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Beaux-Arts Semi-detached Houses (1949)
2012–14 Paulding Ave.
Morris Park, Bronx
© Matthew X. Kiernan
NYBAI15-7501
Fluorite from Ohio, USA. (public display, Geology Department, Wittenberg University, Springfield, Ohio, USA)
A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are about 5400 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.
The halides are the "salt minerals", and have one or more of the following anions: Cl-, F-, I-, Br-.
Fluorite is a calcium fluoride mineral (CaF2). The most diagnostic physical property of fluorite is its hardness (H≡4). Fluorite typically forms cubic crystals and, when broken, displays four cleavage planes (also quite diagnostic). When broken under controlled conditions, the broken pieces of fluorite form double pyramids. Fluorite is a good example of a mineral that can be any color. Common fluorite colors include clear, purple, blue, green, yellow, orange, and brown. The stereotypical color for fluorite is purple. Purple is the color fluorite "should be". A mineral collector doesn't have fluorite unless it's a purple fluorite (!).
Fluorite occurs in association with some active volcanoes. HF emitted from volcanoes can react with Ca-bearing rocks to form fluorite crystals. Many hydrothermal veins contain fluorite. Much fluorite also occurs in the southern Illinois area (Mississippi Valley-type deposits).
Geologic context: vug-filling fluorite crystals in carbonate rock of the Detroit River Group or Dundee Limestone (Lower to Middle Devonian)
Locality: Stoneco Incorporated's Auglaize Quarry, southwest of the town of Junction, northeastern Paulding County, northwestern Ohio, USA
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Photo gallery of fluorite:
A hand edited photo for publication of the USS Fanning DD-37 a Paulding class Destroyer and to the right is the Destroyer USS Sigourney DD-81 a Wickes (Little) class destroyer
during WWI
Paulding County, GA
2023 Freightliner M2-106/Rosenbaur
750gal/1250gpm
Job #1875723
Engine 1 serves the city of Dallas.
Paulding County Fire Station 1:
169 Thomas B. Murphy DR
Dallas, GA 30132
I had a dealer trade run last week and ran across Uncle Sam beckoning me to come in and buy fireworks. I had to pass him by.
Paulding County, GA
2024 Freightliner M2-106/Spencer
750gal/7.5F/1500gpm
Job #17021224
Engine 2 serves the city of Hiram.
Paulding County Fire Station 2:
535 SEABOARD AVE, HIRAM, GA 30141
Army JROTC Cadets from North Paulding High School plunge into an obstacle during the cross-country rescue course, one of the five challenges Cadet Raider Teams had to compete in November 5 at the 2022 Army JROTC National Raider Championships. This outdoor competition featured all-service and Army JROTC Cadet teams from around the country competing in physically and mentally challenging team events November 3-6 at the Gerald Lawhorn Boy Scout Camp in Molena, Ga. (Photo by Sarah Windmueller, U.S. Army Cadet Command Public Affairs)
Army JROTC Cadets from North Paulding High School plunge into an obstacle during the cross-country rescue course, one of the five challenges Cadet Raider Teams had to compete in November 5 at the 2022 Army JROTC National Raider Championships. This outdoor competition featured all-service and Army JROTC Cadet teams from around the country competing in physically and mentally challenging team events November 3-6 at the Gerald Lawhorn Boy Scout Camp in Molena, Ga. (Photo by Sarah Windmueller, U.S. Army Cadet Command Public Affairs)
This is Township Road 152, just east of State Route 49, in rural Paulding County, Ohio. The muddy dirt road has to be the worst road that I have ever seen in the midwestern United States! The sign says "Road Closed When Wet," and you can see why!
I photographed it on a rainy, foggy winter morning. This is the first of two photographs that I made of this scene.
2-25-20
Cadets from the South Paulding High School Army JROTC Raider Team race downhill during the 5K event November 4 at the Gerald Lawhorn Boy Scout Camp in Molena, Ga. This outdoor competition featured Army JROTC Cadet teams from around the country competing in a series of five physically challenging events as part of the 2022 Army JROTC National Raider Championships that took place November 3-6, 2022. (Photo by Sarah Windmueller, U.S. Army Cadet Command Public Affairs)
Phacops rana crassituberculata Stumm, 1953 - fossil trilobites from the Devonian of Ohio, USA. (Dave Mielke collection; temporary public display, Ohio Geological Survey, Columbus, Ohio, USA)
This fossil is also known as Eldredgeops rana crassituberculata.
