UW-Madison Geology Museum
Encyclopedia
The UW–Madison Geology Museum (UWGM) is a geology and paleontology museum housed in Weeks Hall, in the southwest part of the University of Wisconsin–Madison
campus. The museum's main undertakings are exhibits, outreach to the public, and research. It has the second highest attendance of any museum at the University of Wisconsin–Madison
, exceeded only by the Chazen Museum of Art
. The museum charges no admission.
. After the construction of Weeks Hall in the 1970s, the museum moved to its present location in 1981.
Highlights of the museum include:
The museum hosts periodic family events, such as the annual Open House. These sometimes have a special theme, such as the one in 2006 that focused on pterosaur
s and in 2009 on the Mazon Creek fossils
which includes the Tully Monster (Tullimonstrum gregarium).
Formation in Kansas has yielded many marine fossils. The Hell Creek Formation
in Montana
and South Dakota
has produced duck-billed
, horned, and tyrannosaurid dinosaurs, as well as some noteworthy fish.
There is an ongoing summer dig in the Jurassic
Morrison Formation
in Wyoming
, which has produced sauropod and theropod dinosaurs, as well as other remarkable vertebrates.
The museum also conducts local research, such as the study of Pleistocene
mammal
fossils from Midwestern caves.
The museum's fossils include impressive collections from the White River Badlands, the Santana Formation of Brazil, a remarkable Silurian
soft-bodied fauna from a quarry near Waukesha
.
University of Wisconsin–Madison
The University of Wisconsin–Madison is a public research university located in Madison, Wisconsin, United States. Founded in 1848, UW–Madison is the flagship campus of the University of Wisconsin System. It became a land-grant institution in 1866...
campus. The museum's main undertakings are exhibits, outreach to the public, and research. It has the second highest attendance of any museum at the University of Wisconsin–Madison
University of Wisconsin–Madison
The University of Wisconsin–Madison is a public research university located in Madison, Wisconsin, United States. Founded in 1848, UW–Madison is the flagship campus of the University of Wisconsin System. It became a land-grant institution in 1866...
, exceeded only by the Chazen Museum of Art
Chazen Museum of Art
The Chazen Museum of Art is an art museum accredited by the American Association of Museums located at the University of Wisconsin–Madison in Madison, Wisconsin. It was known as the Elvehjem Museum of Art until 2005...
. The museum charges no admission.
History
The museum was founded in the 19th century, and for many years resided with the earth science departments in Science HallUniversity of Wisconsin Science Hall
University of Wisconsin Science Hall is a building on the campus of the University of Wisconsin–Madison. It is significant for its association with Charles R. Van Hise, "who led the Department of Mineralogy and Geology to national prominence" and then served as president of the university. The...
. After the construction of Weeks Hall in the 1970s, the museum moved to its present location in 1981.
Exhibits
Almost 1,000 items are on display in 66 exhibits covering 3000 square feet (278.7 m²). Major sections are devoted to rocks and minerals, invertebrate and fish fossils, and vertebrate fossils. There are also cases of glaciers, meteorites, and fossil plants.Highlights of the museum include:
Rocks
- An excellent specimen of the mineral kermesiteKermesiteKermesite or antimony oxysulfide is also known as red antimony . The mineral’s color ranges from cherry red to a dark red to a black. Kermesite is the result of partial oxidation between stibnite and other antimony oxides such as valentinite or stibiconite...
; - Two glacial erraticGlacial erraticA glacial erratic is a piece of rock that differs from the size and type of rock native to the area in which it rests. "Erratics" take their name from the Latin word errare, and are carried by glacial ice, often over distances of hundreds of kilometres...
pieces of copperCopperCopper is a chemical element with the symbol Cu and atomic number 29. It is a ductile metal with very high thermal and electrical conductivity. Pure copper is soft and malleable; an exposed surface has a reddish-orange tarnish...
weighing hundreds of pounds each; - A case exhibiting 85 mineralMineralA mineral is a naturally occurring solid chemical substance formed through biogeochemical processes, having characteristic chemical composition, highly ordered atomic structure, and specific physical properties. By comparison, a rock is an aggregate of minerals and/or mineraloids and does not...
