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  1. i.amsherlocked

    Found on a mountain top

    Found on a mountain top in the rockies, any idea what it could be? I was wondering if it could be Cambrian?
  2. WOW, what a day! Today I had the pleasure of finally meeting @Jared C after over a year of reading his trip reports and admiring all of the incredible finds he's made exploring the Cretaceous formations of Central Texas. We have a lot in common: both of us are pursuing a career in paleontology, are both (almost) the same age, and are both attending universities in-state that are only an hour and a half away from each other. Needless to say, I can't believe it took us this long to finally go on a hunt together. Jared drove up from his new place in College Station this morning to meet me at my apartment and from there we set off in search of an exposure of the Eagle Ford formation I wasn't sure existed. Last spring I became very active in the geology society here at Baylor, and as a result I found a treasure trove of old literature published by the university in the '70's and '80's. More than a few of the many booklets, articles, and papers I searched through contained almost exact directions to several interesting locales that were apparently known for producing vertebrate material, specifically shark teeth. I cross referenced Google Maps, marked the spots likeliest to be the ones I had read about, and then....did nothing. I was a little too busy with school work at the end of last semester to have the energy to go scout out new locations with a high probability of finding nothing, and so I sat on the information I'd found. Flash forward to earlier this week when Jared and I were talking to each other on Instagram about the incredible plesiosaur tooth he recently found and the topic of the exposure I had read about got brought back up. It wasn't long before he had made plans to visit and help me do some legwork in a formation he was much more familiar with than myself. Just after noon we arrived at the spot. Getting to the location I had predicted to be the exposure was incredibly easy, and in no time my hunch was proven right when we found ourselves facing a steep wall of grey shale. It's worth saying now that I'm a believer in luck, specifically as it relates to fossil hunting trips. Almost all of my best finds have been found when I was with other people. With Jared being so notorious here on the forum for the insane rarity of some of his finds, I had high hopes that some of that luck would rub off on me today - and it seems like it did! Less than a minute after arriving at the Eagle Ford exposure I spotted a Squalicorax falcatus tooth lying on top of some loose shale. I was incredibly excited, as the only shark teeth I've ever found coming fresh out of the formation they originated from is the Grayson that's exposed most famously at the Waco Pit. Even better, finding a tooth this fast meant that that there must be a lot more to be found. Jared congratulated me on the find and the two of us immediately started scanning the shale for a line of shell hash that might indicate more teeth. After what could only have been two or three minutes at most, I laid eyes on my best find to date. Sandwiched between a couple of roots and a thick layer of sandstone was a line of tooth sockets extending directly back into the wall of shale. If I thought I had been excited by the shark tooth just a few minutes prior, I was wrong - NOW I was excited! After several exclamations of "oh my god I found a jaw!" Jared hustled back over to where I was standing and confirmed that yes, my eyes weren't deceiving me. We took a bunch of pictures from several different angles of the bone as it was without being disturbed in case it turned out to be a significant find or if there was articulated material covered up by the shale. Here's a view of the shale wall with my gardening knife marking the spot just below where the jaw was located: After examining what portions of the jawbone we could see that were already exposed, Jared ruled out marine reptile pretty fast. That left bony fish as the only real contender. Based on the shape of the jaw and the differently-sized sockets, I reasoned that we had a Xiphactinus on our hands. With a tentative ID, probably as many pictures taken in the span of a few minutes as possible, and the exact location marked on my phone, all that was left to do was excavate the fish. This proved to be incredibly challenging. Shale is a lot easier to separate and break apart than something like limestone, but unfortunately it's also more similar to soil - roots surrounded the fossil on almost all sides and would be a pain to remove. Jared's pocketknife and the serrated edge of my gardening knife were both pretty blunt, but after several minutes' worth of sawing away we were able to remove the offenders and clear away some of the overburden in the process. What was immediately clear was that what was exposed wasn't a jawbone, but instead the maxillary, with what seemed like a fair amount of the skull and facial elements attached. Traversing the rest of the exposure to find more shark teeth no longer seemed like the direction the day was headed, but to say I didn't mind would be an understatement! During the hours we spent