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Showing results for tags 'Wyoming'.
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I was able to dig in the Lance Formation last summer and finally got the chance to look at this find more closely. I don't think this is a dinosaur fossil and I'm not familiar with the skeletal anatomy of the other vertebrates at the site. Anyone know what it is? I tried taking all the relevant angles. This one came from Niobrara County in Wyoming if that helps.
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Hi there everyone, I just wanted to get some opinions on something. This is supposedly a sauropod transverse process. Can anyone confirm or reject that claim, or just give me your thoughts? It just says “a Jurassic site in Wyoming”, so that could narrow down the potential family/species. I’m sure you can tell it’s apparently the top and bottom of the same bone, just broken and missing a bit in between. Thanks for any and all help!
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How about these? They're also from Weston co Wyoming (granted I bought these two, whereas I dug the previous-posted tooth and non-eggshell). Since we don't have anything from Lance to compare to, I suppose I'm really asking: (1) is it egg shell? (2) is it dino? (3) have you seen anything like it from JRf or HCf?
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Hello, I am making a great of in-situ pictures of my fossil hunting trips for this year. We now have a foot of snow in the ground so fossil hunting season is over. ☹️ These pictures occur in Wyoming, Montana, South Dakota and North Dakota. Mostly Cretaceous aged sites but some Eocene from ND. They are mostly tooth related. I hope everyone likes in-situ pics as much as I do!
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Grad student finds a new saber-toothed species, in a museum
Oxytropidoceras posted a topic in Fossil News
Grad student finds a new saber-toothed species, in a museum, University of Oregon, Department of Earth sciences Abstract The open access paper is: Barrett, P.Z., 2021. The largest hoplophonine and a complex new hypothesis of nimravid evolution. Scientific reports, 11(1), pp.1-9. Yours, Paul H.-
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Can radioactive fossils damage other specimens?
Maniraptora posted a topic in General Fossil Discussion
I know next to nothing about radioactivity-- enough to know licking fossils is inadvisable, although I'll admit that wasn't terribly disappointing news. What I'm wondering is whether specimens not radioactive enough to endanger a person are capable of damaging other specimens. Is there a need to segregate displays here, or am I just confused about the mechanics of this? My specific reason for asking is that at the moment I'm planning for my current favorite mineral specimen (which I am babying forever), an almandine garnet from Broken Hill, New South Wales, Australia, to share a small shelf area with a tooth from the phosphate deposits in Oulad Abdoun Basin, Morocco and a few dinosaur bone pieces from the Hell Creek Formation of Montana (one from Dawson County) and Lance Creek Formation of Niobrara County, Wyoming. The shelf is not enclosed, by the way. Thanks for your help! -
Hello, this is a very small tooth that I had a hard time taking pictures of. I need a new camera or phone able to take nice up close pics!! This tooth was found at a site in Wyoming that I am unsure whether it is Lance or Mesa Verde formation wise. Anyway, this tooth is complete and very nice looking. I believe it is Ceratopsian but as to which species I am unsure. You can see the size of it as compared to my finger (sorry, I work with oil based materials and my fingers are stained up!). Please let me know what opinions y'all have!
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Hi I am going to Wyoming, Montana and maybe South Dakota with my brother in late May and very early June 2023. And we would of course like to look for dinosaur fossils. We know we are not allowed to collect on "State land". But can anyone help with contact to a private owner of land with dinosaurfossils. So we can pay for a couple of days and bring a few things home to Denmark. (I know of Paleoadventures). Hope someone can help us. Thank you and kind regards Torben
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Hi everyone, I am extremely sick today, so I decided to go through my fossils I found in Wyoming over the years while laying in bed. While going through my fossils, I found a piece of large exposed Coprolite. I thought to myself, “I might as well try to extract it. I’ve got nothing else to do because I’m so sick.“ After about 10 minutes of working with it, I was able to extract it in one piece. Then, it broke in my hand into two pieces. To my surprise, inside the Coprolite where it broke, there were bones. Looks like fish bones. Whatever left this Coprolite behind may have been carnivorous. This leads me to my question. Is there any way to tell what animal left this coprolite? If so, what animal left it behind? Any help will be appreciated, Jared
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Here is a great video from a geologist that explains how purported giant tree fossils form. Reminds me of what we try to do on the Forum: using geological principles and logic to determine if a rock is a fossil. Debunking purported fossils seem to be a Sisyphean task around here.
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Hey all. I had these pictures sent to me by a friend, and we're both totally stumped over what this possibly could be. It was found pretty densely surrounded by other shattered bone. Any help at all would be greatly appreciated- we've really been scratching our heads over this one!
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Hello, I believe this bone shows evidence of teeth scoring from a predator Dinosaur (raptor or other theropod) and I am asking for a confirmation of this. I found this a few days ago in Wyoming in a formation I believe may be the Lance but I am not sure. Teeth there include Archeroraptor, other Dromeausaurid (sp), triceratops, avaceratops, paralbula, myledaphus, hybodus shark, edmontosaurus, borealasucbus, brachychampsus, fish, a couple of mammal types, large theropods, Aublysodon?, lissodon, Ankylosaurid, melvius as the most commonly found specimens. Of course, none are common but just in comparison to other fossils.