s from the recent Greiner donation; - A blacklight room that shines both long- and short-wave ultravioletUltravioletUltraviolet light is electromagnetic radiation with a wavelength shorter than that of visible light, but longer than X-rays, in the range 10 nm to 400 nm, and energies from 3 eV to 124 eV...
onto rocks, demonstrating fluorescenceFluorescenceFluorescence is the emission of light by a substance that has absorbed light or other electromagnetic radiation of a different wavelength. It is a form of luminescence. In most cases, emitted light has a longer wavelength, and therefore lower energy, than the absorbed radiation...
and phosphorescencePhosphorescencePhosphorescence is a specific type of photoluminescence related to fluorescence. Unlike fluorescence, a phosphorescent material does not immediately re-emit the radiation it absorbs. The slower time scales of the re-emission are associated with "forbidden" energy state transitions in quantum...
; - A walk-through model of a limestoneLimestoneLimestone is a sedimentary rock composed largely of the minerals calcite and aragonite, which are different crystal forms of calcium carbonate . Many limestones are composed from skeletal fragments of marine organisms such as coral or foraminifera....
cave, complete with sound effects.
Fossils
- Several stromatoliteStromatoliteStromatolites or stromatoliths are layered accretionary structures formed in shallow water by the trapping, binding and cementation of sedimentary grains by biofilms of microorganisms, especially cyanobacteria ....
s from the OrdovicianOrdovicianThe Ordovician is a geologic period and system, the second of six of the Paleozoic Era, and covers the time between 488.3±1.7 to 443.7±1.5 million years ago . It follows the Cambrian Period and is followed by the Silurian Period...
of southwestern WisconsinWisconsinWisconsin is a U.S. state located in the north-central United States and is part of the Midwest. It is bordered by Minnesota to the west, Iowa to the southwest, Illinois to the south, Lake Michigan to the east, Michigan to the northeast, and Lake Superior to the north. Wisconsin's capital is...
; - A slab of sea floor from the CretaceousCretaceousThe Cretaceous , derived from the Latin "creta" , usually abbreviated K for its German translation Kreide , is a geologic period and system from circa to million years ago. In the geologic timescale, the Cretaceous follows the Jurassic period and is followed by the Paleogene period of the...
period in TexasTexasTexas is the second largest U.S. state by both area and population, and the largest state by area in the contiguous United States.The name, based on the Caddo word "Tejas" meaning "friends" or "allies", was applied by the Spanish to the Caddo themselves and to the region of their settlement in...
, containing impressions of many clams; - Shells of giant the cephalopodCephalopodA cephalopod is any member of the molluscan class Cephalopoda . These exclusively marine animals are characterized by bilateral body symmetry, a prominent head, and a set of arms or tentacles modified from the primitive molluscan foot...
EndocerasEndocerasEndocerida is an extinct nautiloid order, a group of cephalopods from the Lower Paleozoic with cone-like deposits in its siphuncle.Endocerida comprises a diverse group of cephalopods that lived from the Early Ordovician possibly to the Late Silurian . Their shells varied in form...
from Wisconsin; - The type specimenBiological typeIn biology, a type is one particular specimen of an organism to which the scientific name of that organism is formally attached...
of the fossil cephalopodCephalopodA cephalopod is any member of the molluscan class Cephalopoda . These exclusively marine animals are characterized by bilateral body symmetry, a prominent head, and a set of arms or tentacles modified from the primitive molluscan foot...
ActinocerasActinocerasActinoceras is the principal and root genus of the Actinoceratidae, a major family in the Actinocerida, that lived during the Middle and Late Ordovician.- Morphology:...
beloitense. - A window showing the workings of the preparation laboratory, where vertebrateVertebrateVertebrates are animals that are members of the subphylum Vertebrata . Vertebrates are the largest group of chordates, with currently about 58,000 species described. Vertebrates include the jawless fishes, bony fishes, sharks and rays, amphibians, reptiles, mammals, and birds...
fossils collected in the field are cleaned for storage or display; - Animals from the Burgess ShaleBurgess ShaleThe Burgess Shale Formation, located in the Canadian Rockies of British Columbia, is one of the world's most celebrated fossil fields, and the best of its kind. It is famous for the exceptional preservation of the soft parts of its fossils...
