Fissility (geology) - Wikipedia In geology, fissility is the ability or tendency of a rock to split along flat planes of weakness (“parting surfaces”) [1] These planes of weakness are oriented parallel to stratification in sedimentary rocks [ 2 ]
FISSILITY Definition Meaning - Merriam-Webster The meaning of FISSILE is capable of or prone to being split or divided in the direction of the grain or along natural planes of cleavage How to use fissile in a sentence Did you know?
Definition of fissility - mindat. org A general term for the property possessed by some rocks of splitting easily into thin layers along closely spaced, roughly planar, and approx parallel surfaces, such as bedding planes in shale or cleavage planes in schist; its presence distinguishes shale from mudstone
Fissility - definition of fissility by The Free Dictionary Define fissility fissility synonyms, fissility pronunciation, fissility translation, English dictionary definition of fissility adj 1 Possible to split 2 Physics Fissionable, especially by neutrons of all energies 3 Geology Easily split along close parallel planes
Cleavage And Fissility - ChestofBooks. com Cleavage is "a capacity present in some rocks to break in certain directions more easily than in others," while fissility is a "structure in some rocks, by virtue of which they are already separated into parallel laminae in a state of nature
fissility - Wiktionary, the free dictionary fissility (usually uncountable, plural fissilities) The quality of being fissile (in any sense) The property of mudstones to split along layers, more or less parallel to the plane of bedding, thus becoming described as shales
Fissility (geology) - Wikiwand In geology, fissility is the ability or tendency of a rock to split along flat planes of weakness (“parting surfaces”) [1] These planes of weakness are oriented parallel to stratification in sedimentary rocks [2]
What does fissility mean? - Definitions. net Fissility refers to the property of rocks to split along planes of weakness into thin sheets This is commonly observed in shales, which are sedimentary rocks, and in slates and phyllites, which are foliated metamorphic rocks