crystal habit

25
Crystal habits of some common minerals • The crystal habit of a mineral describes its visible external shape. It can apply to an individual crystal or an assembly of crystals •.

Upload: robert-craig

Post on 19-Jan-2015

273 views

Category:

Spiritual


1 download

DESCRIPTION

 

TRANSCRIPT

Page 1: Crystal habit

Crystal habits of some common minerals

• The crystal habit of a mineral describes its visible external shape. It can apply to an individual crystal or an assembly of crystals

• .

Page 2: Crystal habit

pyrite

Page 3: Crystal habit

Twelve-sided garnet crystals

Page 4: Crystal habit

• Cleavage or fracture: conchodial fracture• Hardness: 7• Color: Red, green, brown• Other diagnostic: equant 12 sided crystals

• Ca, Fe, Mg, Al, Cr, Mn, silicate

Page 5: Crystal habit

Slender tourmaline crystals

Page 6: Crystal habit

Prismatic quartz crystals

Page 7: Crystal habit

• Cleavage or fracture: conchoidal fracture• Hardness: 7• Color: pink, colorless• Diagnostic properties: elongate six sided

crystals

Page 8: Crystal habit

Potassic feldspar

Page 9: Crystal habit

CaAlSi2O8 + NaAlSi2O8

• Cleavage and fracture : two directions at 90o• Hardness: 6• Other diagnositic: Striations (fine lines) on one

of the two cleavage directions ; solid solution between sodium (albite) and calcium (anthornite) plagioclase

Page 10: Crystal habit

• cubic (or isometric) crystal system is a crystal system where the unit cell is in the shape of a cube. This is one of the most common and simplest shapes found in crystals and minerals.

Page 11: Crystal habit

• There are three main varieties of these crystals:

• Primitive cubic (abbreviated cP[1] and alternatively called simple cubic)

• Body-centered cubic (abbreviated cI[1] or bcc), • Face-centered cubic (abbreviated cF[1] or fcc,

and alternatively called cubic close-packed or ccp)

Page 12: Crystal habit

• Each is subdivided into other variants listed below. Note that although the unit cell in these crystals is conventionally taken to be a cube, the primitive unit cell often is not. This is related to the fact that in most cubic crystal systems, there is more than one atom per cubic unit cell

Page 14: Crystal habit

• A rock containing three crystals of pyrite (FeS2). The crystal structure of pyrite is primitive cubic, and this is reflected in the cubic symmetry of its natural crystal facets.

Page 17: Crystal habit

primitive cubic system (cP)

• The primitive cubic system (cP) consists of one lattice point on each corner of the cube. Each atom at a lattice point is then shared equally between eight adjacent cubes, and the unit cell therefore contains in total one atom (1⁄8 × 8).

Page 19: Crystal habit

A caesium chloride unit cell

• Each of the two atom types forms a separate primitive cubic lattice, with an atom of one type at the center of each cube of the other type. Altogether, the arrangement of atoms is the same as body-centered cubic

Page 20: Crystal habit

• The body-centered cubic system (cI) has one lattice point in the center of the unit cell in addition to the eight corner points. It has a net total of 2 lattice points per unit cell (1⁄8 × 8 + 1).

Page 21: Crystal habit

function of ionic radius

• more likely to be formed from two elements whose ions are of roughly the same size (for example, ionic radius of Cs+ = 167 pm, and Cl− = 181 pm) .

Page 23: Crystal habit

0,0,x > y,0,0 > 0,z,0The ℓ, m, and n directional indices are separated by 90°,

Page 25: Crystal habit