View allAll Photos Tagged Paulding
Paulding Exempted Village Schools 1 - 2006 Blue Bird Vision - Retired; Cardinal Bus Sales - Lima, Ohio. One of many Blue Birds in the fleet.
Basidechenella lucasensis Stumm, 1965 - fossil trilobite 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:
Located at the southern corner of the Connecticut Street Armory at the intersection of Niagara and Connecticut streets, this monument was erected in 1922.
Please refer to this website for more information on the Paulding Doughboy statues located around the nation: doughboysearcher.weebly.com/e-m-viquesney-vs-john-pauldin...
Buffalo is the second largest city in New York with a metropolitan population of roughly 1.2 million (in 2020). It serves as the seat of Erie County, and is situated at the head of the Niagara River at the eastern end of Lake Erie.
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:
John Paulding Engine Company No. 1
Appearing in the 2023 HVVFA Dress Parade held in West Glens Falls, New York on June 17th.
Photo By Derek J. Ewing
Copyright 2023 - All Rights Reserved.
Located south of the Cherry County Courthouse, this monument is a contributing object to the Cherry County Courthouse, which was placed on the National Register of Historic Places in 1990.
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...
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:
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
This is the rare and beautiful Georgia aster. It can be distinguished from other purple asters by the white changing to reddish disk flowers. For more information: plants.usda.gov/java/profile?symbol=SYGE
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...
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)
----------------------------
This species is also known as Dechenella lucasensis.
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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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