View allAll Photos Tagged Paulding
Ships moored at Charlestown Navy Yard. In the foreground is USS Sturtevant DD-240 then USS Childs DD-241, USS Overton DD-239, USS James K Paulding DD-238 Navy Tug Iwana, USS Constitution and the Charlestown receiving ship Southery (IX-26)
Photographer Leslie Jones
Courtesy of the Boston Public Library, Leslie Jones Collection.
Paulding County, GA
2014 Ford F450/Reading
Rescue 3 serves the Mount Tabor and East Paulding Communities.
Paulding County Fire Station 3:
2450 Mt. Tabor Church RD
Dallas, GA 30157
At the site of the Battle of New Hope Church in the War Between the States, Paulding County, Georgia.
Read more: www.confederatedigest.com/2010/08/confederate-avenue-and-...
Nucleocrinus elegans Conrad, 1842 - fossil blastoids in fossiliferous calcareous shale from the Devonian of Ohio, USA.
Blastoids are an extinct group of echinoderms. They resemble crinoids in having a head, or theca, perched atop a long stem of stacked columnals composed of calcite. Crinoids and blastoids are pelmatozoans - stalked echinoderms. Both groups are sessile, benthic, filter-feeding organisms. The overall structure and morphology of crinoid heads and blastoid heads are quite different. Blastoid heads have pentaradial symmetry and somewhat resemble closed flower buds or nuts. They have 5 ambulacral grooves extending outward and downward from the summit of the theca. During life, many thin, delicate brachioles extended from the ambulacral grooves - these structures captured tiny particles of food from seawater as the blastoid engaged in filter feeding.
Classification: Animalia, Echinodermata, Blastozoa, Blastoidea, Spiraculata, Nucleocrinidae
Stratigraphy: Silica Formation, Middle Devonian
Locality: quarry near Paulding, northwestern Ohio, USA
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More info. at:
Paulding County, GA
2019 Rosenbaur Warrior
Job #42431
Squad 1 serves countywide.
Paulding County Fire Station 1:
169 Thomas B. Murphy DR
Dallas, GA 30132
New Hope Cemetery, Paulding County, Georgia
John Harrod was born December 24, 1826 in Alabama. He was the son of William L. Harrod (October 20, 1786-September 1, 1866) and Sarah Chewning (May 5, 1785-July 16, 1856). At some point his family moved to Cadaretta, Choctaw Co., MS. At the age of 35, he was elected 1st Lieutenant of Co. G, "Sons of Liberty" which later became the "Davis Guards," of the 33rd Mississippi Infantry Regiment. On August 19, 1863 he was promoted to Major of the regiment. Compiled Service Records do not indicate the exact date he was promoted to Lt. Colonel, but it was probably early January 1864. As the war for the 33rd Mississippi Infantry moved into Georgia, it was at New Hope Church, a few miles from Atlanta, that the Lt. Colonel was wounded "while gallantly leading his regiment in an attack" and later died on June 11, 1864.
According to his daughter's recollections of the war,
"He was shot through the hand and the knee, just as he raised up from behind a tree with his hand on his knee. They had discovered the Yankee scouts on the other side of the hill. Father's boys gave the blood curdling Confederate yell and the Yankees fled; and so they were able to carry Father back to camp. The little church was used as a hospital. They amputated his leg, and when it was nearly healed, gangrene set in, and he died, like thousands of others, died for lack of proper antiseptics...They made him a coffin of one of the church doors, wrapped him in his soldiers (sic) blanket, and buried him there in a nameless grave." (1)
Prior to the war, On March 6, 1851, John had married Sophia Ann Coleman Smith (May 8, 1833-June 21, 1902) in Cadaretta, Choctaw Co., MS. They had five children. After the war she and the children moved to California.
For more see my blog: www.ConfederateDigest.com
Paulding County Board of DD - 2007 Thomas Saf-T-Liner C2; Myers Equipment Corp. - Canfield, Ohio. Bus was brand new at the time of photography.
A Set of 4 battleship photos. No info on the backs. These photos came from Pennsylvania. I do not know if they are from the WW1 era or the WW2 era.
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 5500 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
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Photo gallery of fluorite:
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
Detail of ice sulpture on main drop of Bond Falls in southern Ontonagon County near Paulding, Upper Michigan. 2/27/2021
PAULDING COUNTY AIRPORT, Dallas Ga. May 9, 2013 – Georgia Army National Guardsmen grew up in their communities and now they conduct mission specific training to be ready to help their fellow citizens or those in need around the world. Today Soldiers from the 560th Battle Field Surveillance Brigade jumped out of a UH-60 Blackhawk helicopter to maintain their currency and proficiency as Airborne Soldiers who may need to parachute in to accomplish their assigned mission.
Parachutes deploy as Soldiers from Georgia’s 560th Battle Field Surveillance Brigade (BFSB) jump out of a UH-60 Blackhawk for their first jump of the day.
(Georgia Army National Guard photo by Maj. Will Cox / Released)
September 18, 2024. Engines 5 & 10, Rescue 4, and Battalion 2 of the Paulding County Fire/Rescue tackle a small structure fire in the Nebo Community.
USS Paulding with WWI camouflage sometime in 1918, photo taken in Queensland ( now Cobh ) Ireland
catalog.archives.gov/id/45513045
www.irishecho.com/2017/05/centenary-of-u-s-navy-arrival-i...
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 photograph was taken at the border line between Indiana and Ohio along United States Highway 30 between Fort Wayne, Indiana and Van Wert, Ohio in Paulding County, Ohio.
