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North Paulding High Wolfpack Cheer Squad performs for the crowd.

Paulding County. Photo by S Are, Nov. 2014.

Part of the Post Mark Collectors Club (PMCC) collection.

The leaves are starting to turn locally.

Near Bluffy Creek, Paulding Forest, GA

The North Paulding Cheerleading Bleacher Club takes the field accompanied by the big girls!

 

Young Miss Borders in the group

Formerly an Apothecary and Hallmark in 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.

 

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 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)

 

Water flowing over Bond Falls on the Middle Branch Ontonagon River near Paulding, MI.

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)

 

North Paulding Cheerleading Bleacher Club w/Young Miss Borders

North Paulding High Wolfpack Cheer Squad performs for the crowd.

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)

 

A lone motorcycle in the distance on Harmony Church Road in Paulding County, Georgia

 

On this day in 1941 just before 0800, 188 U.S. aircraft were destroyed; 2,403 Americans were killed and 1,178 others were wounded by the Imperial Japanese Navy against the United States naval base at Pearl Harbor. .

And now here is the rest of the story:

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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)

 

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 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. 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)

 

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)

 

Took the kids to see the Paulding Light in the Upper Peninsula.

VID00003

#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. ]

[#0,26,121#]

Paulding County Court House

#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 statue is located in Yoctangee Park, just north of the historic commercial district in downtown Chillicothe.

 

For more information regarding this statue please follow this link: en.wikipedia.org/wiki/John_Paulding_(sculptor)

 

Chillicothe, Ohio is a charming small town located in the south of the state, between Columbus and Portsmouth on the Scioto River. It has served as the seat of Ross County since the late 18th century, was the capital of the Northwest Territory (1800-03), and was Ohio's first and third state capital (1803-10 and 1812-16).

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