As July progressed into August and we neared the end of our field season, it was time to start hauling blocks back to camp and closing down quarries. This is Suicide Hill, a spot I didn’t work at very much but which contains lots of juvenile Eolambia. Lindsay has a great system for bringing large blocks back to camp with people-power only, since we cannot use vehicles at many of our sites. We strap them with ratchet straps to a backboard (or what everyone else was calling a sled, but it’s a backboard guys! We were totally prepared for spinal injuries!). This way, 4-8 people can lift large jackets with relative ease and less potential for back injury. I think this jacket was somewhere over 500 pounds.
Elsewhere in the Mesozoic, parts of the field crew were working away at Cretaceous dinosaurs in the Mussentuchit Member of the Cedar Mountain Formation. In may we worked at Crystal Geyser Quarry, which is in the Yellow Cat Member of the same formation and is about 125 million years old, in a part of the Cretaceous called the Barremian. In contrast, the Mussentuchit Member is about 98 million years old, or Cenomanian in age. The Cedar Mountain Formation is a giant unit of rock, and the dinosaur faunas changed dramatically throughout!
I can’t believe that it’s been more than 2 months since we got back from our fieldwork in Utah and I’m only getting around to posting about it now, but I guess that means things have been hopping around here! We had spent a week at the Crystal Geyser Quarry earlier in May, but our main batch of fieldwork lasted for four weeks from mid July to mid August. We drove from North Carolina to near Emery, Utah, to set up camp and work in the Morrison and Cedar Mountain formations.
Camp was comfortable and cozy!
And there were some pretty nice views!