Name/Title
CalciteEntry/Object ID
78.63.45Description
Chemical Composition: CaCO3
Crystal System: Hexagonal System
Description: Common Name: Calcite (Rhomb)
Group Name: Calcite
Chemistry: CaCO3
Location: Canada
Description: Delmar describes this as a: A clevage "Rhomb" of calcite, characterized by the double image it produces when placed in front of an object, called "iceland spar" or optical calcite. This form of calcite was used for bombadier peep sites during WW2, and it was mined for this purpose. It is also used as a polarizing medium.
PHYSICAL CHARACTERISTICS:
•Color is extremely variable but generally white or colorless or with light shades of yellow, orange, blue, pink, red, brown, green, black and gray. Occasionally iridescent.
•Luster is vitreous to resinous to dull in massive forms.
•Transparency: Crystals are transparent to translucent.
•Crystal System is trigonal; bar 3 2/m
•Crystal Habits are extremely variable with almost any trigonal form possible. Common among calcite crystals are the scalenohedron, rhombohedron, hexagonal prism, and pinacoid. Combinations of these and over three hundred other forms can make a multitude of crystal shapes, but always trigonal or pseudo-hexagonal. Twinning is often seen and results in crystals with blocky chevrons, right angled prisms, heart shapes or dipyramidal shapes. A notch in the middle of a doubly terminated scalenohedron is a sure sign of a twinned crystal. lamellar twinning also seen resulting in striated cleavage surfaces. Pseudomorphs after many minerals are known, but easily identified as calcite. Also massive, fibrous, concretionary, stalactitic, nodular, oolitic, stellate, dendritic, granular, layered, etc. etc.
•Cleavage is perfect in three directions, forming rhombohedrons.
•Fracture is conchoidal.
•Hardness is 3 (only on the basal pinacoidal faces, calcite has a hardness of less than 2.5 and can be scratched by a fingernail).
•Specific Gravity is approximately 2.7 (average)
•Streak is white.
•Other Characteristics: refractive indices of 1.49 and 1.66 causing a significant double refraction effect (when a clear crystal is placed on a single line, two lines can then be observed), effervesces easily with dilute acids and may be fluorescent, phosphorescent, thermoluminescence and triboluminescent.
•Associated Minerals are numerous but include these classic associations: Fluorite, quartz, barite, sphalerite, galena, celestite, sulfur, gold, copper, emerald, apatite, biotite, zeolites, several metal sulfides, other carbonates and borates and many other minerals.
•Notable Occurrences include Pugh Quarry, Ohio; Rosiclare, Illinois; Franklin, New Jersey; Elmwood, Tennessee; Brush Creek and other Missouri, Wisconsin, Kansas and Oklahoma localities, USA; Andreasburg, Harz Mountains and Saxony, Germany; Brazil; Guanajuato, Mexico; Cornwall, Durham and Lancashire, England; Bombay area of India; Eskifjord, Iceland; many African localities as well as others around the world with their own unique varieties.
•Best Field Indicators are crystal habit, reaction to acid, abundance, hardness, double refraction and especially cleavage.
Fracture: conchoidal
Hardness: 3 Calcite
Luster: Vitreous
Rock Type: Sedimentary
Specific Gravity: 2.7
Streak: whiteCollection
Delmar Smith Mineral CollectionAcquisition
Accession
78.63Source or Donor
Delmar Smith Crystal CollectionAcquisition Method
DonationDimensions
Width
4-3/8 inDepth
1-1/8 inLength
4-1/8 inDimension Notes
Dimension taken at widest pointsLocation
Location
Display Case
FS-6-ARoom
Frieda Smith HallBuilding
Crater Rock MuseumDate
January 3, 2024Location
Container
Left / BackDrawer
BottomShelf
RightCabinet
Case# 31Wall
EastBuilding
Freida Smith HallCategory
Permanent