Trilobites are extinct marine arthropods. They first appear in Lower Cambrian rocks and the entire group went extinct at the end of the Permian. Trilobites had a calcitic exoskeleton and nonmineralizing parts underneath (legs, gills, gut, etc.). The calcite skeleton is most commonly preserved in the fossil record, although soft-part preservation is known in some trilobites (Ex: Burgess Shale and Hunsruck Slate). Trilobites had a head (cephalon), a body of many segments (thorax), and a tail (pygidium). Molts and carcasses usually fell apart quickly - most trilobite fossils are isolated parts of the head (cranidium and free cheeks), individual thoracic segments, or isolated pygidia. The name "trilobite" was introduced in 1771 by Johann Ernst Immanuel Walch and refers to the tripartite division of the trilobite body - it has a central axial lobe that runs longitudinally from the head to the tail, plus two side lobes (pleural lobes).
Seen here are famous trilobites whose remains are relatively common in the Middle Devonian-aged Silica Formation of northeastern Ohio. These are Phacops rana crassituberculata (also known as Eldredgeops, an unnecessary genus name based on taxonomic oversplitting). Phacops trilobite fossils occur with other typical Middle Paleozoic shallow marine invertebrates: brachiopods, bryozoans, crinoids, and corals.
Classification: Animalia, Arthropoda, Trilobita, Polymerida, Phacopidae
Stratigraphy: Silica Formation (also known as the Silica Shale), Givetian Stage, upper Middle Devonian
Locality: quarry northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 52.55" North latitude, 84° 37' 19.32" West longitude)
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See info. at:
en.wikipedia.org/wiki/Trilobite
and
Phacops rana crassituberculata Stumm, 1953 - enrolled fossil trilobite from the Devonian of Ohio, USA. (Dave Mielke collection; temporary public display, Ohio Geological Survey, Columbus, Ohio, USA)
This fossil is also known as Eldredgeops rana crassituberculata.
Trilobites are extinct marine arthropods. They first appear in Lower Cambrian rocks and the entire group went extinct at the end of the Permian. Trilobites had a calcitic exoskeleton and nonmineralizing parts underneath (legs, gills, gut, etc.). The calcite skeleton is most commonly preserved in the fossil record, although soft-part preservation is known in some trilobites (Ex: Burgess Shale and Hunsruck Slate). Trilobites had a head (cephalon), a body of many segments (thorax), and a tail (pygidium). Molts and carcasses usually fell apart quickly - most trilobite fossils are isolated parts of the head (cranidium and free cheeks), individual thoracic segments, or isolated pygidia. The name "trilobite" was introduced in 1771 by Johann Ernst Immanuel Walch and refers to the tripartite division of the trilobite body - it has a central axial lobe that runs longitudinally from the head to the tail, plus two side lobes (pleural lobes).
Seen here is a famous trilobite whose remains are relatively common in the Middle Devonian-aged Silica Formation of northeastern Ohio. This is Phacops rana crassituberculata (also known as Eldredgeops, an unnecessary genus name based on taxonomic oversplitting). Phacops trilobite fossils occur with other typical Middle Paleozoic shallow marine invertebrates: brachiopods, bryozoans, crinoids, and corals.
Classification: Animalia, Arthropoda, Trilobita, Polymerida, Phacopidae
Stratigraphy: Silica Formation (also known as the Silica Shale), Givetian Stage, upper Middle Devonian
Locality: quarry northwest of the town of Paulding, northern Paulding County, northwestern Ohio, USA (41° 10' 52.55" North latitude, 84° 37' 19.32" West longitude)
----------------------------
See info. at:
en.wikipedia.org/wiki/Trilobite
and
This lovely edifice was erected in 1892 using the designs of architects Bruce and Morgan. It stands on the center square in downtown Dallas, Georgia, and was placed on the National Register of Historic Places in 1980.
