View allAll Photos Tagged Paulding
Rose Pink (Sabatia angularis), also called Rose Gentian. Pickett's Mill Battlefield State Historic Site, Paulding County, Georgia.
This picture emphasizes both the gentle, uninterrupted flow of water and the surrounding beauty of fall foliage, creating a serene and peaceful scene that showcases nature’s harmony.
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).
Located in Waldo Park in Salem, Oregon behind the Veteran's Affairs building, this World War I Monument was designed by John Paulding. For more information about this statue and Mr. Paulding, please see this website: doughboysearcher.weebly.com/the-doughboy-war-viquesney-vs...
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).
Seen here is vug-filling purple fluorite in Devonian carbonate rock at a quarry in northwestern Ohio. Other vug-filling minerals at this site include calcite and sphalerite.
Stratigraphy: derived from the Dundee Limestone or 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 fluorite:
Located in Memorial Park west of the McPherson County Courthouse, this equestrian statue was designed by sculptor John Paulding in 1917.
Limestones and dolostones in the Devonian of Ohio, USA.
This is an active quarry in far-northwestern Ohio. We were forbidden from closely approaching the walls. Large, loose blocks of rock were piled on the quarry floor for close examination and mineral collecting.
Many of the gray-colored rocks are from the the Dundee Limestone, a Middle Devonian unit equivalent to the upper Columbus Limestone and Delaware Limestone elsewhere in Ohio. At this site, the Dundee is principally light gray to gray-brown micrite and dismicrite. These lithologies are sometimes referred to as lithographic limestone and sublithographic limestone. Stylolites are present, as are numerous patches of coarsely-crystalline calcite.
The brownish-colored rocks are from the Lucas Dolomite of the upper Detroit River Group. The Lucas appears to consist of both dolostone and limestone. Finely-laminated, brown dolostone is a common lithology in this unit. Lack of stratigraphic control in the loose quarry blocks makes specific lithologic assessments difficult. Stylolites are also present in the Lucas.
Stratigraphy: Dundee Limestone & 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)
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.
Located in front of the Missoula County Courthouse in downtown Missoula, this World War I Monument was designed by John Paulding. For more information about this statue and Mr. Paulding, please see this website: doughboysearcher.weebly.com/john-pauldings-doughboys.html
Outgoing State Bar President Patrick T. "Pat" O'Connor presents the Best New Entry Award to Matthew Momtahan and Martin Valbuena of the Paulding County Bar Association.
The Best New Entry Award is presented to recognize the excellent efforts of those local and voluntary bar associations that have entered the Award of Merit or Law Day Award competitions for the first time in four years. (Photo credit: Sarah I. Coole)
Stylolite in limestone in the Devonian of Ohio, USA. (cross-section view)
The structure seen here is a stylolite, a pressure dissolution feature that frequently has the appearance of a hospital EKG reading. These occur in many limestones, dolostones, and some marbles, especially in or near orogenic belts. The host rock here is limestone, a biogenic sedimentary rock composed of calcite (CaCO3 - calcium carbonate). Most limestones formed in ancient, warm, shallow ocean environments.
Stratigraphy: loose piece, probably derived from the 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)
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).
Seen here is vug-filling purple fluorite in Devonian carbonate rock at a quarry in northwestern Ohio. Other vug-filling minerals at this site include calcite and sphalerite.
Stratigraphy: derived from the Dundee Limestone or 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 fluorite:
A photograph, circa 1890, apparently "distributed as a pioneer souvenir item" and reproduced from Laurence Hipp's History of Grover Hill — from the Donald Hutslar collection, used courtesy of Jean Hutslar.
The 1917 History of Maumee Valley provides a brief description:
The first white settler in [Paulding County] was Shadrach Hudson, who arrived in the year 1819. He came from Miami County and built a log house on the right bank of the Auglaize River, about half a mile east of the present Village of Junction. It was in the usual style, being constructed of square logs, was two stories in height, and had a huge fire-place in one end. . . . It commanded a splendid view both up and down the river. He had also served in the American army during the War of 1812, and was so impressed with the fertility and natural beauty of this site that he decided to make it his home.
That Hudson found the site beautiful is surprising; Paulding County, in 1819, existed at the heart of Ohio's Great Black Swamp, a region whose land settlers considered nearly worthless.
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.
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.
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.
American hero John Paulding died in 1818 at the age of 60. He was one of the three who captured British spy John André and uncovered the traitor Benedict Arnold and his plot to help West Point fall and George Washington be captured. Paulding is buried locally in the Old VanCortlandtville Cemetery off of Oregon Road and Locust Avenue in the Town of Cortlandt NY.
Last year the VanCortlandtville Historical Society and Old Cemetery Association held a commemoration of the 1780 capture by Paulding and unveiling of a new plaque containing the inscription on Paulding’s monument that has become faded and hard to read. On Sunday, September 23, 2018, they held another commemoration of the 200th Anniversary of Paulding’s death and to show the newly cleaned monument. Prior to the ceremony at the cemetery, there was an outstanding play, “Captor in Question,” performed by actors/educators Sean Grady and Gary Petagine, portraying Pauling and former Revolutionary War Intelligence Officer/Congressman Benjamin Tallmadge.
It was an honor to participate once again in honoring Paulding and helping to preserve his memory and American history.
Located in Memorial Park off of E. 3rd Street N., this statue is titled American Doughboy. It was designed by sculptor John Paulding, and it represents the WWI veterans of Rusk County, Wisconsin.
