View allAll Photos Tagged Paulding
The Spirit Of South Paulding, Georgia, USA.
From a collection of photographs taken at the 29th London New Year's Day Parade 2015 (LNYDP 2015). We were standing on opposite sides of the road in Piccadilly near the junction with Regent Street. The parade featured bands and participants from all over the world, along with representatives from London Boroughs whose theme was "London on the Move". See www.lnydp.com for more information.
Here is one more from the waterfall I came across last week in Paulding County. This is basically the view as you come down the path to the final approach to the fall area. I really can't wait to see this place in a few weeks when everything starts to bloom and some greenery starts making it's way in.
I stacked a 8x ND with a polarizer on this and the other shots from High Shoals Falls. shot comprised of 3 exposures blended using Photomatix 4.
Check out more about the location of this waterfall and others throughout the eastern US in our waterfall database
BLOG I I I WSM photography
© Scott Moore 2011 - All rights reserved
The structure seems to have been designed as a brooder house for incubating and raising young chicks. While brooder houses come in various shapes, they share certain key features. To keep hatchlings and young chicks warm, the building is placed in an open area with south-facing windows. It has a shed roof, which allows for larger coops without significantly increasing air space. Ventilators or flues extend from the structure to provide a proper ventilation and air exchange system.
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
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.
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)
----------------------------
See info. at:
en.wikipedia.org/wiki/Trilobite
and
Alley Cat Lanes, 120 Weast Jackson Street, Paulding, Ohio. A bowling alley in downtown Paulding, now permanently closed.
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
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
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)
----------------------------
See info. at:
en.wikipedia.org/wiki/Trilobite
and
Mediospirifer? fossil brachiopod with encrusting Aulopora corals from the Devonian of Ohio, USA. (Dave Mielke collection; temporary public display, Ohio Geological Survey, Columbus, Ohio, USA)
Auloporids are a group of extinct tabulate corals. They consist of calcareous colonies of hard substrate-encrusting, trumpet-shaped corallites. They first appear in the Ordovician and go extinct in the Permian. The auloporids seen here are encrusting a spiriferid brachiopod from Ohio's famous Silica Formation, a richly fossiliferous unit.
Click on the photo to zoom in and look around. The small, subtle, squiggly, vine-like structures near the lower right side of the fossil are a problematic fossil known as Hederella, which was also a hard-substrate encruster. Hederella was once considered to be a type of bryozoan, or "moss animal", similar to the cyclostomes Corynotrypa and Cuffeyella (those genera occur in the Ordovician-aged Cincinnatian Series of the Ohio-Indiana-Kentucky tristate area). Recent studies have indicated that Hederella is not a bryozoan at all, but is, or is closely related to, the phoronids, a group of lophophorates.
Classification of corals: Animalia, Cnidaria, Anthozoa, Tabulata, Auloporidae
Classification of brachiopod: Animalia, Brachiopoda, Articulata (also known as Rhynchonelliformea), Spiriferida, Spinocyrtiidae
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)
Merlin Entertainments Orlando Eye, International Drive, Orlando, Florida - 7th November 2014 (Photographer: Nigel G. Worrall)
During the construction site tour, James Paulding, General Manager of New Openings North America, provided insight on the expansion of Merlin Entertainments into central Florida including these must-see attractions, and updates on the LEGOLAND Florida Hotel. Also attending the event is John Stine, Director of Marketing for I-Drive 360, providing updates on the development. Explore the three new attractions coming to Orlando – The Orlando Eye, Madame Tussauds, and Sea Life Orlando Aquarium.
Thank you to our event sponsors:
UK & Trade and Investment: www.gov.uk/ukti
AFEX: www.afex.com/unitedstates
Orlando City Soccer Club: www.orlandocitysc.com
Tavistock Group: www.tavistock.com
Aston Martin: www.astonmartinorlando.com
Jaguar: www.jaguarorlando.com
Merlin Entertainments: www.merlinentertainments.biz
Madame Tussauds: www.madametussauds.com/Orlando/
Orlando Sealife Aquarium: www.visitsealife.com/orlando/
Legoland: www.florida.legoland.com
The Orlando Eye: www.officialorlandoeye.com
iDrive 360: www.i-drive360.com
Corocrinus nodosus Kier, 1952 - fossil crinoid from the Devonian of Ohio, USA. (Dave Mielke collection; temporary public display, Ohio Geological Survey, Columbus, Ohio, USA)
Crinoids (sea lilies) are sessile, benthic, filter-feeding, stalked echinoderms that are relatively common in the marine fossil record. Crinoids are also a living group, but are relatively uncommon in modern oceans. A crinoid is essentially a starfish-on-a-stick. The stick, or stem, is composed of numerous stacked columnals, like small poker chips. Stems and individual columnals are the most commonly encountered crinoid fossils in the field. Intact, fossilized crinoid heads (crowns, calices, cups) are unusual. Why? Upon death, the crinoid body starts disintegrating very rapidly. The soft tissues holding the skeletal pieces together decay and the skeleton falls apart.
Classification: Animalia, Echinodermata, Crinoidea, Periechocrinidae
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:
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
Paulding Exempted Village Schools 1 - 2006 Blue Bird Vision - Retired; Cardinal Bus Sales - Lima, Ohio. One of many Blue Birds in the fleet.
