Lesson 2: Physical Properties of Mineral Flashcards
(70 cards)
Crystal Form and Crystal Habit
- Morphology
- Form
- Habit
- Unit Cell
- Aggregate
- completely bounded by crystal
- growth during primary crystallization or recrystallization was not restrained or interfered with by adjacent grains, and the faces were not greatly affected by late physical or chemical erosion
Euhedral Crystals (idiomorphic or automorphic)
- partly bounded by crystal and partly by surfaces formed against pre-existing grains
- minerals were able to crystallize with their characteristic habit only in part, due to the presence of neighboring crystals that partly constrained their growth
Subhedral (ipidiomorphic)
- lacks crystal faces and shows rounded or irregular surfaces due to crowding of adjacent minerals
- e.g. embayed crystals with irregular outline, but also interstitial grains that grew in the space left between other, pre-existing crystals
Anhedral (xenomorphic or allotriomorphic)
The outward expression of the internal ordered atomic arrangement of a crystal
Morphology
Consists of a group of crystal faces which have the same relation to the elements of symmetry
Form
Includes the general shape of a crystal and its
growth irregularities
Habit
The smallest unit of structure that if stacked indefinitely in three dimensions would form the whole structure (further discussion in Crystallography)
Unit cell
Minerals whose crystals come in groups (e.g. thousands of crystals intimately intergrowing to form unique aggregate shapes)
Aggregate
For a crystal with one dimension markedly longer than the other two
Prismatic
With the external form of a rhombohedron
Rhombohedral
With the external form of a cube
Cubic
With the external form of an octahedron
Octahedral
With the pronounced development of one or more two-sided forms (pinacoid)
Pinacoidal
Crystals are roughly equidimensional
Equant
Flat and plate-like but crystals are typically thin and can be stacked on top of each other like sheets of paper
Lamellar
Flat and plate-like but have lengths and widths that are much larger than their thickness
Tabular
Crystals are elongated and flattened, like a knife blade, crystals are much longer than they are wide, and their width exceeds their depth
Bladed
Form as thin, flat sheets or flakes that are easily peeled or split off the larger mass
Micaceous
when edges are fully developed but the interior spaces are not filled in (hollowed-out step lattice formation)
Hopper
Crystal growth that produces fine, feathery scales from the Latin “pluma” = feather (fan-like or feather-like)
Plumose
needlelike, contains long, slender crystals which may radiate out like needles or bristles from a common base
Acicular
exhibits hairlike or threadlike filaments (Latin
“filum” = thread)
Filiform
exhibits clumps of sinewy, stringy, or hairlike fibers, the direction of growth is parallel to the longest dimension of the crystal
Fibrous