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New long-necked polycotylid plesiosaur discovered in Wyoming
pachy-pleuro-whatnot-odon posted a topic in Fossil News
A new polycotylid plesiosaur has been recovered from the upper half of the upper member of the lower Maastrichtian (Late Cretaceous) Pierre Shale Formation of Wyoming: Serpentisuchops pfisterae, the snake-like crocodile face. The interesting aspect to this new discovery is that this polycotylid, contrary to most other known members of this clade (that is, all with the exception of the Turonian Thililua longicollis and Manemergus anguirostris from Morocco), has a elongated neck, convergent on those of elasmosauridae. The pertinent article can be found here: Scott Persons IV, Street and Kelley, 2022. A long-snouted and long-necked polycotylid plesiosaur from the Late Cretaceous of North America.
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I had the opportunity to cruise around Wyoming, Colorado, and Utah on my own for 5 days The first day of my fossil hunting excursion was to be spent at the Petrified Blue Forest site in Western Wyoming. Having been there before, I knew fragments of wood abound, many carrying the blue agate on it. But I was determined to find a “large” log this trip. I had researched how to up my odds and stopped at a hardware store the night before and purchased a shovel as step one. So early that morning, I found myself looking out at the vastness of this “forest” thinking where to start. That is when this antelope startled me. After a short stare down both the antelope and I were on our merry way. Soon after stepping out of my vehicle to scout around, I began finding many small pieces of petrified wood with the characteristic blue agate that everyone is after. Here is a piece of wood next to a skull that I do not recognize. Any thoughts about what animal this was? After an hour, and not finding anything substantial, I jumped back into the car and followed an obscure path that led me to the top of a hill. From up here, one can appreciate the vastness of the region. Looking around told me that petrified wood existed even up here. So out came the shovel again. The ground is made up of a loosely broken sedimentary like rock that can be shoveled with some (much) difficulty. As I dug, my eyes were intently focused on the hole created looking for a hint of an algae fossil that has a very distinct look to it. Why look for algae???? Because within the algal mat is where the wood lies! Finally, after many digs, some significant algae appeared in my hole. Here is a picture of it as found and the debris surrounding it removed. A piece of the top layer of algae is removed, exposing the wood inside. Unfortunately, when I tried to wedge the log out of its hiding place it split in two, leaving this piece in tact and the other piece in a crumbled mess. Thank goodness I had purchased a small container of acetone at the store and I immediately added it to the Paraloid B 72 crystals I had brought with me from Minnesota. This stabilized the intact piece fairly well, though I could have used many more resin crystals than what I packed. The Blue Forest wood was deposited into a fresh water, algae filled, shallow lake that was full of silica. Soon after the fresh wood was deposited in the water, algae formed a thick crust around it. Here is a small branch showing the layering of algae. The wood with time shrunk, providing space for the silica rich water to do its thing!!!! In addition to the mineral deposits, this wood has exquisite preservation due to the algae blanket protecting it from the elements. Here is a piece that shows the boring holes by insects as fresh as if they were made today. Now some of my specimens brought home. Unfortunately, the specimens found on top of the Butte contained mostly yellow calcite crystals. Next time I will stay down below and hope for much bluer specimens. Here is a branch that was completely mineralized!!
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A Surprise Geology Lesson on my Trip From Farson, Wyoming to Vernal, Utah
minnbuckeye posted a topic in Fossil Hunting Trips
On a recent trip out west, I ended my day of collecting petrified wood in the Farson, Wyoming area by driving to Vernal, Utah. On this trip through some gorgeous country, I was pleasantly surprised by occasional roadside signs telling of the geology that I was traveling through. And by the time I arrived in Vernal, I feel I had a better understanding of the local geology!!! Thanks to whoever was responsible for the signage. Here was my lesson! One question I have about the next formation, the Mowry Shale. I did pull over here to stretch my legs and found a few pieces of matrix that contained some nice fish scales. It wasn't until I returned home and saw these that it occurred to me, did I collect this illegally along the road's right of way? Are vertebrate fossils open to collection on a road right of way?
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Found this tooth on the Powder River in Wyoming. I don't know much but my best guess is a real young Mammoth tooth? Thanks for the help.
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Hello, Is this a Knightia eocaena? It's from the Green River Fm. of Wyoming, USA, and measures ~8.5 cm long. Thanks.