crouched amongst the loose shale, slowly chipping away at the earth around the fossil with a dental pick and a knife, I was immensely glad that I had waited to explore this location with someone else who knew what they were doing when it came to articulated remains (and in this formation no less!), as I had never come across anything like it before. Jared's knowledge from his mosasaur excavation and time spent in the Hell Creek was a lifesaver. Thankfully he had also decided on a whim this morning to bring Paraloid pellets and acetone which saved us a trip to the local Lowe's. After a while it became clear that there wasn't an end to the fish in sight and more overburden shale would need to be cleared out of the way before we continued any farther. Jared produced a roll of aluminum foil from his backpack and we got to work wrapping what was already exposed. Once protected by the foil, the risk of falling shale damaging the fossil was greatly decreased. Once the overburden was cleared it was time to get rid of some more pesky roots. Distinguishing between shale and bone became increasingly difficult as the hours wore on. In many places the bone was the exact same color as the shale that surrounded it. As a result, a couple of pieces were broken off by accident, however, videos were taken explaining where they came from before they were glued back into place. After a while Jared and I both needed a break and some time to stretch our legs. We ended up following the exposure further away from the direction we came from. I followed Jared, and so I squinted my eyes to try and see if I could spot a shark tooth he might have overlooked. That's why I was so surprised when I found an ammonite right next to the snakeskin he'd just been examining. Jared had just started walking away again when I pulled the ammonite out of the shale, flipped it over, and spotted a tiny Ptychodus tooth clinging to the underside of it. After getting home and pulling the tooth out of the matrix tonight, my best guess is that it's a posterior tooth from Ptychodus anonymous, one of the more common species from the Cenomanian; although decurrens is also a possibility. On our way back to the dig site Jared spotted a large slab of limestone with some really eye-catching gastropod internal molds. I wonder why they all seem to be facing the same direction? Finally, after several more hours spent uncovering and preserving the sections of bone we could see, the sun was beginning to set and that meant it was time to leave. The chances of getting the skull out in one piece before we left were looking very unlikely. Jared had initially been optimistic and I wanted to be as well as I knew the forecast for this upcoming week looks like multiple days of rain. Unfortunately it just wasn't doable. We both decided it would be best to cover up the bone still in place with tinfoil and take the assorted loose fragments with us. I took another look at what he had exposed and did a quick mockup later of what the portion of the skull I think we uncovered today looks like (although it's debatable whether or not the orbital is part of that portion just yet): All-in-all, today was one of the best days of fossil hunting I've ever experienced, made even better by great company, amazing finds, good weather, and excellent ice-cold lemonades from Sonic after Jared and I headed home. Some time this week I plan to speak with the paleontology professors at Baylor that I know personally and get their opinion on what should be done next. There is obviously more bone to be found than just what Jared and I were able to uncover today, and I don't have the equipment or the expertise needed to do it properly. Luckily I know quite a few graduate geology students who would be more than willing to help. With the direction of a professor or two we should be able to get the fish out in one piece. I'll make sure to keep everyone posted! I know this is just the sort of thing that I'd be waiting every week to hear more about. Until then.... - Graham
  3. I have collected wet clay or shale with many types of fossils embedded in it. I have found leaves, a fish, a pine cone, wooden bits, ect. Much of the fossils are there and havent turned to rock, so may not be considered an actual fossil. I am hoping some may have ideas on how to preserve these. I got them from Clarkia, ID. There is a youtube video called "Plants are Cool, too! Episode 2: Fossilized Forests!" that talks about the area. I am missing out on fossils opening it a wet clay because I can't split many thin layers, but splitting it in when dry it seems to crumble. Trying to figure out the best process without having to ruin more to get it figured out, any tips? What is the best way to dry it out, and for how long? I also dont know what to do with the pine cone, haha. I dont have the rock impression, I am regretting that I wasnt careful enough to keep it. It is weird that these are dated 15, 000,000 years old but I can pull out the actual biological items out of clay. Also, what do you do with your fossils that are unidentifiable. There are imprints that I dont know if it is from a seed or a bug. I have found actual seeds and such, so I am wondering if these are most likely bug remnants. Is there a good way to know a the difference?
  4. Barrelcactusaddict