Merlin Entertainments Orlando Eye, International Drive, Orlando, Florida - 7th November 2014 (Photographer: Nigel G. Worrall)
During the construction site tour, James Paulding, General Manager of New Openings North America, provided insight on the expansion of Merlin Entertainments into central Florida including these must-see attractions, and updates on the LEGOLAND Florida Hotel. Also attending the event is John Stine, Director of Marketing for I-Drive 360, providing updates on the development. Explore the three new attractions coming to Orlando – The Orlando Eye, Madame Tussauds, and Sea Life Orlando Aquarium.
Thank you to our event sponsors:
UK & Trade and Investment: www.gov.uk/ukti
AFEX: www.afex.com/unitedstates
Orlando City Soccer Club: www.orlandocitysc.com
Tavistock Group: www.tavistock.com
Aston Martin: www.astonmartinorlando.com
Jaguar: www.jaguarorlando.com
Merlin Entertainments: www.merlinentertainments.biz
Madame Tussauds: www.madametussauds.com/Orlando/
Orlando Sealife Aquarium: www.visitsealife.com/orlando/
Legoland: www.florida.legoland.com
The Orlando Eye: www.officialorlandoeye.com
iDrive 360: www.i-drive360.com
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)
----------------------------
See info. at:
en.wikipedia.org/wiki/Trilobite
and
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)
----------------------------
See info. at:
en.wikipedia.org/wiki/Trilobite
and
Paulding Exempted Village Schools buses 6 & 28 - 2001 & 2002 Blue Bird GMCs - Retired; Cardinal Bus Sales - Lima, Ohio
Merlin Entertainments Orlando Eye, International Drive, Orlando, Florida - 7th November 2014 (Photographer: Nigel G. Worrall)
During the construction site tour, James Paulding, General Manager of New Openings North America, provided insight on the expansion of Merlin Entertainments into central Florida including these must-see attractions, and updates on the LEGOLAND Florida Hotel. Also attending the event is John Stine, Director of Marketing for I-Drive 360, providing updates on the development. Explore the three new attractions coming to Orlando – The Orlando Eye, Madame Tussauds, and Sea Life Orlando Aquarium.
Thank you to our event sponsors:
UK & Trade and Investment: www.gov.uk/ukti
AFEX: www.afex.com/unitedstates
Orlando City Soccer Club: www.orlandocitysc.com
Tavistock Group: www.tavistock.com
Aston Martin: www.astonmartinorlando.com
Jaguar: www.jaguarorlando.com
Merlin Entertainments: www.merlinentertainments.biz
Madame Tussauds: www.madametussauds.com/Orlando/
Orlando Sealife Aquarium: www.visitsealife.com/orlando/
Legoland: www.florida.legoland.com
The Orlando Eye: www.officialorlandoeye.com
iDrive 360: www.i-drive360.com
Photograph-"The Heritage of Paulding County Georgia, 1832-1999"
During the Great Depression the majority of children in small, farming families had to leave school to support their family. This is the Hiram School House where most of my family attended school. My great aunt and uncle were among the many children who had to quit going to school. My great uncle quit school when he was in second grade. He stayed home and helped his father with the cotton gin that his family ran. Having my great uncle work at the gin helped his family out greatly. During this time, the families needed all of the help that they could get in terms of having enough money to buy the essentials. Because my great uncle worked at the gin, he gave his parents one more source of income that helped them keep a roof over their heads and food on the table. My great aunt did not leave school until she was in the sixth grade. After she left school, her mother went to work. They needed my great aunt to leave school so she could take care of the household while her mother was out working. She took care of the cooking, cleaning, laundry, etc. Because most children were not able to finish school it was kind of difficult for them in the future. But despite the later difficulties these children, even at very young ages, put their families first and learned a great deal of responsibility.
Wroble, Lisa A. Kids Throughout History: Kids Durint the Great Depression. New York: PowerKids Press, 1999.
For more information visit:
Paulding Exempted Village Schools 23 - 1997 Blue Bird TC/2000 FE - Retired; Cardinal Bus Sales - Lima, Ohio
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)
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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)
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See 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
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:
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.
Located on the southeast corner of the Llano 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...
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)
-----------------------------------
See info. at:
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.
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
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
Merlin Entertainments Orlando Eye, International Drive, Orlando, Florida - 7th November 2014 (Photographer: Nigel G. Worrall)
During the construction site tour, James Paulding, General Manager of New Openings North America, provided insight on the expansion of Merlin Entertainments into central Florida including these must-see attractions, and updates on the LEGOLAND Florida Hotel. Also attending the event is John Stine, Director of Marketing for I-Drive 360, providing updates on the development. Explore the three new attractions coming to Orlando – The Orlando Eye, Madame Tussauds, and Sea Life Orlando Aquarium.
Thank you to our event sponsors:
UK & Trade and Investment: www.gov.uk/ukti
AFEX: www.afex.com/unitedstates
Orlando City Soccer Club: www.orlandocitysc.com
Tavistock Group: www.tavistock.com
Aston Martin: www.astonmartinorlando.com
Jaguar: www.jaguarorlando.com
Merlin Entertainments: www.merlinentertainments.biz
Madame Tussauds: www.madametussauds.com/Orlando/
Orlando Sealife Aquarium: www.visitsealife.com/orlando/
Legoland: www.florida.legoland.com
The Orlando Eye: www.officialorlandoeye.com
iDrive 360: www.i-drive360.com