, including the chordateChordateChordates are animals which are either vertebrates or one of several closely related invertebrates. They are united by having, for at least some period of their life cycle, a notochord, a hollow dorsal nerve cord, pharyngeal slits, an endostyle, and a post-anal tail...
PikaiaPikaiaPikaia gracilens is an extinct animal known from the Middle Cambrian Burgess Shale of British Columbia. -Discovery:It was discovered by Charles Walcott and was first described by him in 1911. It was named after Pika Peak, a mountain in Alberta, Canada. Based on the obvious and regular segmentation...
, the hyolith HaplophrentisHaplophrentisHaplophrentis was a tiny shelled hyolithid which lived in the Cambrian Period. Its shell was long and conical, with the open end protected by an operculum, from which two fleshy arms called helens protruded at the sides...
, and fragments of the stem-arthropodArthropodAn arthropod is an invertebrate animal having an exoskeleton , a segmented body, and jointed appendages. Arthropods are members of the phylum Arthropoda , and include the insects, arachnids, crustaceans, and others...
AnomalocarisAnomalocarisAnomalocaris is an extinct genus of anomalocaridid, which are, in turn, thought to be closely related to the arthropods. The first fossils of Anomalocaris were discovered in the Ogygopsis Shale by Joseph Frederick Whiteaves, with more examples found by Charles Doolittle Walcott in the famed...
; - Several skeletons from the CretaceousCretaceousThe Cretaceous , derived from the Latin "creta" , usually abbreviated K for its German translation Kreide , is a geologic period and system from circa to million years ago. In the geologic timescale, the Cretaceous follows the Jurassic period and is followed by the Paleogene period of the...
NiobraraNiobrara FormationThe Niobrara Formation, also called the Niobrara Chalk , is a geologic formation in North America that was laid down between 87 and 82 million years ago during the Coniacian, Santonian, and Campanian ages of the Late Cretaceous. It is composed of two structural units, the Smoky Hill Chalk Member...
chalk of KansasKansasKansas is a US state located in the Midwestern United States. It is named after the Kansas River which flows through it, which in turn was named after the Kansa Native American tribe, which inhabited the area. The tribe's name is often said to mean "people of the wind" or "people of the south...
:- HesperornisHesperornisHesperornis is a genus of flightless aquatic birds that spanned the first half of the Campanian age of the Late Cretaceous period . One of the lesser-known discoveries of the paleontologist O. C. Marsh in the late 19th century Bone Wars, it was an important early find in the history of avian...
, a swimming bird with teeth; - A slab of chalk containing the sharkSharkSharks are a type of fish with a full cartilaginous skeleton and a highly streamlined body. The earliest known sharks date from more than 420 million years ago....
SqualicoraxSqualicoraxSqualicorax is a genus of extinct lamniform shark known to have lived during the Cretaceous period. A fully articulated 1.9 m long fossil skeleton of Squalicorax has been found in Kansas, evidence of its presence in the Western Interior Seaway...
, including its teeth, vertebrae, and some bones from its last meal; - An exceptionally well-preserved slab of a floating colony of the sea lilyCrinoidCrinoids are marine animals that make up the class Crinoidea of the echinoderms . Crinoidea comes from the Greek word krinon, "a lily", and eidos, "form". They live both in shallow water and in depths as great as 6,000 meters. Sea lilies refer to the crinoids which, in their adult form, are...
Uintacrinus; - A nearly complete skeleton of the mosasaurMosasaurMosasaurs are large extinct marine lizards. The first fossil remains were discovered in a limestone quarry at Maastricht on the Meuse in 1764...