Paulding County Board of DD - 2007 Thomas Saf-T-Liner C2; Myers Equipment Corp. - Canfield, Ohio. Bus was brand new at the time of photography.
[F093917] Potter Scott Paulding has a better lighting setup for photographing Vicki's pots and dinnerware. When we were unsuccessful at lighting anything but nearly flat pieces, Paul came to the rescue with his setup.
There are two side lights (out of the photo) and a top light in the upper right corner here. The modern flourescents work great and I could, with my telephonto zoom, attempt slightly different perspectives shooting over Paul's shoulder.
More than that, I was able to see what is needed to take better pictures for Vicki and I have figured out where we could set it up and take it down in my downstairs home office. A new project to put in my personal kanban.
Antwerp is a village in Paulding County, Ohio, United States, along the Maumee River. The population was 1,740 at the 2000 census.
Antwerp is the nearest village to the Six Mile Reservoir, the site of the Reservoir War in 1887. The place is named after the Belgian city of Antwerp.
Antwerp is located in the former wetland region known until the 19th century as the Great Black Swamp. The area was avoided by the early settlers due to its thick forestation and extensive swamps and marshes. After the area had been drained, small industries developed here, and the construction of the canals along the Maumee River in the 1840s and the land reclamation project that followed helped convert the former swamplands into fertile farmlands, leading to the growth of a farming community in Antwerp.
In the late 19th century, Antwerp was the largest village in Paulding County; its economy was driven by a lucrative local logging industry. Accordingly, when the Wabash, St. Louis and Pacific Railway decided to erect a train station in the village, it was built larger than stations in most other communities in the region. After the train station closed in 1976, it was purchased by the local historical society; today, it is listed on the National Register of Historic Places as the "Antwerp Norfolk and Western Depot".
en.wikipedia.org/wiki/Antwerp%2C_Ohio
en.wikipedia.org/wiki/Wikipedia:Text_of_Creative_Commons_...
Paulding Exempted Village Schools 28 - 2002 Blue Bird GMC - Retired; Cardinal Bus Sales - Lima, Ohio
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
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Photo gallery of fluorite:
Built in 1972, this structure serves the 1st District of Jasper County. It is located in one of the state's smallest county seats.
The other Jasper County seat is Bay Springs.
Paulding is a tiny village that once had a much larger population but has seen much decline ever since the Reconstruction Era. It is today Mississippi's only unincorporated county seats.
Paulding Exempted Village Schools 1 - 2006 Blue Bird Vision - Retired; Cardinal Bus Sales - Lima, Ohio. One of many Blue Birds in the fleet.
Fluorite and calcite 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 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 occurs in the vicinity of southern Illinois (Mississippi Valley-type deposits).
Locality: Auglaize Quarry, southeast of the town of Junction, northeastern Paulding County, northwestern Ohio, USA
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Photo gallery of fluorite:
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)
Sphalerite-calcite from Ohio, USA.
Blackish = sphalerite (ZnS - zinc sulfide)
Whitish = calcite (CaCO3 - calcium carbonate)
Grayish = carbonate host rock
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 6000 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 sulfide minerals contain one or more sulfide anions (S-2). The sulfides are usually considered together with the arsenide minerals, the sulfarsenide minerals, and the telluride minerals. Many sulfides are economically significant, as they occur commonly in ores. The metals that combine with S-2 are mainly Fe, Cu, Ni, Ag, etc. Most sulfides have a metallic luster, are moderately soft, and are noticeably heavy for their size. These minerals will not form in the presence of free oxygen. Under an oxygen-rich atmosphere, sulfide minerals tend to chemically weather to various oxide and hydroxide minerals.
Sphalerite is a somewhat common zinc sulfide mineral (ZnS). It has a metallic to submetallic to resinous to adamantine luster. Many metals can substitute for the zinc, such as iron, cadmium, and manganese. Sphalerite almost always has some iron in it, so a better chemical formula would be (Zn,Fe)S. Sphalerite has a wide color range, depending principally on iron content. Pure to almost pure sphalerite is whitish to greenish. With increasing iron content, sphalerite becomes yellowish to brownish to blackish. One variety of sphalerite has a strikingly intense dark red color (ruby sphalerite). Its streak color also varies with iron content from whitish to pale yellowish to brownish. Sphalerite is also distinctive in being moderately heavy for its size and having six different planes of cleavage.
Sphalerite is the most important zinc ore mineral. Zinc produced from sphalerite is used for many purposes, including mixing with copper to produce brass, rust protection of iron & steel, and for making modern American pennies (although the cost of making each zinc penny is more than 1¢).
Locality: quarry in Paulding County, northwestern Ohio, USA
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Photo gallery of sphalerite:
Historic 1921 World War I Monument in front of the old Knoxville High School in Knox County, Tennessee. The monument contains John Paulding's cast bronze doughboy statue "Over the Top" (Model 2043-A). It was dedicated by U.S. Gen. John “Black Jack” Pershing in 1922.
The World War I Monument was listed on the National Register of Historic Places (NRHP) in 1994 as a contributing resource to the Emory Place Historic District (NRIS No. 94001259).
An 1886 building, similar in appearance to the Lenawee County Courthouse in Adrian, Michigan. Edward Fallis, a native of Toledo, designed both structures.
Paulding is, by all accounts, Ohio's most topographically featureless county, and it remained sparsely populated until the final decades of the nineteenth century. Between 1880 and 1890, its population nearly doubled, from 13,485 to 25,932.
Upper Bond Falls In Autumn
Ontonagon River
Michigan State Scenic Site
Paulding, Michigan
View it extra large here