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In the summer of 2020 jpc and I had planned to get together in Eastern Wyoming to collect. That trip was unfortunately aborted by the coronavirus outbreak that year. This year, that conversation resumed and a new plan for a three day excursion in June emerged. I decided to make it a two week long car trip, driving all the way from New York, a longer car trip than any I've made in the past 25 years. That would afford me the opportunity to stop at some other sites on the way there and back, plus see some family. Another big reason for driving was an opportunity to visit and collect at the Big Cedar Ridge Cretaceous plant site. Having the car would afford me the opportunity to bring the necessary tools and be able to transport the fragile specimens safely. The rising price of gasoline certainly had an impact, and my plan was to cut costs as much as possible wherever I could. Part of that plan was camping 10 nights I departed the suburbs of New York City on Saturday, June 11th. That evening I arrived at Sturgis, MI, just off interstate 80. Spent the night in a motel and headed off the next day, driving through the heart of Chicago enshrouded in mist. It was my very first time driving through that city. I headed north and in the middle of the day arrived at my cousin's place in Madison, WI. He had moved there from Manhattan five years ago to teach music at the University of Wisconsin. This was my first time visiting him there, my first time in Wisconsin, actually. He took me on a lovely tour of the school and the town. I spent the night and was on my way again just before noon the next day. It rained off and on as I drove through Western Wisconsin and crossed the Mississippi into Dubuque, Iowa. From there it was a short drive to my first fossil stop- at Graf. This Upper Ordovician site in Maquoketa Formation is famous for its nautiloid death assemblage. I have found quite a few nautiloids over the course of my collecting career, but I've never encountered a site where they are thoroughly dominant. There was a layer of limestone, a few feet thick that was in many places just packed with their shells.
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Wyoming Amber in Matrix (Hanna Fm., ~57-56 Ma)
Barrelcactusaddict posted a gallery image in Member Collections
From the album: Fossil Amber and Copal: Worldwide Localities
Specimen: 9.0g / 43x28x12mm Collected June 15, 2022 "Glory Hole" Site Hanna Basin Carbon County, WY Hanna Formation (~57-56 Ma) Deposit: *While amber is found throughout the Hanna Basin, only one site is known to yield large pieces of clear, stable amber: the locality known as "Glory Hole" is located within the north-central section of the Hanna Basin, in south-central Wyoming; exposures are positioned about 8,500 ft. above the base of the Hanna Fm., and at an elevation of roughly 8,900 ft. above sea level. Extensive layers of lignite and carbonaceous (lignitic) mudstone host abundant plant fossils and amber; the matrix is fissile (easily separated into thin layers) and friable (crumbly). Physical weathering (freeze-thaw, wind erosion, thermal expansion, etc.) of the exposures has created an expansive area of disintegrated substrate. This particular site was once a watery paleoenvironment, characterized by shallow swamps. At the very top of the bluff are layers of fissile, light-colored shale referred to as the "Upper Lacustrine Unit" of the Hanna Fm. Amber: *Occurring as small droplets, runs, and globular masses, much of the amber is transparent and of a reddish-orange color throughout, with some containing plentiful internal fractures. The intact, non-fractured amber is very hard, measuring 2.5-3.0 on the Mohs scale, being generally harder than Dominican and Chiapas ambers. It is very fragile and fractures easily, but takes a high, glassy polish like Myanmar amber. Through PyGC-MS, the amber is shown to come from a cupressaceous source tree, and is extremely similar chemically to cretaceous amber from the Raritan Fm. in New Jersey. Of several hundreds of pieces collected by some of the authors, et al., of the cited publication, prepared, and studied at the American Museum of Natural History, only one contained a single insect inclusion: a wingless thrips (1.1mm) that was heavily-compressed and deformed due to geologic forces. From my time at the site, I observed that much of the in-situ amber, especially large pieces, was concentrated within a short horizon only a couple feet in depth. It was especially common near buried, coalified remains of branches and logs, and matrix layers containing numerous leaf remains (mostly cupressaceous). Additionally, I've noticed that some of this material is fairly phosphorescent when exposed to longwave UV light. Minerals and Fossils: While collecting at the site, I noticed several other interesting features besides the amber I sought: carbonized leaves were present in some of the separated matrix layers, petrified wood was present in-situ and eroded from the matrix, and transparent gypsum crystals (some being relatively large) were commonly exposed along the site's surface. Also found in-situ were coalified twigs, branches, logs, and even stumps; I had partially uncovered a few such logs in my shallow excavations (6-12" deep) for amber. I observed a few stumps (~15" diameter) still preserved in an upright position, perpendicular to the matrix layers, with the majority of the lignitic remains buried beneath the surface. Recovered from coarse-grained