View allAll Photos Tagged Paulding
Located in a small city park across the street from the Freeburg post office
For more information regarding this statue, please refer to this website: doughboysearcher.weebly.com/the-doughboy-war-viquesney-vs...
Funding for this Carnegie library was granted on July 13, 1912 in the form of $40,000. It stands at 205 South Main Street, and is claimed to be the first Carnegie library to serve an entire county. The building was placed on the National Register of Historic Places in 1984.
The building was designed by Howard & Merriam using a Beaux-Arts style.
Paulding is a small northwestern Ohio county seat, located to the east of Fort Wayne.
Very dark reddish brown = sphalerite (ZnS)
Gray = limestone
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 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.
Stratigraphy: loose block likely derived from the Lucas Dolomite, upper Detroit River Group, Devonian
Locality: Auglaize Quarry (= Shelly Company, Stoneco's Auglaize Facility), southeast of the town of Junction, northeastern Paulding County, northwestern Ohio, USA (41° 10' 27.83" North latitude, 84° 25' 19.75" West longitude)
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Photo gallery of sphalerite:
Alley Cat Lanes, 120 Weast Jackson Street, Paulding, Ohio. A bowling alley in downtown Paulding, now permanently closed.
Wording on the base:
Citizen, lawyer, statesman, historian
Born on a Paulding County farm Feb. 15, 1851
Died in Dallas Georgia, May 17, 1926
His life was largely given to the service of his people of his home county as justice of the peace, deputy sheriff, representative of his county in the state legislature for forty years. Judge of the Tallapoosa Circuit for eight years. Postmaster of Brownsville, GA. Also chairman of the board of trustees of the town of Dallas for twelve years.
Judge Bartlett was an active mason. At the grand lodge of Georgia in Oct. 1902. He was selected as one of the trustees to build the Masonic home at Macon. The Bartlett Lodge of Hiram, GA was names for him. He was made a Mason in 1874 at Douglasville, GA and created a noble of the Mystic Shrine in 1897, being a member of Yaarab Temple Atlanta, GA
Whitish gray = calcite (CaCO3)
Brown = dolostone
Lustrous blackish-yellowish-reddish masses at center = sphalerite (ZnS)
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 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.
Stratigraphy: loose block likely derived from the Lucas Dolomite, upper Detroit River Group, Devonian
Locality: Auglaize Quarry (= Shelly Company, Stoneco's Auglaize Facility), southeast of the town of Junction, northeastern Paulding County, northwestern Ohio, USA (41° 10' 27.83" North latitude, 84° 25' 19.75" West longitude)
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Photo gallery of sphalerite:
Common Bluets, also called Quaker Ladies (Houstonia caerulea). Pickett's Mill State Historic Site, Paulding County, Georgia.
Petroleum in a Hexagonaria fossil coral in the Devonian of Ohio, USA.
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 Hexagonaria, a colonial rugose coral having many hexagonally-shaped corallites, as seen in plan view - this is a cross-section view.
The black areas are petroleum. Hydrocarbons have migrated into fractures and other porous areas of the coral. This specimen is in a quarry in 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, Rugosa, Phillipsastraeidae
Stratigraphy: Dundee Limestone, 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:
and
Paulding Exempted Village Schools 1 - 2006 Blue Bird Vision - Retired; Cardinal Bus Sales - Lima, Ohio. One of many Blue Birds in the fleet.
Petroleum in a Favosites fossil coral from the Devonian of Ohio, USA. (~8.0 centimeters across at its widest)
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
Open Door Baptist Church - Lima, OH. Purchased used from Paul's Equipment, who bought it from Georgia.
Paulding County, GA
Not a lot of water flow today...
For many years, the pool below the falls was used as a baptizing hole by the nearby High Shoals Baptist Church.
Fossiliferous chert nodule in carbonate in the Devonian of Ohio, USA.
The brownish mass in the photo is a chert nodule representing partially silicified carbonate rock. This is an out-of-place quarry block of either limestone or dolostone. Within the chert nodule are two silicified solitary rugose corals ("horn corals").
Classification: Animalia, Cnidaria, Anthozoa, Rugosa
Stratigraphy: loose quarry block of Dundee Limestone or Lucas Dolomite, Middle Devonian
Locality: Auglaize Quarry (= Shelly Company, Stoneco's Auglaize Facility), southeast of the town of Junction, northeastern Paulding County, northwestern Ohio, USA (41° 10' 27.83" North latitude, 84° 25' 19.75" West longitude)
On Saturday, September 23, 2017 the Old Van Cortlandtville Cemetery Association held a Plaque Dedication to unveil a new marker for the John Paulding gravesite. I was honored to be a part of the ceremony and also to secure the funds needed to create the plaque. Knowing of my interest and involvement in promoting history and being a Revolutionary War Reenactor for over 40 years, members of the association approached me hoping I would help in the creation of the plaque. I was glad to have the opportunity to have a hand in the initiative to create the plaque and was able to obtain the funding required to have the plaque created and installed.
