Charles Mound. Elevation 1,235 ft., located in Jo Daviess County.
March 4, 1837 from Jo Daviess County. It was named for Col. Benjamin Stephenson.
The Tully Monster was designated as the State Fossil in 1989.
The Tully Monster (Tullimonstrum gregarium) was a soft bodied animal. It preserves as outlines and flattened forms in nodules of ironstone from several areas in Illinois. It lived in the ocean that covered much of Illinois during the Pennsylvanian Period (about 300 million years ago). It was probably an active, swimming carnivore.
The flexible body was probably round or oval in cross section. It may have been segmented, but some recent work suggests that it was not. The tail had horizonal fins and a dorsal fin; all three of these fins were triangular.
The Tully Monster had a long proboscis. At the end was a "jaw" that contained eight small, sharp teeth. There is no evidence that the throat went down the proboscis. It seems more likely that the proboscis was a muscular organ used to pass food to the mouth.
Near the middle of the body was a transverse bar the passed through the body. This bar had swellings on the end. These may have been the animal's sensory organ.
Scientists do not know to what other animals the Tully Monster is related. Some scientists have speculated that it is related to snails and other molluscs.
The Tully Monster was first found by Mr. Francis Tully in 1958. He took the specimen to the Field Museum of Natural History in Chicago. The specimen defied identification and became known as the "Tully Monster." The name stuck. When Dr. Eugene Richardson formally described the new animal, he gave it the name Tullimonstrum gregarium.
The species name gregarium means common. This refers to the fact that Tully Monsters are fairly common fossils in the Mazon Creek deposits. More recently they have also been found in open-pit coal mines in central Illinois.
The Mazon Creek deposits are located in Will and Grundy Counties. They are some of the most important fossil deposits in North America because the soft parts of many organisms are preserved. The deposits contain the remains of both plants and animals. Some of the organisms lived in the ocean; others were washed in from the nearby shore. The material is preserved in concretions of ironstone.
Illinois Blue Book 1993-1994
Jo Daviess; Carroll; Ogle; Winnebago, in Illinois, and Lafayette; Green and a tiny corner of Rock in Wisconsin.
1) Mississippi Valley via St. Louis and Galena by steamer and by wagon.
2) The lake route from upper New York state and New England, via the Erie Canal and Chicago.
3) Overland from Pennsylvania by wagon and railroad. After 1853 by railroad west from Chicago.