The Fannin-Cooper Farm in Paulding County was honored as a 2013 Georgia Centennial Farm because it was farmed by multiple families for more than 100 years and because it is listed in the National Register of Historic Places. The farm has been operated continuously since 1858 by the Fannin and Cooper families and is owned by Anthony A. Cooper, Jr. The Fannins raised corn and cotton, as well as cattle and hogs. The 84-acre farmstead includes two houses, outbuildings, and farmland. Today the main crops are hay, timber and cattle.
Photo by Charlie Miller
This lovely edifice was erected in 1892 using the designs of architects Bruce and Morgan. It stands on the center square in downtown Dallas, Georgia, and was placed on the National Register of Historic Places in 1980.
Fluorite from Ohio, USA.
A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are over 6100 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.
The halides are the "salt minerals", and have one or more of the following anions: Cl-, F-, I-, Br-.
Fluorite is a calcium fluoride mineral (CaF2). The most diagnostic physical property of fluorite is its hardness (H≡4). Fluorite typically forms cubic crystals and, when broken, displays four cleavage planes (also quite diagnostic). When broken under controlled conditions, the broken pieces of fluorite form double pyramids. Fluorite is a good example of a mineral that can be any color. Common fluorite colors include clear, purple, blue, green, yellow, orange, and brown. The stereotypical color for fluorite is purple. Purple is the color fluorite "should be". A mineral collector doesn't have fluorite unless it's a purple fluorite (!).
Fluorite occurs in association with some active volcanoes. HF emitted from volcanoes can react with Ca-bearing rocks to form fluorite crystals. Many hydrothermal veins contain fluorite. Much fluorite also occurs in the southern Illinois area (Mississippi Valley-type deposits).
Geologic context: vug-filling fluorite crystals in carbonate rock of the Detroit River Group or Dundee Limestone (Lower to Middle Devonian)
Locality: Stoneco Incorporated's Auglaize Quarry, southwest of the town of Junction, northeastern Paulding County, northwestern Ohio, USA
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Photo gallery of fluorite:
Gentle, uninterrupted flow of water and the surrounding beauty of fall foliage.
Bond Falls is a waterfall on the middle branch of the Ontonagon River, a few miles east of Paulding in Haight Township in southern Ontonagon County, Michigan. The total drop of the falls is about 50 feet (15 m).
Army JROTC Cadets from North Paulding High School race through the cross-country rescue course, one of the five challenges Cadet Raider Teams had to compete in November 5 at the 2022 Army JROTC National Raider Championships. This outdoor competition featured all-service and Army JROTC Cadet teams from around the country competing in physically and mentally challenging team events November 3-6 at the Gerald Lawhorn Boy Scout Camp in Molena, Ga. (Photo by Sarah Windmueller, U.S. Army Cadet Command Public Affairs)
Paulding County, GA
2016 E-ONE Cyclone II
300gal/2400gpm/100'
Job #140305
Truck 2 serves the cities of Hiram and Dallas.
Paulding County Fire Station 2:
535 Seaboard AVE
Hiram, GA 30141
Rock gypsum from the Devonian of Ohio, USA.
Sedimentary rocks form by the solidification of loose sediments. Loose sediments become hard rocks by the processes of deposition, burial, compaction, dewatering, and cementation.
There are three categories of sedimentary rocks:
1) Siliciclastic sedimentary rocks form by the solidification of sediments produced by weathering & erosion of any previously existing rocks.
2) Biogenic sedimentary rocks form by the solidification of sediments that were once-living organisms (plants, animals, micro-organisms).
3) Chemical sedimentary rocks form by the solidification of sediments formed by inorganic chemical reactions. Most sedimentary rocks have a clastic texture, but some are crystalline.
Rock gypsum (also known as gyprock) is a chemical sedimentary rock. It is an example of an evaporite - it forms by the evaporation of water (usually seawater) and the precipitation of dissolved minerals. Rock salt & rock gypsum often occur together in evaporitic successions. Rock gypsum is composed of the mineral gypsum (CaSO4·2H2O - hydrous calcium sulfate). Heating of gypsum or rock gypsum drives off the water, leaving only calcium sulfate behind (the mineral anhydrite). Adding water to anhydrite results in the formation of gypsum again.