The act of John Paulding and his comrades Isaac Van Wart and David Williams capturing British spy Major John Andre was a turning point in our nation’s history. In recent years, the story has a renewed interest due the background setting of West Point, George Washington, Benedict Arnold and especially the new details regarding the spy ring involved in the war. A number of books and even a television series has appeared in just the last few years giving renewed interest in the story.
John Paulding, the lead figure in the capture of Andre, is buried in the Old Van Cortlandt Cemetery just yards from the historic Revolutionary War Era Old St. Peter’s Church. He died in 1818 at the age of 60 and was honored with a prominent site and stone/obelisk structure. Over time, the words engraved into the marble monument have faded and it is just a matter of time until they are lost forever. The new plague that was installed replicates the engraved words exactly so as to preserve them for generations to come.
Petroleum in a Hexagonaria fossil coral from the Devonian of Ohio, USA. (Dave Mielke collection; temporary public display, Ohio Geological Survey, Columbus, Ohio, USA)
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 Hexagonaria, a colonial rugose coral having many hexagonally-shaped corallites, as seen in plan view (click on the photo to zoom in - the corallite shapes are a tad difficult to discern here).
The black areas are petroleum. Hydrocarbons have migrated into fractures and other porous areas of the coral. The black spots are corallite centers. 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, Rugosa, Phillipsastraeidae
Stratigraphy: Dundee Limestone, 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:
and
The goat barn contained exclusively boer goats. I mean, I like them and all, but where were the pygmy goats?
Stylolite from the Devonian of Ohio, USA. (cross-section view)
This dark crust at top is a stylolite, a pressure dissolution feature that frequently has the appearance of a hospital EKG reading in cross-section view (see elsewhere in this photo album). These occur in carbonate rocks (limestones, dolostones, marbles), especially in or near orogenic belts.
Stratigraphy: attributed to the Lucas Formation, Middle Devonian
Locality: undisclosed site in Paulding County (likely a quarry), northwestern Ohio, USA
United Methodist Women, Twin Oaks United Methodist Church, Oakwood (Paulding County) Ohio, opening umbrellas to intercept human traffickers.
Submitted by Helen Maddock, Social Action Coordinator
#UMWumbrellas
Petroleum in a favositid fossil coral in the Devonian of Ohio, USA.
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 a favositid, or "honeycomb coral", an extinct group of tabulate corals.
The black areas are petroleum. Hydrocarbons have migrated into fractures and other porous areas of the coral. This specimen is in a quarry in 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: Dundee Limestone, 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/Favosites
and
Located in Olathe Cemetery at Northgate and Harold, this statue is titled American Doughboy. It was designed by sculptor John Paulding, and it represents the WWI veterans of Johnson County, Kansas.
The Olathe Cemetery was established in 1865, and was placed on the National Register of Historic Places in 2017.
Petroleum in a Favosites fossil coral from the Devonian of Ohio, USA. (field of view: ~6.0 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
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 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.
Pyrite is a common iron sulfide mineral (FeS2). It’s nickname is “fool's gold”. Pyrite has a metallic luster, brassy gold color (in contrast to the deep rich yellow gold color of true gold - www.flickr.com/photos/jsjgeology/sets/72157651325153769/), dark gray to black streak, is hard (H=6 to 6.5), has no cleavage, and is moderately heavy for its size. It often forms cubic crystals or pyritohedrons (crystals having pentagonal faces).
Pyrite is common in many hydrothermal veins, shales, coals, various metamorphic rocks, and massive sulfide deposits.
Seen here is finely-crystalline pyrite coating a fracture in Devonian carbonate rock.
Stratigraphy: derived from the Dundee Limestone or the Lucas Dolomite, Devonian
Locality: Auglaize Quarry (= Shelly Company, Stoneco's Auglaize Facility), southeast of the town of Junction, northeastern Paulding County, northwestern Ohio, USA (41° 10' 27.83" North latitude, 84° 25' 19.75" West longitude)
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Photo gallery of pyrite:
Sign on the side of the Masonic Temple, corner of South Main Street and East Perry Street, Paulding, Ohio. It's not clear if this building is still in use, but it certainly looks in fine shape.
Located in a small triangular park near the base of the Columbia River bridge (U.S. 101) in Astoria, Oregon
Please refer to this website for more information regarding this statue: doughboysearcher.weebly.com/the-doughboy-war-viquesney-vs...