View allAll Photos Tagged Paulding
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).
Paulding Theatre, 114 West Perry Street, Paulding, Ohio. This former theatre closed in the 1990s and has been vacant ever since. A neon sign atop the facade was removed for restoration soon before this picture was taken.
The Paulding County Courthouse is a historic governmental building in downtown Paulding, Ohio, United States. A Richardsonian Romanesque building erected in 1886, it is the third courthouse to serve the residents of Paulding County.
When Paulding County was established in 1820, the small community of Charloe was named the county seat. This arrangement proved to be short-lived: the older community of Paulding grew significantly while Charloe stagnated, and the county seat was eventually moved to the larger village. Once Paulding had been named the county seat, the county's second courthouse was erected on the village's central square in 1837. After approximately fifty years of service, this frame structure was demolished, and the present structure was built on the same location in 1886.
Designed by the E.O. Fallis Company and built by workers under the direction of general contractor Rudolph Ehrhart, the courthouse is a brick structure with a stone foundation and a roof of asphalt. Two-and-one-half stories tall with a central tower, the courthouse features nearly identical entrances on each of its four sides. Measuring 60 feet square, and 163 feet tall at the tip of its domed tower, the courthouse was patterned after the Lenawee County Courthouse in Michigan, which was also designed by the Fallis architects.
In 1974, the Paulding County Courthouse was listed on the National Register of Historic Places, due to its well-preserved architecture that was deemed significant statewide. It is one of four buildings in Paulding County on the Register, along with a rural round barn, a former train station in the village of Antwerp, and the Carnegie library in Paulding.
Two image panorama detailing the dramatic water force at the crest of Bond Falls. Paulding, Michigan on February 16, 2019.
Paulding County, Ohio Sheriff Department Unmarked Ford Crown Victoria at the courthouse in Paulding.
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...
This Richardsonian Romanesque-style courthouse, built in 1886, is the third courthouse built for Paulding County, Ohio. It was added to the National Register of Historic Places in 1974 (74001589). Paulding is on the Indiana line, east of Ft. Wayne, and is the third county south of the Michigan line; it is one of several counties Ruth Ann and I went to in 2012 after visiting my mother in the Toledo area. I was looking up some places I had gone to, or at least heard mentioned a lot, when growing up a few counties southwest of here.
Press "L" for larger image.
Paulding County, GA
x- Roswell, GA
2001 Sutphen SA75
1500/500/75'
Job #HS-3537
Truck 2 is currently using this loander apparatus from the local Sutphen dealer, Williams Fire Apparatus, while their E-ONE is out for repair and their new SPH100 is still being built.
Paulding County Fire Station 2:
535 SEABOARD AVE, HIRAM, GA 30141
I couldn't pass up this abandoned house when we came across it, even though the midday light was harsh. We had just spent several days in Toledo visiting my mom and I wanted to drive around some areas that were familiar to me from when I was a kid; some of the places were familiar only because I had heard my parents and others talk about them, rather than because I had visited them (we moved from NW Ohio just after I turned 13). This house was south of Paulding, Ohio, on US 127; a small part of the Blue Creek Wind Farm can be seen on the right.
Paulding County, GA
2021 Ford F-250 XL
Rescue 4 serves the southern half of the county as the ALS unit.
Paulding County Fire Station 4:
624 Harmony RD
Temple, GA 30179
Turbulent or frozen, it is COLD and beautiful ice water. Bond Falls in Paulding, Michigan, taken January 14, 2017.
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).
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
------------------------
Photo gallery of fluorite:
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
Took this last weekend at cruise the coop show and shine at paulding meadows!
© 2013 † B.H.B. † PHOTOGRAPHY All Rights Reserved No Use Allowed without Permission
North Baltimore EMS OH Unit 983
2000 Ford/McCoy Miller
Ambulance
#7136
We had just finished photographing the North Baltimore EMS units when they were dispatched to a run for a person with heat stroke (the temperature was in the upper 90's).
Phacops rana crassituberculata Stumm, 1953 - 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
Basidechenella lucasensis Stumm, 1965 - fossil trilobite and brachiopods from the Devonian of Ohio, USA. (Dave Mielke collection; temporary public display, Ohio Geological Survey, Columbus, Ohio, USA)
----------------------------
This species is also known as Dechenella lucasensis.
----------------------------
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 rare trilobite called Basidechenella lucasensis from the Middle Devonian-aged Silica Formation of northeastern Ohio. Silica Formation trilobites occur with other typical Middle Paleozoic shallow marine invertebrates: brachiopods, bryozoans, crinoids, and corals.
Classification: Animalia, Arthropoda, Trilobita, Polymerida, Proetidae
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:
Piedmont Azalea (Rhododendron canescens). Pickett's Mill State Historic Site, Paulding County, Georgia.