sandstone originating from above the lignite deposits, was a partial angiosperm leaf imprint with distinct veins. Significance of Hanna Basin Deposits: *Throughout the Hanna Basin, amber is found in various quantities, physical conditions, sizes, and ages: the age range of the ambers' host strata sequence ranges from Late Cretaceous to Late Paleocene (76-56 Ma), an unprecedented range among all the world's known amber deposits. A stratigraphic interval more than 5 miles thick separates the highest and lowest occurrences of amber within the Hanna Basin. Paleocene amber is very rare, with only a handful of significant deposits in the world, notably from the Paris Basin and 5 localities in Switzerland. Source: * "Amber from Upper Cretaceous through Paleocene strata of the Hanna Basin, Wyoming, with evidence for source and taphonomy of fossil resins"; Rocky Mountain Geology, Vol. 35, No. 2, pp. 163-204, December 2000; David A. Grimaldi, Jason A. Lillegraven, Thomas W. Wampler, Denise Bookwalter, and Alexander Shedrinsky© Kaegen Lau
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Wyoming Amber in Matrix (Hanna Fm., ~57-56 Ma)
Barrelcactusaddict posted a gallery image in Member Collections
From the album: Fossil Amber and Copal: Worldwide Localities
Specimen: 9.0g / 43x28x12mm Specimen pictured here is fluorescing under exposure to longwave UV light, and also illuminated by ambient LED light. Collected June 15, 2022 "Glory Hole" Site Hanna Basin Carbon County, WY Hanna Formation (~57-56 Ma) Deposit: *While amber is found throughout the Hanna Basin, only one site is known to yield large pieces of clear, stable amber: the locality known as "Glory Hole" is located within the north-central section of the Hanna Basin, in south-central Wyoming; exposures are positioned about 8,500 ft. above the base of the Hanna Fm., and at an elevation of roughly 8,900 ft. above sea level. Extensive layers of lignite and carbonaceous (lignitic) mudstone host abundant plant fossils and amber; the matrix is fissile (easily separated into thin layers) and friable (crumbly). Physical weathering (freeze-thaw, wind erosion, thermal expansion, etc.) of the exposures has created an expansive area of disintegrated substrate. This particular site was once a watery paleoenvironment, characterized by shallow swamps. At the very top of the bluff are layers of fissile, light-colored shale referred to as the "Upper Lacustrine Unit" of the Hanna Fm. Amber: *Occurring as small droplets, runs, and globular masses, much of the amber is transparent and of a reddish-orange color throughout, with some containing plentiful internal fractures. The intact, non-fractured amber is very hard, measuring 2.5-3.0 on the Mohs scale, being generally harder than Dominican and Chiapas ambers. It is very fragile and fractures easily, but takes a high, glassy polish like Myanmar amber. Through PyGC-MS, the amber is shown to come from a cupressaceous source tree, and is extremely similar chemically to cretaceous amber from the Raritan Fm. in New Jersey. Of several hundreds of pieces collected by some of the authors, et al., of the cited publication, prepared, and studied at the American Museum of Natural History, only one contained a single insect inclusion: a wingless thrips (1.1mm) that was heavily-compressed and deformed due to geologic forces. From my time at the site, I observed that much of the in-situ amber, especially large pieces, was concentrated within a short horizon only a couple feet in depth. It was especially common near buried, coalified remains of branches and logs, and matrix layers containing numerous leaf remains (mostly cupressaceous). Additionally, I've noticed that some of this material is fairly phosphorescent when exposed to longwave UV light. Minerals and Fossils: While collecting at the site, I noticed several other interesting features besides the amber I sought: carbonized leaves were present in some of the separated matrix layers, petrified wood was present in-situ and eroded from the matrix, and transparent gypsum crystals (some being relatively large) were commonly exposed along the site's surface. Also found in-situ were coalified twigs, branches, logs, and even stumps; I had partially uncovered a few such logs in my shallow excavations (6-12" deep) for amber. I observed a few stumps (~15" diameter) still preserved in an upright position, perpendicular to the matrix layers, with the majority of the lignitic remains buried beneath the surface. Recovered from coarse-grained sandstone originating from above the lignite deposits, was a partial angiosperm leaf imprint with distinct veins. Significance of Hanna Basin Deposits: *Throughout the Hanna Basin, amber is found in various quantities, physical conditions, sizes, and ages: the age range of the ambers' host strata sequence ranges from Late Cretaceous to Late Paleocene (76-56 Ma), an unprecedented range among all the world's known amber deposits. A stratigraphic interval more than 5 miles thick separates the highest and lowest occurrences of amber within the Hanna Basin. Paleocene amber is very rare, with only a handful of significant deposits in the world, notably from the Paris Basin and 5 localities in Switzerland. Source: * "Amber from Upper Cretaceous through Paleocene strata of the Hanna Basin, Wyoming, with evidence for source and taphonomy of fossil resins"; Rocky Mountain Geology, Vol. 35, No. 2, pp. 163-204, December 2000; David A. Grimaldi, Jason A. Lillegraven, Thomas W. Wampler, Denise Bookwalter, and Alexander Shedrinsky© Kaegen Lau
