MUSEUM
INFORMATION

MECHANICAL HALL

30 North College Ave.
Newark, DE 19716

Hours:
Wed-Sun 12:00-5:00 pm
Thur - 12:00-8:00 pm
Closed during University breaks and holidays

Directions

Parking:
Parking for the Mechanical Hall Gallery is in Trabant University Center Garage located between Delaware Avenue and Main St.

Phone:
302-831-8037 or
302-831-8088

MINERALOGICAL MUSEUM

255 Academy St.
Newark, DE 19716

Hours:
Wed-Sun 12:00-5:00 pm
Thur - 12:00-8:00 pm
Closed during University breaks and holidays

Directions

Parking:
Parking for the Mineralogical Museum is in Perkins Garage located on Academy Street.

Phone:
302-831-6557 or
302-831-8037 or
302-831-4840

OLD COLLEGE GALLERY

18 East Main St.
Newark, DE 19716

Hours:
Wed-Sun 12:00-5:00 pm
Thur - 12:00-8:00 pm
Closed during University breaks and holidays

Directions

Parking:
Parking for the Old College Gallery is in Trabant University Center Garage located between Delaware Avenue and Main St.

Phone:
302-831-8037 or
302-831-6589

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MINERALOGICAL MUSEUM


China Exhibit

September 8-December 5, 2010

Although the Mineralogical Museum was founded with the gift of the collection of Irenee du Pont, Sr., it has grown to encompass specimens gifted or made possible by many generous donors, including Mrs. David Craven, Alvin B. Stiles and Frederick Keidel. Because of our intimate space, we have chosen to focus on individual displays that illustrate particular mineralogical concepts or themes. These include gem minerals from the du Pont collection mined in the early 20th century, as well as more recent finds of minerals from North America. Newly installed display cabinets with fiber optic lighting provide accurate color balance for specimens from the wire silvers to the vivid orange wulfenites.

Among the exhibits in the Museum, you will see:

Rhodochrosite: Santa Isabella Vein, Huallapon Mine, Pasto Bueno, Peru (9 cm x 6 cm x 3.75 cm)

Irenee du Pont Exhibit

The minerals exhibited here are from the collection of Irenee du Pont, Sr. (1876 – 1963), whose collection was gifted to the University of Delaware in 1964. Du Pont purchased much of his collection from George Kunz, Vice-President of Tiffany & Co., in 1919. This display emphasizes minerals from extinct localities – deposits that have been mined out or even mines that have vanished into later open pit mining operations.

Two boxes of tourmaline crystals are part of a set of four fitted boxes with specimens from the Himalaya Mine, San Diego County, California, acquired from Kunz. The Himalaya Mine opened in 1898 and was the world’s largest producer of tourmalines, largely exported to China for carving as snuff bottles and other small objects.

The lead and bismuth specimens in this display are important rarities, as these elements are almost always found in combination with other elements in minerals and not in their native states.

Crystal System Exhibit

All minerals are crystalline, with orderly and repeating arrangements of atoms. Growth occurs by the addition of atoms to the arrangement. If growth takes place in an open space or in soft material, a crystal, reflecting the internal atomic arrangement may form. Although ideal crystals are perfect shapes, many actual crystals are distorted due to variations in growth over time.

Although, there are enormous variations in crystal shapes, they can all be grouped into six crystal systems based on the geometry of the internal structure.

Minerals From Caves Exhibit

Almost all caves are limestone, with light- colored white to beige stalactites and stalagmites. Other unique cave deposits include vivid pink rhodochrosite stalactities in Argentina, deep green banded malachite formations in Republic of Congo and exotic specimens such as this goethite from Spain.

Pseudomorphs and other Growth Phenomena

A pseudomorph is a “false form” – one mineral adopting the shape of another; the second mineral is said to be a pseudomorph after the first. Pseudomorphs may be formed in different ways;

• A mineral formed under certain conditions may change to another, chemically similar mineral with a different atomic arrangement, if the conditions change. The illustrated hematite is an example of this type

• A mineral may be replaced by another that has such a great chemical difference that it is considered a replacement pseudomorph

• A mineral may coat another, preserving the original shape and forming an encrustation pseudomorph. All of these are illustrated by specimens on exhibition.

Crystals may also deviate from their ideal shapes because of internal defects in atomic arrangement or because of the manner in which the atoms have been bonded to the surfaces of crystal faces during growth. Elongated or twisted crystals sometimes result from these arrangements.

  • University of Delaware   •   Newark, DE 19716   •   USA
    Phone: (302) 831-2792   •   © 2011