Rock gypsum, unlike rock salt, does not have a salty taste, and is softer (H = 2) - it can be scratched with a fingernail. Rock gypsum’s color is often a mottled whitish-light grayish-light brownish. It is usually microcrystalline and powdery looking (it’s much finer-grained than typical rock salt deposits). Rock gypsum superficially resembles chalk. Chalk is calcitic, and so will bubble in acid - rock gypsum does not bubble in acid. Rock gypsum samples vary from extremely friable to moderately solid.
Stratigraphy: attributed to the Lucas Formation, Middle Devonian
Locality: undisclosed site in Paulding County (likely a quarry), northwestern Ohio, USA
Photograph-"The Heritage of Paulding County Georgia, 1892-1999"
The Great Depression also brought about a larger interest in sports. Although most people could not afford to attend regular games, they were able to go and watch the local high school teams in their town. Also, many families would gather around a radio and enjoy the game together. Sports were an outlet for many people. It relieved their stress and gave the listeners something to do to get their minds off of the problems surrounding the Great Depression. For the players it did the same thing. For the few hours that people were playing sports, whether it be in the big leagues or in their back yard, they would almost forget about what they were going through. It allowed them to be carefree and just have fun playing the game. When children were not out working, they would be with the rest of the neighborhood kids out playing a game. Often times, it was a relief for parents to see their kids having fun. They wanted to put the least amount of the burden on the children as they possibly could. Sports became the great American pastime. It was a way for people to come together and get away from the reality of the Great Depression.
Loudermilk, Dale. The Heritage of Paulding County, Georgia, 1832-1999. Missouri: Walsworth Publishing, 1999.
For more information visit:
1911 Photo of USS Sterett DD-27, a Paulding class destroyer
This lovely edifice was erected in 1892 using the designs of architects Bruce and Morgan. It stands on the center square in downtown Dallas, Georgia, and was placed on the National Register of Historic Places in 1980.
A Cadet from North Paulding High School in Dallas, Georgia, comes up for air after low crawling through an obstacle on the Cross-Country Rescue Course during the JROTC's National Raider Championships held at the Gerald Lawhorn Boy Scout Camp in Molena, Georgia, Nov. 4-5. (Photo by Michael Maddox, Cadet Command Public Affairs)
Located in front of the Craighead County Courthouse in Jonesboro, this monument was designed by sculptor John Paulding.
Please refer to this website for more information on the Paulding Doughboy statues located around the nation: doughboysearcher.weebly.com/the-doughboy-war-viquesney-vs...
Paulding Exempted Village Schools 23 - 1997 Blue Bird TC/2000 FE - Retired; Cardinal Bus Sales - Lima, Ohio
Paulding County, GA
2023 Freightliner M2-106/Rosenbaur
750gal/1250gpm
Engine 3 serves the Mt. Tabor & East Paulding COmmunities.
Paulding County Fire Station 3:
2450 Mt. Tabor Church RD
Dallas, GA 30157
Fluorite from Ohio, USA. (Joseph Vasichko collection)
A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are about 5400 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.
The halides are the "salt minerals", and have one or more of the following anions: Cl-, F-, I-, Br-.
Fluorite is a calcium fluoride mineral (CaF2). The most diagnostic physical property of fluorite is its hardness (H≡4). Fluorite typically forms cubic crystals and, when broken, displays four cleavage planes (also quite diagnostic). When broken under controlled conditions, the broken pieces of fluorite form double pyramids. Fluorite is a good example of a mineral that can be any color. Common fluorite colors include clear, purple, blue, green, yellow, orange, and brown. The stereotypical color for fluorite is purple. Purple is the color fluorite "should be". A mineral collector doesn't have fluorite unless it's a purple fluorite (!).
Fluorite occurs in association with some active volcanoes. HF emitted from volcanoes can react with Ca-bearing rocks to form fluorite crystals. Many hydrothermal veins contain fluorite. Much fluorite also occurs in the southern Illinois area (Mississippi Valley-type deposits).