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VIDEO: Wyoming Amber (Hanna Fm., ~57-56 Ma)
Barrelcactusaddict posted a gallery image in Member Collections
From the album: Fossil Amber and Copal: Worldwide Localities
Field Collection: June 12-15, 2022 "Glory Hole" Site Hanna Basin Carbon County, WY Hanna Formation (~57-56 Ma) Deposit: *While amber is found throughout the Hanna Basin, only one site is known to yield large pieces of clear, stable amber: the locality known as "Glory Hole" is located within the north-central section of the Hanna Basin, in south-central Wyoming; exposures are positioned about 8,500 ft. above the base of the Hanna Fm., and at an elevation of roughly 8,900 ft. above sea level. Extensive layers of lignite and carbonaceous (lignitic) mudstone host abundant plant fossils and amber; the matrix is fissile (easily separated into thin layers) and friable (crumbly). Physical weathering (freeze-thaw, wind erosion, thermal expansion, etc.) of the exposures has created an expansive area of disintegrated substrate. This particular site was once a watery paleoenvironment, characterized by shallow swamps. At the very top of the bluff are layers of fissile, light-colored shale referred to as the "Upper Lacustrine Unit" of the Hanna Fm. Amber: *Occurring as small droplets, runs, and globular masses, much of the amber is transparent and of a reddish-orange color throughout, with some containing plentiful internal fractures. The intact, non-fractured amber is very hard, measuring 2.5-3.0 on the Mohs scale, being generally harder than Dominican and Chiapas ambers. It is very fragile and fractures easily, but takes a high, glassy polish like Myanmar amber. Through PyGC-MS, the amber is shown to come from a cupressaceous source tree, and is extremely similar chemically to cretaceous amber from the Raritan Fm. in New Jersey. Of several hundreds of pieces collected by some of the authors, et al., of the cited publication, prepared, and studied at the American Museum of Natural History, only one contained a single insect inclusion: a wingless thrips (1.1mm) that was heavily-compressed and deformed due to geologic forces. From my time at the site, I observed that much of the in-situ amber, especially large pieces, was concentrated within a short horizon only a couple feet in depth. It was especially common near buried, coalified remains of branches and logs, and matrix layers containing numerous leaf remains (mostly cupressaceous). Additionally, I've noticed that some of this material is fairly phosphorescent when exposed to longwave UV light. Minerals and Fossils: While collecting at the site, I noticed several other interesting features besides the amber I sought: carbonized leaves were present in some of the separated matrix layers, petrified wood was present in-situ and eroded from the matrix, and transparent gypsum crystals (some being relatively large) were commonly exposed along the site's surface. Also found in-situ were coalified twigs, branches, logs, and even stumps; I had partially uncovered a few such logs in my shallow excavations (6-12" deep) for amber. I observed a few stumps (~15" diameter) still preserved in an upright position, perpendicular to the matrix layers, with the majority of the lignitic remains buried beneath the surface. Recovered from coarse-grained sandstone originating from above the lignite deposits, was a partial angiosperm leaf imprint with distinct veins. Significance of Hanna Basin Deposits: *Throughout the Hanna Basin, amber is found in various quantities, physical conditions, sizes, and ages: the age range of the ambers' host strata sequence ranges from Late Cretaceous to Late Paleocene (76-56 Ma), an unprecedented range among all the world's known amber deposits. A stratigraphic interval more than 5 miles thick separates the highest and lowest occurrences of amber within the Hanna Basin. Paleocene amber is very rare, with only a handful of significant deposits in the world, notably from the Paris Basin and 5 localities in Switzerland. Source: * "Amber from Upper Cretaceous through Paleocene strata of the Hanna Basin, Wyoming, with evidence for source and taphonomy of fossil resins"; Rocky Mountain Geology, Vol. 35, No. 2, pp. 163-204, December 2000; David A. Grimaldi, Jason A. Lillegraven, Thomas W. Wampler, Denise Bookwalter, and Alexander Shedrinsky© Kaegen Lau
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VIDEO: Wyoming Amber (Hanna Fm., ~57-56 Ma)
Barrelcactusaddict posted a gallery image in Member Collections
From the album: Fossil Amber and Copal: Worldwide Localities
Field Collection: June 12-15, 2022 432.5g of amber recovered; lot is initially displaying fluorescence under longwave ultraviolet light (365nm). "Glory Hole" Site Hanna Basin Carbon County, WY Hanna Formation (~57-56 Ma) Deposit: *While amber is found throughout the Hanna Basin, only one site is known to yield large pieces of clear, stable amber: the locality known as "Glory Hole" is located within the north-central section of the Hanna Basin, in south-central Wyoming; exposures are positioned about 8,500 ft. above the base of the Hanna Fm., and at an elevation of roughly 8,900 ft. above sea level. Extensive layers of lignite and carbonaceous (lignitic) mudstone host abundant plant fossils and amber; the matrix is fissile (easily separated into thin layers) and friable (crumbly). Physical weathering (freeze-thaw, wind erosion, thermal expansion, etc.) of the exposures has created an