For more information about this and other WWI monuments, please refer to the following site: doughboysearcher.weebly.com/
Stylolite in limestone in the Devonian of Ohio, USA. (cross-section view)
The structure seen here is a stylolite, a pressure dissolution feature that frequently has the appearance of a hospital EKG reading. These occur in many limestones, dolostones, and some marbles, especially in or near orogenic belts. The host rock here is limestone, a biogenic sedimentary rock composed of calcite (CaCO3 - calcium carbonate). Most limestones formed in ancient, warm, shallow ocean environments.
Stratigraphy: loose piece, probably derived from the 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)
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:
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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...
Euryzone arata (Hall, 1862) - fossil snail in limestone in the Devonian of Ohio, USA
The gastropods (snails & slugs) are a group of molluscs that occupy marine, freshwater, and terrestrial environments. Most have a calcareous external shell (the snails). Some lack a shell completely, or have reduced internal shells (the slugs & sea slugs & pteropods). Most members of the Gastropoda are marine. Most marine snails are herbivores (algae grazers) or predators/carnivores.
Classification: Animalia, Mollusca, Gastropoda, Pleurotomariida, Gosseletinidae
Stratigraphy: Dundee Limestone, 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)
Horizon Wind Energy's Timber Road $1 billion wind farm in Paulding and Van Wert Counties will consist of 55 wind turbines. The wind farm will generate 99 mega watts of power, which will all be sold to American Electric Power.
This structure, typical of Ohio's fantastic courthouses, was erected in 1886-88 by contractor Rudolph Ehrhart with the designs of the architectural firm of E. O. Fallis and Company.
It was placed on the National Register of Historic Places in 1974.
Location: Paulding, Ohio
Title: Industry
Artist: Charles Umlauf
Dated: 1940
Medium: carved mahogany bas-relief
Located in front of the Leavenworth County Courthouse
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...
Stylolite in limestone in the Devonian of Ohio, USA. (cross-section view)
The structure seen here is a stylolite, a pressure dissolution feature that frequently has the appearance of a hospital EKG reading. These occur in many limestones, dolostones, and some marbles, especially in or near orogenic belts. The host rock here is limestone, a biogenic sedimentary rock composed of calcite (CaCO3 - calcium carbonate). Most limestones formed in ancient, warm, shallow ocean environments.
Stratigraphy: loose piece, probably derived from the 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)
Open Door Baptist Church - Lima, OH. Purchased used from Paul's Equipment, who bought it from Georgia.
This bland, flagging strip mall was the site of the John I. Paulding Company in New Bedford, up until 1986 or so. I worked summers at Paulding after high school, and was offered a job there when I graduated college in 1980. I turned it down.
Between the point I took this shot and the Papa Ginos, there was a small office building. I only went in there a few times, but I did help re-roof it (with spray tar) one supremely hot summer day.
Where the other stores are (across the drive) was a big sprawling factory, with a couple of machine shops, a welding shop, a huge industrial pottery, a room full of screw machines, a room for electroplating, injection molding machines for plastic, and a big assembly floor.
Part of it dated back to colonial times. A machine shop on the first floor and the engineering lab on the second floor shared a part of the facility made from fieldstones. It had a tower with rifle slots instead of windows that the company used for storage, since the need to protect the stagecoach horses while they rested en route to Boston was no longer necessary by then.
Production was moved away from the unionized factory in New Bedford, and I think ultimately the whole company failed. I don't think there is anything with the Paulding name made anywhere now on the market.
The Fieldstone Marketplace itself is looking pretty tired, now, with lots of empty stores.
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.
American hero John Paulding died in 1818 at the age of 60. He was one of the three who captured British spy John André and uncovered the traitor Benedict Arnold and his plot to help West Point fall and George Washington be captured. Paulding is buried locally in the Old VanCortlandtville Cemetery off of Oregon Road and Locust Avenue in the Town of Cortlandt NY.
Last year the VanCortlandtville Historical Society and Old Cemetery Association held a commemoration of the 1780 capture by Paulding and unveiling of a new plaque containing the inscription on Paulding’s monument that has become faded and hard to read. On Sunday, September 23, 2018, they held another commemoration of the 200th Anniversary of Paulding’s death and to show the newly cleaned monument. Prior to the ceremony at the cemetery, there was an outstanding play, “Captor in Question,” performed by actors/educators Sean Grady and Gary Petagine, portraying Pauling and former Revolutionary War Intelligence Officer/Congressman Benjamin Tallmadge.
It was an honor to participate once again in honoring Paulding and helping to preserve his memory and American history.
Lyndhurst was built in 1838, designed by A. J. Davis. It has been called home by railroad tycoon Jay Gould, New York mayor Willam Paulding, and New York merchant George Merritt. The house was donated by Gould's daughter's sister in 1961 to the National Trust for Historic Preservation, whom have lended a helping hand in the restoration of the house.
Lyndhurst is located in Tarrytown, New York, less than an hour north of Manhattan. I suggest visiting the grounds and taking a tour of the house. It's located right on the Hudson River and there is also a great view of the Tappenzee bridge.
Lynhurst.org
nthp.org
Auglaize Quarry is in far-northwestern Ohio. The quarry walls have Devonian-aged carbonates of the lower Dundee Limestone over the upper Lucas Dolomite. Collector-grade calcite, sphalerite, and fluorite occur in these rocks.
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)