    Wyoming Amber in Matrix (Hanna Fm., ~57-56 Ma)

    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

  5. Barrelcactusaddict

    Wyoming Amber in Matrix (Hanna Fm., ~57-56 Ma)

    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

  6. Barrelcactusaddict

    VIDEO: Wyoming Amber (Hanna Fm., ~57-56 Ma)

    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

  7. Barrelcactusaddict

    VIDEO: Wyoming Amber (Hanna Fm., ~57-56 Ma)

    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

  8. Barrelcactusaddict

    VIDEO: Wyoming Amber (Hanna Fm., ~57-56 Ma)

    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

  9. Barrelcactusaddict

    Wyoming Amber in Matrix (Hanna Fm., ~57-56 Ma)

    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

  10. Barrelcactusaddict

    Wyoming Amber in Matrix (Hanna Fm., ~57-56 Ma)

    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

  11. Barrelcactusaddict

    Wyoming Amber in Matrix (Hanna Fm., ~57-56 Ma)

    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

  12. Barrelcactusaddict

    Wyoming Amber in Matrix (Hanna Fm., ~57-56 Ma)

    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

  13. Barrelcactusaddict

    Wyoming Amber (Hanna Fm., ~57-56 Ma)

    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

  14. Barrelcactusaddict

    Wyoming Amber (Hanna Fm., ~57-56 Ma)

    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

  15. Barrelcactusaddict

    Wyoming Amber (Hanna Fm., ~57-56 Ma)

    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

  16. Barrelcactusaddict

    Wyoming Amber in Matrix (Hanna Fm., ~57-56 Ma)

    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

  17. Barrelcactusaddict

    Wyoming Amber (Hanna Fm., ~57-56 Ma)

    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

  18. saidthegirl

    How to prep coral colony?

    I would greatly appreciate any advice on how to clean/prep this coral colony. It was found in a shale pit in northern Iowa-from the Lime Creek formation. As you can see, there’s quite a bit still clinging to it. Is it safe to clean with some water and a toothbrush? The underside seems to have crystallized(?). Very new to fossil collecting and subsequent preparation. Thank you in advance! If anyone has a guess at ID please let me know as well.
  19. Hey there Fossil ID. Reddit couldn't do anything for me so I came here for a chance of getting this fossils ID'd! Here are the main informations I can give you about it: It was found on a roadside shale cliff in Château-Richer, just north of Québec City (Province Of Québec, Canada); According to Québec Government geological maps, the specimen was found in the Upper Ordovician Lotbinière Formation of the Sainte-Rosalie Group (just on top of the Utica shale); Two trilobites and several (dozens and dozens) of graptoliths were found around it; There is a graptolith overlying the main animal/plant I would like to ID, if you look well (reverse "V" shape); The fossil is preserved as some kind of carbon layer, just like graptoliths normally preserve; The specimen is roughly 4 cm long, if you compare it to my (dirty) thumb. Any hint will be greatly appreciated, thank you very much!
  20. All, I have been finding a few dermal denticles in Northeast Oklahoma Pennsylvanian shales. Based on published reports and images from our area, I believe these are Petrodus. I’ve attached an image of two denticles I found yesterday. I’ve been looking for images of the entire shark because I’m curious about the animal’s overall appearance; however, I’m only finding images of the denticles. Do scientists know what these sharks looked like, and if so, does anyone know of resources containing overall images? Best wishes.
  21. Hi! I'm looking for advice. I found this fossil yesterday and like so many others I find it's on an unstable piece and has a major crack through it. I'd hate to coat it with anything as I prefer to keep things natural. Yet I'm also worried that it might just fall apart on its own or from handling. What's my best course of action? Any advice/help is appreciated.
  22. Tales From the Shale

