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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)
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
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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. 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 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)
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)
#NWGA #News #NorthWestGA #NorthwestGeorgia Coach, point guard credit each other for helping #Hiram boys basketball team reach Final Four Paulding_Sports t.co/cgjdasRBP4 — Paulding Neighbor (PauldingNews) March 12, 2018 (via Twitter twitter.com/RedneckGremlin/status/973188919754919936)
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)
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 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)
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)
10260 Pamphlet- Pickett’s Mill Battlefield Historic Site, 4432 Mt. Tabor Church Rd., Dallas, Paulding, GA. April 25, 2014. Decimal degrees: 33.971818, -84.766456
“Directions:
To walk a trail loop, refer to the map, where you will see numbered stations. Follow the stations in order! The stations are identified along the trail by a wooden post with an arrow, color-blaze, and station number on it.
The blaze corresponds to the loop color and the arrow tells you which direction to go as you read the text in the guide.
RED LOOP
Ravine Overlook:
In front of you is the head of the large ravine where the heaviest Federal losses occurred. The ravine becomes deeper as it flows toward Pickett’s Mill Creek to the north. The Confederate infantry brigade of Brig. Gen. Hiram S. Granbury was in position a short distance in front of you, on the other side of the road, which is in the same place where three Federal assaults occurred, without trenches.
Station #1:
--The original Civil War road continues to your right to Pickett’s Mill; the road behind you was not present during the battle. –
( Phase I Map) Here was the end of Granbury’s line that was located just downhill from the road. The Federals charged up the hill out of the ravine through dense woods similar to what you see here and engaged Granbury’s men, in some places hand-to-hand.”
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)