expansive area of disintegrated substrate. This particular site was once a watery paleoenvironment, characterized by shallow swamps. At the very top of the bluff are layers of fissile, light-colored shale referred to as the "Upper Lacustrine Unit" of the Hanna Fm. Amber: *Occurring as small droplets, runs, and globular masses, much of the amber is transparent and of a reddish-orange color throughout, with some containing plentiful internal fractures. The intact, non-fractured amber is very hard, measuring 2.5-3.0 on the Mohs scale, being generally harder than Dominican and Chiapas ambers. It is very fragile and fractures easily, but takes a high, glassy polish like Myanmar amber. Through PyGC-MS, the amber is shown to come from a cupressaceous source tree, and is extremely similar chemically to cretaceous amber from the Raritan Fm. in New Jersey. Of several hundreds of pieces collected by some of the authors, et al., of the cited publication, prepared, and studied at the American Museum of Natural History, only one contained a single insect inclusion: a wingless thrips (1.1mm) that was heavily-compressed and deformed due to geologic forces. From my time at the site, I observed that much of the in-situ amber, especially large pieces, was concentrated within a short horizon only a couple feet in depth. It was especially common near buried, coalified remains of branches and logs, and matrix layers containing numerous leaf remains (mostly cupressaceous). Additionally, I've noticed that some of this material is fairly phosphorescent when exposed to longwave UV light. Minerals and Fossils: While collecting at the site, I noticed several other interesting features besides the amber I sought: carbonized leaves were present in some of the separated matrix layers, petrified wood was present in-situ and eroded from the matrix, and transparent gypsum crystals (some being relatively large) were commonly exposed along the site's surface. Also found in-situ were coalified twigs, branches, logs, and even stumps; I had partially uncovered a few such logs in my shallow excavations (6-12" deep) for amber. I observed a few stumps (~15" diameter) still preserved in an upright position, perpendicular to the matrix layers, with the majority of the lignitic remains buried beneath the surface. Recovered from coarse-grained sandstone originating from above the lignite deposits, was a partial angiosperm leaf imprint with distinct veins. Significance of Hanna Basin Deposits: *Throughout the Hanna Basin, amber is found in various quantities, physical conditions, sizes, and ages: the age range of the ambers' host strata sequence ranges from Late Cretaceous to Late Paleocene (76-56 Ma), an unprecedented range among all the world's known amber deposits. A stratigraphic interval more than 5 miles thick separates the highest and lowest occurrences of amber within the Hanna Basin. Paleocene amber is very rare, with only a handful of significant deposits in the world, notably from the Paris Basin and 5 localities in Switzerland. Source: * "Amber from Upper Cretaceous through Paleocene strata of the Hanna Basin, Wyoming, with evidence for source and taphonomy of fossil resins"; Rocky Mountain Geology, Vol. 35, No. 2, pp. 163-204, December 2000; David A. Grimaldi, Jason A. Lillegraven, Thomas W. Wampler, Denise Bookwalter, and Alexander Shedrinsky© Kaegen Lau
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VIDEO: Wyoming Amber (Hanna Fm., ~57-56 Ma)
Barrelcactusaddict posted a gallery image in Member Collections
From the album: Fossil Amber and Copal: Worldwide Localities
Field Collection: June 12-15, 2022 "Glory Hole" Site Hanna Basin Carbon County, WY Hanna Formation (~57-56 Ma) Deposit: *While amber is found throughout the Hanna Basin, only one site is known to yield large pieces of clear, stable amber: the locality known as "Glory Hole" is located within the north-central section of the Hanna Basin, in south-central Wyoming; exposures are positioned about 8,500 ft. above the base of the Hanna Fm., and at an elevation of roughly 8,900 ft. above sea level. Extensive layers of lignite and carbonaceous (lignitic) mudstone host abundant plant fossils and amber; the matrix is fissile (easily separated into thin layers) and friable (crumbly). Physical weathering (freeze-thaw, wind erosion, thermal expansion, etc.) of the exposures has created an expansive area of disintegrated substrate. This particular site was once a watery paleoenvironment, characterized by shallow swamps. At the very top of the bluff are layers of fissile, light-colored shale referred to as the "Upper Lacustrine Unit" of the Hanna Fm. Amber: *Occurring as small droplets, runs, and globular masses, much of the amber is transparent and of a reddish-orange color throughout, with some containing plentiful internal fractures. The intact, non-fractured amber is very hard, measuring 2.5-3.0 on the Mohs scale, being generally harder than Dominican and Chiapas ambers. It is very fragile and fractures easily, but takes a high, glassy polish like Myanmar amber. Through PyGC-MS, the amber is shown to come from a cupressaceous source tree, and is extremely similar chemically to cretaceous amber from the Raritan Fm. in New Jersey. Of several hundreds of pieces collected by some of the authors, et al., of the cited publication, prepared, and studied at the American Museum of Natural History, only one contained a single insect inclusion: a wingless thrips (1.1mm) that was heavily-compressed and deformed due to geologic