    Alabama Graptolites

    Here are some of the fossils I acquired in a shale roadcut I was told about thanks to @prem. These are ordovician in age, and I have to say it was difficult to collect them due to the fragility of the surrounding material. Ive identified most of my finds, however there were these unusual pill like outlines I wasn't familar with.
  23. I was able to take another trip to the Leighton Formation today! It's been a while since I've been able to visit (months and months), but I've finally been able to. Unfortunately, during the winter the place is completely covered in snow and ice. Not really the best collecting conditions... My last trip there was in August of last year, and the spring has been very busy. Today it was time. It was supposed to be overcast with a chance of rain, but it came out sunny and bright. Absolutely beautiful day out. The collecting was very good. I unfortunately forgot to take a picture of the site. I was working in the same spot as last time, and at another outcrop a little farther down the shoreline. Place hasn't changed much, still as minuscule and weathered as ever. I had a better idea where to look though. Last time, I collected a lot, but I was mainly working in layers where the fossils were very evident. These layers contained a plethora of brachiopods, ostracods, tentaculites and other invertebrates - plus my first conodont. This time, though, I was going to try something a little different. The layers between the extremely fossiliferous layers had finer sediments, and generally seemed to keep the specimens intact better. I chose to mainly work in what I now call the "Chonetes layer". It's the only layer in these outcrops that contain Chonetes bastini brachiopods. The layer doesn't shatter as much as the other shale, so the pieces come out without a lot of cracking. It was also the same place that I found a nice trilo-bit, and I was hoping it would pay off. It did... The best finds of the day went to the trilobite cephalons. I found two Acaste cf. zerinae sp. - mostly intact, but an eye cracked off on the first, and both on the second. I was (luckily) able to find them, and I intend to glue them back on. At least the external molds are completely intact. In all of the following pictures, internal molds come first, external molds second. Cephalon #1, the one-eyed wonder. Cephalon #2 - missing both of the eyes. Sad, it would have been so nice too... Then came the pygidia - four of them! I believe that they are all the same species as the cephalons - A. zerinae - but I could be wrong. I'm sure the trilo-experts here can help me with that. Pygidium #1, the nicest one. Pygidium #2 - this little guy got a bit beat up when the rock split. Pygidium #3 - little bugger needs to be prepped a bit. Pygidium #4 - the internal mold of this cracked in half - and it's missing a piece. This one's a neat little trace fossil. It looks like an infilled burrow to me, but I'll set up a separate thread for that - with better pictures. And this very odd little guy. Another one I'll have to take better pictures on, and as soon as the matrix is pared down a bit I will scrutinize it under a microscope. It's not very evident, but it feathers out at the right end. It could be mineral staining or something, but I'm not sure yet. Then the stuff I couldn't bear to leave behind. I was trying to keep my collecting to new stuff, but some of them just sneaked in there... I feel like we've all experienced this before. Orbiculoidea sp. brachiopod. Lingula sp. brachiopod. Leiopteria rubra bivalve. It was a pretty good day. On top of these finds, I brought back some promising shale pieces to look for micro-fossils in - and a few more interesting unknowns. But that's for another time.. Thanks for reading!
  24. Lucid_Bot

    Hidden Fossil

    Hi, I found this beautiful little asterophyllites yesterday and noticed that there seems to be some rock covering part of the fossil. I'd like to be able to remove the rock and expose the fossil. It's very solid and too thin for any of my chisels. Would an air-abrasive pen or dental equipment work? Perhaps professional help would be appropriate.
  25. deutscheben

    Odd Pennsylvanian shale impressions

    This is probably an extremely long shot, but I wanted to post these interesting pics in case they ring a bell for anyone. These were all found in a Late Pennsylvanian shale associated with the Herrin Coal, which generally preserves plant fossils. I’m not sure if they are fossils or diagenetic artifacts- the shale is baked on the spoil pile which can introduce unusual shapes. The first one is a strange pattern- it appears to be asymmetrical and doesn’t immediately match any plant parts I’m familiar with, but there are so many possibilities I might be missing something. It’s 5 mm wide. This next one is part and counterpart of a smooth cylindrical impression- the entire visible impression is about 15 mm long. These next three could be a result of the heating of the shale, which can produce bubbles and smooth surfaces like these, but it would unusual for that to be the case without any other distortion around it. The final impression comes from the other side of one of the pieces above and is similarly smooth-walled, but only a small portion is visible.
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