🍂 HAPPY NOVEMBER, EXPLORERS!
Join us at Moab Giants for a prehistoric adventure filled with life-sized dinosaurs, interactive discoveries, and unforgettable family fun.
🦖 NOVEMBER SPECIAL: 15% OFF!
Use code DINOVEMBER15 when you buy tickets online.
Valid through November 30.
🕒 NOVEMBER OPENING HOURS
Open: Thursday–Monday
Closed: Tuesdays & Wednesdays
Hours: 10:00 AM – 5:00 PM
🎟 Last Admission: 4:00 PM
🦃 CLOSED THANKSGIVING DAY
We’ll be closed on Thursday, November 26, so our team can celebrate with their families. We’ll reopen Friday, November 27, at 10:00 AM. Happy Thanksgiving!
Bring the whole family for a day of discovery and excitement in Utah’s dinosaur country. We can’t wait to welcome you on your prehistoric adventure!
📲 Follow @moabgiants for the latest updates, special events, and more.
[ BOOK NOW & SAVE 15% ]
Diet : Herbivorous
Habitat : Forests
Length : 26 feet (8 meters)
Weight : Up to 7,000 lbs (3.2 tons)
Caririchnium “means track from a region called Carir” in Brazil. This track was probably made by the dinosaur Iguanodon. Trackers also use the name Iguanodontipus meaning “Iguanodon track” for similar footprints. Iguanodon and its tracks are best known from Europe, Asia and North America. In the Moab area Iguanodon remains are known from the Cedar Mountain Formation and it is fairly certain that this type of trackmaker made Caririchnium tracks from the same formation at the Mill Canyon tracksite.
Iguanodon was the second dinosaur ever named, in 1825. It was found in England in the same deposits as footprints it was thought to have made. Iguanodon has since been found in the USA and other areas, with the same type of tracks. Skeletal remains named Iguanodon ottingeri from the Moab area are named in honor of the famous Moab Rock Shop owner Lin Ottinger. In the 19th century Iguanodon was imagined to be a ponderous lizard with a horn on its nose, but the supposed horn turned out to be a spiky thumb. Iguanodon was a very common, large herbivore in the Early Cretaceous, and Caririchnium is one of the most widely known tracks found in rocks of this age.