forces. From my time at the site, I observed that much of the in-situ amber, especially large pieces, was concentrated within a short horizon only a couple feet in depth. It was especially common near buried, coalified remains of branches and logs, and matrix layers containing numerous leaf remains (mostly cupressaceous). Additionally, I've noticed that some of this material is fairly phosphorescent when exposed to longwave UV light. Minerals and Fossils: While collecting at the site, I noticed several other interesting features besides the amber I sought: carbonized leaves were present in some of the separated matrix layers, petrified wood was present in-situ and eroded from the matrix, and transparent gypsum crystals (some being relatively large) were commonly exposed along the site's surface. Also found in-situ were coalified twigs, branches, logs, and even stumps; I had partially uncovered a few such logs in my shallow excavations (6-12" deep) for amber. I observed a few stumps (~15" diameter) still preserved in an upright position, perpendicular to the matrix layers, with the majority of the lignitic remains buried beneath the surface. Recovered from coarse-grained sandstone originating from above the lignite deposits, was a partial angiosperm leaf imprint with distinct veins. Significance of Hanna Basin Deposits: *Throughout the Hanna Basin, amber is found in various quantities, physical conditions, sizes, and ages: the age range of the ambers' host strata sequence ranges from Late Cretaceous to Late Paleocene (76-56 Ma), an unprecedented range among all the world's known amber deposits. A stratigraphic interval more than 5 miles thick separates the highest and lowest occurrences of amber within the Hanna Basin. Paleocene amber is very rare, with only a handful of significant deposits in the world, notably from the Paris Basin and 5 localities in Switzerland. Source: * "Amber from Upper Cretaceous through Paleocene strata of the Hanna Basin, Wyoming, with evidence for source and taphonomy of fossil resins"; Rocky Mountain Geology, Vol. 35, No. 2, pp. 163-204, December 2000; David A. Grimaldi, Jason A. Lillegraven, Thomas W. Wampler, Denise Bookwalter, and Alexander Shedrinsky© Kaegen Lau
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VIDEO: "Glory Hole" Amber Deposit (Hanna Basin, Wyoming)
Barrelcactusaddict posted a gallery image in Member Collections
From the album: Fossil Amber and Copal: Worldwide Localities
Field Collection: June 12-15, 2022 "Glory Hole" Site Hanna Basin Carbon County, WY Hanna Formation (~57-56 Ma) Deposit: *While amber is found throughout the Hanna Basin, only one site is known to yield large pieces of clear, stable amber: the locality known as "Glory Hole" is located within the north-central section of the Hanna Basin, in south-central Wyoming; exposures are positioned about 8,500 ft. above the base of the Hanna Fm., and at an elevation of roughly 8,900 ft. above sea level. Extensive layers of lignite and carbonaceous (lignitic) mudstone host abundant plant fossils and amber; the matrix is fissile (easily separated into thin layers) and friable (crumbly). Physical weathering (freeze-thaw, wind erosion, thermal expansion, etc.) of the exposures has created an expansive area of disintegrated substrate. This particular site was once a watery paleoenvironment, characterized by shallow swamps. At the very top of the bluff are layers of fissile, light-colored shale referred to as the "Upper Lacustrine Unit" of the Hanna Fm. Amber: *Occurring as small droplets, runs, and globular masses, much of the amber is transparent and of a reddish-orange color throughout, with some containing plentiful internal fractures. The intact, non-fractured amber is very hard, measuring 2.5-3.0 on the Mohs scale, being generally harder than Dominican and Chiapas ambers. It is very fragile and fractures easily, but takes a high, glassy polish like Myanmar amber. Through PyGC-MS, the amber is shown to come from a cupressaceous source tree, and is extremely similar chemically to cretaceous amber from the Raritan Fm. in New Jersey. Of several hundreds of pieces collected by some of the authors, et al., of the cited publication, prepared, and studied at the American Museum of Natural History, only one contained a single insect inclusion: a wingless thrips (1.1mm) that was heavily-compressed and deformed due to geologic forces. From my time at the site, I observed that much of the in-situ amber, especially large pieces, was concentrated within a short horizon only a couple feet in depth. It was especially common near buried, coalified remains of branches and logs, and matrix layers containing numerous leaf remains (mostly cupressaceous). Additionally, I've noticed that some of this material is fairly phosphorescent when exposed to longwave UV light. Minerals and Fossils: While collecting at the site, I noticed several other interesting features besides the amber I sought: carbonized leaves were present in some of the separated matrix layers, petrified wood was present in-situ and eroded from the matrix, and transparent gypsum crystals (some being relatively large) were commonly exposed along the site's surface. Also found in-situ were coalified twigs, branches, logs, and even stumps; I had partially uncovered a few such logs in my shallow excavations (6-12" deep) for amber. I observed a few stumps (~15" diameter) still preserved in an upright position, perpendicular to the matrix layers, with the majority of the lignitic remains buried beneath