Platycarpus, suspended from the ceiling. It has some distinctive pathologiesPathologyPathology is the precise study and diagnosis of disease. The word pathology is from Ancient Greek , pathos, "feeling, suffering"; and , -logia, "the study of". Pathologization, to pathologize, refers to the process of defining a condition or behavior as pathological, e.g. pathological gambling....
, including injured ribs and a rear right flipper with arthritis; - A suspended replica of the pterosaurPterosaurPterosaurs were flying reptiles of the clade or order Pterosauria. They existed from the late Triassic to the end of the Cretaceous Period . Pterosaurs are the earliest vertebrates known to have evolved powered flight...
PteranodonPteranodonPteranodon , from the Late Cretaceous geological period of North America in present day Kansas, Alabama, Nebraska, Wyoming, and South Dakota, was one of the largest pterosaur genera and had a maximum wingspan of over...
;
- Hesperornis
- Vertebrate skeletons from other places:
- The PermianPermianThe PermianThe term "Permian" was introduced into geology in 1841 by Sir Sir R. I. Murchison, president of the Geological Society of London, who identified typical strata in extensive Russian explorations undertaken with Edouard de Verneuil; Murchison asserted in 1841 that he named his "Permian...
reptile CaptorhinusCaptorhinusCaptorhinus is an extinct genus of Captorhinidae that lived in the Permian. Its remains are known from North America. An immature specimen of Captorhinus was originally named Bayloria, and classified as a member of the synapsid group Eothyrididae.-Species:1. Captorhinus aguti = C. isolomus = C....
; - A composite skeleton of the duck-billed dinosaurHadrosauridHadrosaurids or duck-billed dinosaurs are members of the family Hadrosauridae, and include ornithopods such as Edmontosaurus and Parasaurolophus. They were common herbivores in the Upper Cretaceous Period of what are now Asia, Europe and North America. They are descendants of the Upper...
EdmontosaurusEdmontosaurusEdmontosaurus is a genus of crestless hadrosaurid dinosaur. It contains two species: Edmontosaurus regalis and Edmontosaurus annectens. Fossils of E. regalis have been found in rocks of western North America that date from the late Campanian stage of the Cretaceous Period 73 million years ago,...
, the first dinosaur on display in Wisconsin; - The Boaz mastodonBoaz mastodonThe Boaz mastodon is the skeleton of a mastodon found near Boaz, Wisconsin in 1897. A fluted quartzite spear point found near the Boaz mastodon suggests that humans hunted mastodons in southwestern Wisconsin.-History:...
, a PleistocenePleistoceneThe Pleistocene is the epoch from 2,588,000 to 11,700 years BP that spans the world's recent period of repeated glaciations. The name pleistocene is derived from the Greek and ....
relative of elephants found in 1897 on a farm in southwestern Wisconsin near the village of BoazBoaz, WisconsinBoaz is a village in Richland County, Wisconsin, United States. The population was 137 at the 2000 census.-Geography:Boaz is located at ....
.
- The Permian
Extraterrestrial exhibits
- A large fragment of the Canyon Diablo meteorite that left Meteor CraterMeteor CraterMeteor Crater is a meteorite impact crater located approximately east of Flagstaff, near Winslow in the northern Arizona desert of the United States. Because the US Department of the Interior Division of Names commonly recognizes names of natural features derived from the nearest post office, the...
in Arizona. - Several small meteorites, both stony and metallic, that fell in Wisconsin.
Outreach
Every year hundreds of school groups from around the state tour the museum, led by student guides. Staff and students at the museum also travel to schools in the area to teach children and their teachers about geology.The museum hosts periodic family events, such as the annual Open House. These sometimes have a special theme, such as the one in 2006 that focused on pterosaur
Pterosaur
Pterosaurs were flying reptiles of the clade or order Pterosauria. They existed from the late Triassic to the end of the Cretaceous Period . Pterosaurs are the earliest vertebrates known to have evolved powered flight...
s and in 2009 on the Mazon Creek fossils
Mazon Creek fossils
The Mazon Creek fossil beds are a conservation found near Morris, in Grundy County, Illinois. The fossil beds are located in ironstone concretions, formed approximately in the mid-Pennsylvanian epoch of the Carboniferous period...
which includes the Tully Monster (Tullimonstrum gregarium).
