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Dinosaur Horns Assortment

Dinosaur Horns Assortment
Dinosaur Horns Assortment

Dinosaur Horns Assortment

These are nose horns from various Triceratops with perhaps a dermal scute from Ankylosaur in the front row that looks like Apollo 11 re-entry capsule.

Each horn has it’s story regarding how I found it, the “Eureka” moment, the rush of adrenaline. I have only prepped the rear one. As they were found, the remaining stay. Restoration occurred on the BIG horn in the rear. It was in 80 separate pieces when I found it.. Restored to “pretty cool” condition. I’ll post it later. The best one is the smallest on up front row. It’s an amazing fossil.

Paleontological Musings:

Triceratops horns are like cattle horns in that they take on many different shapes even within the same group. These are all from the same bone bed I call “Horn Sieve Beds” as they have given up over 30 of them to me.

Hell Creek/Lance Formations are the Cretaceous River Sands/muds is where the last of the dinosaurs hung out. Both formations cover our ranch. We span the MT/WY state line. There the Formations change names formally. Same rocks, different name.🤣

I got my masters degree around most things Paleo-Environmental……. I might have been one of the first Pale-environmentalist ever minted lolol. There is another that will read this I graduated with. Hi Dave!

So, paleo-topography when this dinosaur roamed was a broad equatorial coastal plain sloping like the piedmont of North Carolina east facing toward the then interior sea way stretching from the current Gulf of Mexico across the continent to Canada.

Location: Bliss Dinosaur Ranch, Wyoming/Montana borderlands (Wyotana)

Title: Dinosaur Horns Assortment

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Triceratops Dinosaur Rib Excavation

Triceratops Dinosaur Rib Excavation
Triceratops Dinosaur Rib Excavation

Triceratops Dinosaur Rib Excavation (Tough Long Read)

There might be a few words to google here. My apologies ⚒⚒⚒. Geology has it’s nomenclatural requirements. To put all this in the big picture is the tough part.

Our Ranch by coincidence 🤔 is located upon a 700 feet thickness of Sandstone. It has exposures of the famous Hell Creek/Lance Formation (Cretaceous Period) The Uppermost Cretaceous was a period of life on a coastal plain similar topographically to the piedmont of North Carolina. Locally the climate was pretty lush, warm and wet. Meandering Huge Rivers choked with Sand / silt worn off the rapidly eroding mountains to the (current) west. The land lay of different orientation that currently.

North America appears to have been rotated 90 degrees west of how it’s positioned currently. Located around the equator with plate tectonics moving/rotating the continent to it’s current position over the intervening 66 million years. T-rex, Triceratops, Duckbills, ankylosaurs, all those dinosaurs kids know the names of lived here. Here one died…

This is higher up rock section toward the top of the Hell Creek formation not long before the massive “Bolide” (google this) struck the earth. Chicxulub Mexico sits on that big impact area. punctuated the extinction process already underway at the end of the Cretaceous. Big 80 percent of all species Extinction events. Extinction ultimately is initiated by a populations inability to reproduce .

There was a pizza oven effect from the radiant heat from all that Bolide ejecta re-entering the atmosphere. That effect didn’t help anything that wasn’t underground or in the water (mammals) as 20 percent of species survived this age. There is a discussion that dinosaur and other groups were waining in density/diversity near the actual time of the Bolide ended the age of Dinosaurs. Dinosaurs as a group died off but avian dinosaurs did not. (Birds are dinosaurs more or less just short tail and teeth). Eventually the environmental effects killed off the food web in the ocean too. Bad time on the planet for most.

SO:

This sediment is called Bentonite. Wyoming sells LOTS of Bentonite. Cooking it turns it white. Lots of industrial uses. Dave Love (a famous Wyoming Geologist) famously wrote/said: “Wyoming is a wonderful State, we can sell our dirt”. 🤘👀⚒ Bentonite is a clay rich volcanic ash as this is a lake deposit. This rib belonged to an animal that floated into a body of water. Spreading of this carcass did occur and one rib bone excavated was vertical as someone stepped on it and pushed it into the mud on edge. I found a raptor tooth mixed in the mud with this 20 percent Triceratops carcass. (It was Dromeosaur richardoestesia )

Above the Triceratops rib is it’s upside down fragment of pelvis. Another rib hides in the upper right corner of the frame. This was one of the smaller ribs collected on a smaller Tric. The little bottles are full of thin superglue which we consume by the pint. We have the tip off the end of it …. A rib like this will come out in 30 pieces and reassembled back at the ranch headquarters.

Location: Bliss Dinosaur Ranch, Wyoming/Montana borderlands.

Title: Triceratops Dinosaur Rib Excavation

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Triceratops Toe “Phalanx” Fossil

Triceratops Toe "Phalanx" Fossil

Triceratops Toe “Phalanx” Fossil sees the first light of day in “Some Time” 😜

The latest Cretaceous Age here on the Bliss Dinosaur Ranch was a time of fine grained sediment accumulation deposited from huge rivers. These rivers were sweeping back and forth across the landscape choked by the sand and finer grained sediment load they carried. Sand sized material was the rule for these rivers ability/capacity to carry things down river. This Triceratops Toe “Phalanx” Fossil survived it’s transport from the distant past to the present under my gentle brush.

With the exception of isolated small scale deposits like this, the Hell Creek/Lance Formation is largely barren of fossils. In 5.5 square miles of HellCreek/Lance formation on my ranch, only about an acre can be called ‘fossilferous”. That acre is the total of 25 smaller locations (microsites) and a bone bed Triceratops Toe “Phalanx” Fossil sits here “In situ”. (In place in the undesturbed bedrock).