the surface. Recovered from coarse-grained sandstone originating from above the lignite deposits, was a partial angiosperm leaf imprint with distinct veins. Significance of Hanna Basin Deposits: *Throughout the Hanna Basin, amber is found in various quantities, physical conditions, sizes, and ages: the age range of the ambers' host strata sequence ranges from Late Cretaceous to Late Paleocene (76-56 Ma), an unprecedented range among all the world's known amber deposits. A stratigraphic interval more than 5 miles thick separates the highest and lowest occurrences of amber within the Hanna Basin. Paleocene amber is very rare, with only a handful of significant deposits in the world, notably from the Paris Basin and 5 localities in Switzerland. Source: * "Amber from Upper Cretaceous through Paleocene strata of the Hanna Basin, Wyoming, with evidence for source and taphonomy of fossil resins"; Rocky Mountain Geology, Vol. 35, No. 2, pp. 163-204, December 2000; David A. Grimaldi, Jason A. Lillegraven, Thomas W. Wampler, Denise Bookwalter, and Alexander Shedrinsky© Kaegen Lau
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VIDEO: "Glory Hole" Amber Deposit (Hanna Basin, Wyoming)
Barrelcactusaddict posted a gallery image in Member Collections
From the album: Fossil Amber and Copal: Worldwide Localities
Field Collection: June 12-15, 2022 "Glory Hole" Site Hanna Basin Carbon County, WY Hanna Formation (~57-56 Ma) Deposit: *While amber is found throughout the Hanna Basin, only one site is known to yield large pieces of clear, stable amber: the locality known as "Glory Hole" is located within the north-central section of the Hanna Basin, in south-central Wyoming; exposures are positioned about 8,500 ft. above the base of the Hanna Fm., and at an elevation of roughly 8,900 ft. above sea level. Extensive layers of lignite and carbonaceous (lignitic) mudstone host abundant plant fossils and amber; the matrix is fissile (easily separated into thin layers) and friable (crumbly). Physical weathering (freeze-thaw, wind erosion, thermal expansion, etc.) of the exposures has created an expansive area of disintegrated substrate. This particular site was once a watery paleoenvironment, characterized by shallow swamps. At the very top of the bluff are layers of fissile, light-colored shale referred to as the "Upper Lacustrine Unit" of the Hanna Fm. Amber: *Occurring as small droplets, runs, and globular masses, much of the amber is transparent and of a reddish-orange color throughout, with some containing plentiful internal fractures. The intact, non-fractured amber is very hard, measuring 2.5-3.0 on the Mohs scale, being generally harder than Dominican and Chiapas ambers. It is very fragile and fractures easily, but takes a high, glassy polish like Myanmar amber. Through PyGC-MS, the amber is shown to come from a cupressaceous source tree, and is extremely similar chemically to cretaceous amber from the Raritan Fm. in New Jersey. Of several hundreds of pieces collected by some of the authors, et al., of the cited publication, prepared, and studied at the American Museum of Natural History, only one contained a single insect inclusion: a wingless thrips (1.1mm) that was heavily-compressed and deformed due to geologic forces. From my time at the site, I observed that much of the in-situ amber, especially large pieces, was concentrated within a short horizon only a couple feet in depth. It was especially common near buried, coalified remains of branches and logs, and matrix layers containing numerous leaf remains (mostly cupressaceous). Additionally, I've noticed that some of this material is fairly phosphorescent when exposed to longwave UV light. Minerals and Fossils: While collecting at the site, I noticed several other interesting features besides the amber I sought: carbonized leaves were present in some of the separated matrix layers, petrified wood was present in-situ and eroded from the matrix, and transparent gypsum crystals (some being relatively large) were commonly exposed along the site's surface. Also found in-situ were coalified twigs, branches, logs, and even stumps; I had partially uncovered a few such logs in my shallow excavations (6-12" deep) for amber. I observed a few stumps (~15" diameter) still preserved in an upright position, perpendicular to the matrix layers, with the majority of the lignitic remains buried beneath the surface. Recovered from coarse-grained sandstone originating from above the lignite deposits, was a partial angiosperm leaf imprint with distinct veins. Significance of Hanna Basin Deposits: *Throughout the Hanna Basin, amber is found in various quantities, physical conditions, sizes, and ages: the age range of the ambers' host strata sequence ranges from Late Cretaceous to Late Paleocene (76-56 Ma), an unprecedented range among all the world's known amber deposits. A stratigraphic interval more than 5 miles thick separates the highest and lowest occurrences of amber within the Hanna Basin. Paleocene amber is very rare, with only a handful of significant deposits in the world, notably from the Paris Basin and 5 localities in Switzerland. Source: * "Amber from Upper Cretaceous through Paleocene strata of the Hanna Basin, Wyoming, with evidence for source and taphonomy of fossil resins"; Rocky Mountain Geology, Vol. 35, No. 2, pp. 163-204, December 2000; David A. Grimaldi, Jason A. Lillegraven, Thomas W. Wampler, Denise Bookwalter, and Alexander Shedrinsky© Kaegen Lau
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