wiki/John_Paulding_(sculptor)
Prior to 1905, this part of Bay City, which is located to the west of the Saginaw River, was a separate incorporated community called West Bay City. It was annexed to the rest of the municipality of Bay City.
Bay City, Michigan is a small city located in the central eastern part of the state. It is the northeastern-most of the Tri-Cities, and the least populated of the three. The community, which serves as the seat of Bay County, derives its name from its position of Saginaw Bay.
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 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.
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 a combination cement-making plant and waste processing plant near Paulding in northwestern Ohio. The cement plant uses rocks that are quarried nearby. 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)
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)
#23, Rickey Paulding, Forward von den EWE Baskets Oldenburg in Aktion während des Pokalspiels zwischen den Artland Dragons und den EWE Baskets Oldenburg Foto: Ulf Duda
[ (c) fotoduda sports and more, Muehlenteichstr.17, 26316 Varel (G e r m a n y), Tel.: +49-176 210 29 819 ; info@pressefotoduda.de, Konto: Raiffeisen-Volksbank Varel-Nordenham eG - Kto.-Nr.: 100 559 602, BLZ: 282 626 73; - Jede Nutzung des Fotos ist honorarpflichtig gemaess derzeit gueltiger MFM Liste zzgl. Mehrwertsteuer. Urhebervermerk wird nach Paragraph 13 UrhG ausdruecklich verlangt. Belegexemplar erforderlich! Bei Verwendung des Fotos ausserhalb journalistischer Zwecke bitte Ruecksprache mit dem Fotografen halten. - Each usage of the photo requires a royalty fee in accordance to MFM and byline Ulf Duda. No model release. For any usage other than editorial purposes please contact the author. ]
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#23, Rickey Paulding, Forward von den EWE Baskets Oldenburg in Aktion während des Spiels zwischen den EWE Baskets Oldenburg und den LTi GIESSEN 46ers
Foto: Ulf Duda
[ (c) fotoduda sports and more, Muehlenteichstr.17, 26316 Varel (G e r m a n y), Tel.: +49-176 210 29 819 ; info@pressefotoduda.de, Konto: Raiffeisen-Volksbank Varel-Nordenham eG - Kto.-Nr.: 100 559 602, BLZ: 282 626 73; - Jede Nutzung des Fotos ist honorarpflichtig gemaess derzeit gueltiger MFM Liste zzgl. Mehrwertsteuer. Urhebervermerk wird nach Paragraph 13 UrhG ausdruecklich verlangt. Belegexemplar erforderlich! Bei Verwendung des Fotos ausserhalb journalistischer Zwecke bitte Ruecksprache mit dem Fotografen halten. - Each usage of the photo requires a royalty fee in accordance to MFM and byline Ulf Duda. No model release. For any usage other than editorial purposes please contact the author. ]
[#0,26,121#]
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)
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.
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)
Spiriferid brachiopod in the Devonian of Ohio, USA.
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).
Classification: Animalia, Brachiopoda, Articulata (a.k.a. Rhynchonelliformea), Spiriferida
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)
I'm sure this offends someone passing by on US-127 every day. Doesn't bug me much, but I'm not an Native American. Heck, if it said "Home Of The Polacks", I probably wouldn't care either. The indian on here looks like he's having gas pains. I think this was near Pauling, OH, but don't start writing them, since I could be wrong. As you can see, it was snowing like mad, so I wasn't paying attention that closely. ...other than to see this sign. Oh, they have a teepee on their sports field too. That should complete things for ya.
In the woodlands near Atlanta, a small buckeye tree with red flowers is locally common. However, the colors are variable -- ranging from quite red to only slightly red. Apparently these are all hybrids between the Red Buckeye (Aesculus pavia) and the Painted Buckeye (Aesculus sylvatica). Pickett's Mill 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.
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 Spiels zwischen den EWE Baskets Oldenburg und Phoenix Hagen
Foto: Ulf Duda
[ (c) fotoduda sports and more, Muehlenteichstr.17, 26316 Varel (G e r m a n y), Tel.: +49-176 210 29 819 ; info@pressefotoduda.de, Konto: Raiffeisen-Volksbank Varel-Nordenham eG - Kto.-Nr.: 100 559 602, BLZ: 282 626 73; - Jede Nutzung des Fotos ist honorarpflichtig gemaess derzeit gueltiger MFM Liste zzgl. Mehrwertsteuer. Urhebervermerk wird nach Paragraph 13 UrhG ausdruecklich verlangt. Belegexemplar erforderlich! Bei Verwendung des Fotos ausserhalb journalistischer Zwecke bitte Ruecksprache mit dem Fotografen halten. - Each usage of the photo requires a royalty fee in accordance to MFM and byline Ulf Duda. No model release. For any usage other than editorial purposes please contact the author. ]
[#0,26,121#]
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. 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 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)