This fossil is positioned in the outcrop deeper than you might suspect. Your looking at a toe bone physiologically behind a claw/nail. it is 4 more inches deeper into the outcrop so this is the top 2 inches of the bone exposed. Triceratops had big toes lolol. It’s deeper than it is long. I like to take photos of fossils in the outcrop as it’s sort of the “Eureka”/adrenaline rush moment.

Geologic Musings on this ranches “Dirt”:

Geologists consider the Cretaceous to have ended 66 million years ago. This toe bone has literally not seen the light of day in that unfathomable period of time. The sediment it is in, is a mix of sand, clay with chunky chunks (up to 2 feet) of torn up river bottom clays. The ripped up chunks of clay were rounded by bounding down a river/transport. There is a 2 foot thick or so blue clay pure of any fossil or other detritus directly under this 3 foot thick channel. That above that clay is a channel packed with chunks of clay/mud from upstream. . A mix of at least 3 different mud chunks from various sources nearby. I’ve seen chunks of mud angular like they got torn up 50 feet up stream. So this is a “channel” I’ve been following that tapers on either side that filled up with ripped up chunks of upstream river bottom mixed with a variety of bones from who ever was walking around at the time.

The bones were dropped here for me to find because the river waters slowed enough in this location to drop them out of suspension here mixed in among chunks of mud. The spaces between the “Cobbles of mud” are filled with sandy material that “Sifted in” from the flowing water. This is classic river sedimentation/deposit stuff. That is where you find the little fossils too. Sands mixed with smaller rounded pebbles of river bottom clay. It’s all part of the “Bed load” of a river and what is in it depends on river current velocity… (followed by a really long discussion lolol). IF the river is fast enough to move

Location: Bliss Dinoaur Ranch, Wyoming/Montana.

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Triceratops Vertebra with Processes

Triceratops Vertebra with Processes
Triceratops Vertebra with Processes

While finding a Cretaceous age Triceratops Vertebra with Processes still attached is possible, it doesn’t happen very often with an isolated fossil not attached to another bone.

Geologic Musings:

I spent many years working on determining paleo-environments. It the environment of deposition that produced rock deposits. This can be determined from any number of clues left in the rocks. (Wrote a Masters thesis on this). I am biostratigraphically and sedimentologically very aware of how this Triceratops vertebra with processes got to be here…cer. There are many indications to what was going on during it’s deposition. This Bentonitic Clay rich Mud was on the edge of a lake. This deposit consisted of what was then Volcanic Ash as a “dump” was washed into the lake hydraulically. That washed in volcanic “mud” made a “deltaic” intrusion into the much larger lake.

This particular bed of sediment I have traced over about 2 square miles. I loose visual on the bed as it disappears either underground or has been removed by erosion. So this was a pretty big lake and a big delta deposit into that lake. Represented is not a high energy Splay deposit that might exist next to a big natural river levy (highest things on the landscape probably). It’s not high energy like a splay proven from the lack of larger chunks of plant matter….

There were BIG rivers sweeping back then. Sweeping back and forth carrying LOTS of sand during this time in Wyoming/Montana. The sand was mixed along with this finer material (clays) by the boat load and dumping it. Low energy let the fine clays settle out (like in lakes). Otherwise the clays (size term just like sand) would stay in suspension in agitated water. This had to be a calm environment like a lake. Most of my Hell Creek Fossils are found in RIver NOT lake deposits by the way lol.

Considerations:

That volcanic ash was altered over the 66 million intervening years into “Bentonite” which is an incomplete description of the sediment. Bentonite is just ONE Clay mineral that is represented here. Dozens of clay minerals are in this mix. Digging in this stuff is like pushing a wood awl through very thick hard modeling clay. Sometimes you can get it in a few inches, others just a quarter of an inch. You stick and pluck the awl and slowly clear off sediment to facilitate this treasures removal. It’s all very moist and most of the fossils have a white crust around them. They usually clean up beautifully brown.

Overview

Maybe 20 percent of this Triceratops was recovered nearby this isolated Triceratops vertebra with processes. We finally all gave up looking for more of the carcass. It could be 1 inch down and we wouldn’t know it lolol. It’s bones were obviously scattered/fed on and stepped on after it floated into the lake at least once. I noted that ALMOST all the bone fossils in this deposit were laying flat horizontal to the lake bottom. One rib was obviously stepped on as it was broken in half with 1/2 of it being vertical. It was pushed down into the mud by someone walking over. I’ve found coprolites (fossil poop) here too. This would be indicating that active feeding and pooping was happening for a while. Also found a smaller raptor tooth in the mix. (Dromaeosaur richaroestacia. (sic).

The soft organic rich mud covering the fossil was rich in small fragments macerated plant matter. This is an obvious lake deposit covering several square miles at a minimum. The energy was very low here. Calm water, no doubt shallow as the wading dinosaurs confirm. There was not a lot of topography on the Hell Creek Formations mostly sandy river deposits on a broad sweeping plane. Much of a rib cage was recovered along with a scapula and several other very nice fossils from this animal. I found this site by tracing a big chunk of Triceratops Brow Horn back up hill to where it came from. Took a few looks lol.

Location: Bliss DInosaur Ranch, Wyoming/Montana borderlands.

Triceratops Vertebra with Processes