Geologic context: vug-filling fluorite crystals in carbonate rock (found in September 2016) of the Detroit River Group or Dundee Limestone (Lower to Middle Devonian)
Locality: Stoneco Incorporated's Auglaize Quarry, southwest of the town of Junction, northeastern Paulding County, northwestern Ohio, USA
------------------------
Photo gallery of fluorite:
Petroleum in a Favosites fossil coral from the Devonian of Ohio, USA. (field of view: ~6.3 centimeters across)
Corals are essentially sea anemones (polyps) that make a skeleton, which is usually mineralized. Most corals are colonial, but some are solitary. This particular fossil is Favosites, a colonial coral having corallites arranged in a honeycomb-like fashion.
The dark areas are petroleum - hydrocarbons have migrated into porous areas of the fossil. This specimen is from northwestern Ohio, which had a significant petroleum system that was heavily exploited in the late 1800s. Ohio used to be the # 1 petroleum exporter in the world!
Classification: Animalia, Cnidaria, Anthozoa, Tabulata, Favositidae
Stratigraphy: upper Dundee Limestone, Middle Devonian
Locality: Auglaize Quarry (a.k.a. Stoneco Auglaize Quarry; Maumee Stone Company's Auglaize Quarry), eastern side of the Auglaize River, along River Road, southeast of the town of Junction, Auglaize Township, northeastern Paulding County, northwestern Ohio, USA
PaulD Gaskell kindly gave this photo for publication.
A Northern Electric Class 319 heads north (right to left) over the stream at Gerards Bridge Junction. The junction itself is under the train's first or second carriage, we can see the end of its fourth carriage.
Paul's parents, never mind his grandparents, would no more recognise this sylvan setting than the dark side of the moon.
As recently as the late 1960s this would have been a barren industrial wasteland.
Copyright Paul D Gaskell 2015.
Paulding Exempted Village Schools 28 - 2002 Blue Bird GMC - Retired; Cardinal Bus Sales - Lima, Ohio
Photograph-"The Heritage of Paulding County Georgia, 1832-1999"
In the larger, urban communities during the Great Depression, the crime rate skyrocketed with the presence of gangsters and mobs. In rural communities, however, the crimes were committed on a much smaller scale. A huge problem for farmers and crop growers was stealing. People would go out in the middle of the night and go in the fields and steal the farmer’s crops. They would steal such things as watermelons, corn, wheat, etc. Illegal fishing was a small but prominent crime committed during the Great Depression as well. People would not have the money to make or buy proper fishing reels so they would illegally fish with their hands. This was not means for jail time like stealing was, but it did require a fine. Most people would end up going to jail because they could not pay their fine. Also during the Great Depression the laws of prohibition played a huge role in crime. And this not only affected the larger and urban areas, it affected rural communities as well. On rare occasion, someone from a small town would get caught trying to smuggle alcohol from a larger town. Because of the economic depression, people felt as if they would have no way to survive in certain areas without committing a crime to get what they wanted.
Bloch, Herbert A. 1949. Economic Depression as a Factor in Rural Crime: Journal of Criminal Law and Criminology, Vol. 40, No. 4. 458-470. (JSTOR)
For more information visit:
This structure, located behind the small trailer unit post office in Paulding, was erected around the turn of the 19th century by the Pauly Jail Company of Missouri. It was listed on the National Register of Historic Places in the 1990s and had deteriorated greatly since that time.
Paulding is one of two county seats for Jasper County.
The statue of one of the militiamen who apprehended John Andre atop the Captors Monument in Patriots Park.
Paulding, Mississippi
Constructed between 1895-1900 by the Pauly Jail Building and Manufcturing Co. of St Louis. It was a one story, 2 room jail with 16 inch thick walls. At the time of it's listing on the NRHP (1994), the roof was already pretty much gone but the walls were still standing.
Cadets from North Paulding High School work together to finsih the last obstacle on the Cross Country Rescue course during the JROTC Raider Nationals All-Army competition at the Gerald Lawhorn Boy Scout Camp in Molena, Georgia, Nov. 6. Cadets from across the country competed in the All-Army competition. (Photo by Michael Maddox, U.S. Army Cadet Command Public Affairs)