Research
The museum has conducted fossil digs in many Western states. The Late Cretaceous NiobraraNiobrara Formation
The Niobrara Formation, also called the Niobrara Chalk , is a geologic formation in North America that was laid down between 87 and 82 million years ago during the Coniacian, Santonian, and Campanian ages of the Late Cretaceous. It is composed of two structural units, the Smoky Hill Chalk Member...
Formation in Kansas has yielded many marine fossils. The Hell Creek Formation
Hell Creek Formation
The Hell Creek Formation is an intensely-studied division of Upper Cretaceous to lower Paleocene rocks in North America, named for exposures studied along Hell Creek, near Jordan, Montana...
in Montana
Montana
Montana is a state in the Western United States. The western third of Montana contains numerous mountain ranges. Smaller, "island ranges" are found in the central third of the state, for a total of 77 named ranges of the Rocky Mountains. This geographical fact is reflected in the state's name,...
and South Dakota
South Dakota
South Dakota is a state located in the Midwestern region of the United States. It is named after the Lakota and Dakota Sioux American Indian tribes. Once a part of Dakota Territory, South Dakota became a state on November 2, 1889. The state has an area of and an estimated population of just over...
has produced duck-billed
Hadrosaurid
Hadrosaurids or duck-billed dinosaurs are members of the family Hadrosauridae, and include ornithopods such as Edmontosaurus and Parasaurolophus. They were common herbivores in the Upper Cretaceous Period of what are now Asia, Europe and North America. They are descendants of the Upper...
, horned, and tyrannosaurid dinosaurs, as well as some noteworthy fish.
There is an ongoing summer dig in the Jurassic
Jurassic
The Jurassic is a geologic period and system that extends from about Mya to Mya, that is, from the end of the Triassic to the beginning of the Cretaceous. The Jurassic constitutes the middle period of the Mesozoic era, also known as the age of reptiles. The start of the period is marked by...
Morrison Formation
Morrison Formation
The Morrison Formation is a distinctive sequence of Late Jurassic sedimentary rock that is found in the western United States, which has been the most fertile source of dinosaur fossils in North America. It is composed of mudstone, sandstone, siltstone and limestone and is light grey, greenish...
in Wyoming
Wyoming
Wyoming is a state in the mountain region of the Western United States. The western two thirds of the state is covered mostly with the mountain ranges and rangelands in the foothills of the Eastern Rocky Mountains, while the eastern third of the state is high elevation prairie known as the High...
, which has produced sauropod and theropod dinosaurs, as well as other remarkable vertebrates.
The museum also conducts local research, such as the study of Pleistocene
Pleistocene
The Pleistocene is the epoch from 2,588,000 to 11,700 years BP that spans the world's recent period of repeated glaciations. The name pleistocene is derived from the Greek and ....
mammal
Mammal
Mammals are members of a class of air-breathing vertebrate animals characterised by the possession of endothermy, hair, three middle ear bones, and mammary glands functional in mothers with young...
fossils from Midwestern caves.
Collections
Like most museums, the Geology Museum has far more specimens stored in its collections than on display. It holds a majority of the meteorites ever collected in Wisconsin, and an abundance of rocks and minerals collected by faculty and donated by friends of the museum.The museum's fossils include impressive collections from the White River Badlands, the Santana Formation of Brazil, a remarkable Silurian
Silurian
The Silurian is a geologic period and system that extends from the end of the Ordovician Period, about 443.7 ± 1.5 Mya , to the beginning of the Devonian Period, about 416.0 ± 2.8 Mya . As with other geologic periods, the rock beds that define the period's start and end are well identified, but the...
soft-bodied fauna from a quarry near Waukesha
Waukesha, Wisconsin
Waukesha is a city in and the county seat of Waukesha County, Wisconsin, in the Upper Midwest region of the United States. The population was 70,718 at the 2010 census, making it the largest community in the county and 7th largest in the state. The city is located adjacent to the Town of Waukesha...
.