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Not certain of the age of this fossil and no idea where it came from. Barb found it and gave it to me as a gift many years ago.
Taken 6th January 2012
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more photos to come bit by bit. swamped with freelance projects ;)
they have a lot of African animals there...
Eurypterus remipes DeKay, 1825 - fossil sea scorpion in dolostone from the Silurian of New York State, USA.
The eurypterids, or sea scorpions, are an extinct group of chelicerate arthropods. They have an elongated, scorpion-like body that could reach enormous sizes (2.5 to 3 meters!), with a nonmineralizing exoskeleton composed of chitinous material. They are generally found in shallow to very shallow water marine and marginal marine facies.
Shown here is Eurypterus remipes, a classic example of this bizarre group of creatures. It, and other eurypterid species, is well represented in the famous Bertie Dolomite of New York State. The host rock is fine-grained dolostone (dolomudstone).
Classification: Animalia, Arthropoda, Chelicerata, Merostomata, Xiphosura, Eurypterida, Eurypteridae
Stratigraphy: Phelps Member, Fiddlers Green Formation, Bertie Dolomite Group, Upper Silurian
Locality: unrecorded/undisclosed site in Herkimer County, New York State, USA (but probably from the Allan Lang Quarry in southern Herkimer County)
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See info. at:
Fossil / South Carolina, USA / Copyright ©2007 by William Tanneberger - All Rights Reserved.
Fossilized Bone
South Carolina (Cooper River)
Trilobites ("three-lobes") are extinct arthropods that form the class Trilobita. They appeared in the Early Cambrian period and flourished throughout the lower Paleozoic era before beginning a drawn-out decline to extinction when, during the Late Devonian extinction, all trilobite orders, with the sole exception of Proetida, died out. The last of the trilobites disappeared in the mass extinction at the end of the Permian about 250 million years ago (m.y.a.).
Trilobites are very well-known, and possibly the second-most famous fossil group, after the dinosaurs. When trilobites appear in the fossil record of the Lower Cambrian they were already highly diverse and geographically dispersed. Because of their diversity and an easily fossilized exoskeleton, they left an extensive fossil record with some 17,000 known species spanning Paleozoic time.
More here: en.wikipedia.org/wiki/Trilobite
We found this in Big Brook, a stream in New Jersey that is noted for its Cretaceous fossils. A fellow fossil enthusiast with extensive knowledge of ammonites identified this for me.
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Deteriorated glass frame on fossil fern display, cedar ridge exhibit on s kaibab trail. 01aug 1968. Nps.
1 fossil-fish drawing (13 x 21 cm.)
Repository: Ernst Mayr Library, Museum of Comparative Zoology, Harvard University
Call number: bfAg 168.60.7s
Fossil ferns just photographed .
They are so fragile that they can rub off the stone leaving a feint impression
This is orlas find and though there are so many traces that look alike...I actually think they look like the one in my find og what i think could be a trace fossil from perhaps a kind of tubeworm....
I have a link to one I think it looks like found by Henrik Madsen from the moclay museum in Mors here in Denmark...here is a link:
www.vestjyskstenklub.dk/nye%20fund/2009fund/Nyt%20fra%20M...
Fossil Public School
Fossil, Oregon
Listed 5/22/2013
Reference Number: 13000312
he Fossil Public School is locally significant, and is eligible for the National Register of Historic Places under Criterion A for the significant role the school played in the educational development of the rural community since its construction in 1924. The Fossil Public School was also known as Wheeler County Public School throughout much of its history, as it housed both the grade school and high school. The school is located in downtown Fossil at 404 Main Street, near the intersection of First and Jay streets. The two-story Classical Revival-style school building is locally significant and eligible for the National Register of Historic Places under Criterion A for the important role it played in the educational development of this rural community since its construction. The Period of Significance of the Fossil Public School spans from its original construction date of 1924, based on the design by DeYoung and Roald Architects from Portland, Oregon, to 1949 when the Fossil High School was built and ninth through twelfth grades were transferred to the new location, which to a degree altered the way that the building was used. The gymnasium associated with the school is a contributing resource to the site, completed with aid from the Works Progress Administration in 1936, within the Period of Significance for the school. Both the school building and gymnasium retain a high degree of integrity through original design, workmanship, and material features with no alterations to the original location or function.
Fossil tree, species Sigillaria, from the Carboniferous period. About 320 million years old. Found in a quarry near Stanhope, County Durham, in 1913 and brought to Stanhope churchyard.
From the toxic waste created by the extreme extraction of tar sands destroying indigenous communities in Canada, to toxins created by the BP Whiting refinery producing sacrifice communities in the Greater Chicago area, to the resultant catastrophic effect on our climate, the urgent need for a just transition away from fossil fuels to a 100% renewable energy economy is abundantly clear.
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These fossils are at a creek near Pelion Hut. There was an amazing variety, it was fun to see the diversity and complexity.
Day 3 of Overland Track
Australia oz2009 236
Glyptodon clavipes fossil. Sand Dune Coast near Quequen. Two men (one Elmer Riggs). 1926.
Name of Expedition: 2nd Captain Marshall Field Paleontological Expedition
Participants: Elmer S. Riggs (Leader and Photographer),Robert C. Thorne (Collector), Rudolf Stahlecker (Collector), Felipe Mendez
Expedition Start Date: April 1926
Expedition End Date: November 1926
Purpose or Aims: Geology Fossil Collecting
Location: South America, Argentina, Buenos Aires, Quequen
Original material: 5x7 inch glass negative
Digital Identifier: CSGEO69502
Wall of small fossils, mostly leaves, at Utah Field House of Natural History State Park Museum in Vernal, UT
Cedar ridge fossil fern exhibit with early interpretive signage. S kaibab trial. Circa 1940's ? Nps photo.
These fossils are at a creek near Pelion Hut. There was an amazing variety, it was fun to see the diversity and complexity.
Day 3 of Overland Track
Australia oz2009 237