URI	prefLabel	Definition	Source
http://resource.geosciml.org/classifier/cgi/lineationtype/augen_lineation	augen lineation	A shape lineation defined by elongate augen.	this vocabulary
http://resource.geosciml.org/classifier/cgi/lineationtype/bedding_cleavage_intersection_lineation	bedding cleavage intersection lineation	Lineation defined by the intersection of bedding surfaces and cleavage surfaces.	this vocabulary
http://resource.geosciml.org/classifier/cgi/lineationtype/biotite_mineral_lineation	biotite mineral lineation	"Mineral lineation defined by aligned elongate biotite aggregates in a foliation surface. Biotite does not have an elongate (prismatic, acicular) mineral habit, so production of lineation must reflect elongate aggregates of biotite crystals."	this vocabulary
http://resource.geosciml.org/classifier/cgi/lineationtype/cleavage_intersection_lineation	cleavage intersection lineation	Lineation defined by the intersection of two cleavages.	this vocabulary
http://resource.geosciml.org/classifier/cgi/lineationtype/crenulation_lineation	crenulation lineation	"Lineation defined by small-scale wrinkles, typically of phylosillicate minerals, on another surface, typically a cleavage or schistosity. Use instead of intersection lineation if the wrinkles are the measured feature and the intersecting planar feature is not apparent."	this vocabulary
http://resource.geosciml.org/classifier/cgi/lineationtype/flow_lineation	flow lineation	"A linear alignment of fabric elements, especially elongate or rod-shaped minerals, interpreted to have been aligned by flow of magma, lava, pyroclastic material, or diapiric flow of sedimentary rock."	"Geoscience Victoria, Australia"
http://resource.geosciml.org/classifier/cgi/lineationtype/hornblende_mineral_lineation	hornblende mineral lineation	Mineral lineation defined by aligned hornblende crystals.	this vocabulary
http://resource.geosciml.org/classifier/cgi/lineationtype/igneous_lineation	igneous lineation	Lineation defined by alignment of elongate fabric elements formed in lava or magma before complete crystallization. Some typical fabric elements are elongate phenocrysts and vesicles.	this vocabulary
http://resource.geosciml.org/classifier/cgi/lineationtype/igneous_mineral_lineation	igneous mineral lineation	Lineation in igneous rock defined by aligned crystals where there is evidence that the crystal alignment is related to process occurring before the rock was solidified.	this vocabulary
http://resource.geosciml.org/classifier/cgi/lineationtype/igneous_particle_shape_lineation	igneous particle shape lineation	"Lineation in an igneous rock, usually welded tuff, defined by elongate objects in the rock (usually pumice pads, also elongate crystals). Descriptive--elogation may be due to deformation or to rotation/alignment of originally elongate (prolate ellipsoid) objects in the rock."	 this vocabulary
http://resource.geosciml.org/classifier/cgi/lineationtype/igneous_vesicle_lineation	igneous vesicle lineation	lineation defined in a volcanic rock by aligned elongation direction of vesicles.	this vocabulary
http://resource.geosciml.org/classifier/cgi/lineationtype/intersection_lineation	intersection lineation	A lineation produced by the intersection of two planar fabrics.	"Neuendorf et al 2005, this vocabulary"
http://resource.geosciml.org/classifier/cgi/lineationtype/lineation	lineation	Nongenetic term for a penetrative linear structure.	"Neuendorf et al 2005, this vocabulary"
http://resource.geosciml.org/classifier/cgi/lineationtype/mineral_lineation	mineral lineation	Lineation defined by alignment of elongate crystals that have a prismatic crystal habit or of monomineralic grain aggregates.	"Neuendorf et al 2005, this vocabulary"
http://resource.geosciml.org/classifier/cgi/lineationtype/particle_shape_lineation	particle shape lineation	"Lineation defined by alignment of long axes of prolate-shaped particles such as clasts, fossils, crystals, or phenocrysts. Particles may be polycrystalline aggregates formed by deformation of pre-existing particles. General category does not specify genesis of particles or their alignment."	this vocabulary
http://resource.geosciml.org/classifier/cgi/lineationtype/pencil_lineation	pencil lineation	"Lineation defined by tendency of rock to break into long, slender pieces resembling pencils. Typically produced by intesection of bedding and cleavage or intersection of two cleavages. Fabric is generally only observed in weakly metamorphosed rocks."	based on Neuendorf et al 2005
http://resource.geosciml.org/classifier/cgi/lineationtype/quartz_fibre_lineation	quartz fibre lineation	Aligned quartz fibres that define a measurable lineation	this vocabulary
http://resource.geosciml.org/classifier/cgi/lineationtype/rodding_lineation	rodding lineation	Linear structure in metamorphic rocks in which the stronger parts have been shaped into parallel rods (eg. vein quartz)	Jackson 1997
http://resource.geosciml.org/classifier/cgi/lineationtype/sillimanite_mineral_lineation	sillimanite mineral lineation	Mineral lineation defined by aligned sillimanite crystals.	this vocabulary
http://resource.geosciml.org/classifier/cgi/lineationtype/slickenline	slickenline	"Lineation on a brittle slip surface defined by grooves, ridges, or striations"	based on Neuendorf et al 2005
http://resource.geosciml.org/classifier/cgi/lineationtype/stretching_lineation	stretching lineation	"Lineation defined by elongate (prolate) fabric elements in which the alignment of the fabric elements, and the formation of prolate fabric elements is interpreted to be the product of crystal plastic deformation processes. Associated with mylontic foliation."	this vocabulary
http://resource.geosciml.org/classifier/cgi/lineationtype/tectonic_lineation	tectonic lineation	"Penetrative linear structure in a rock body defined by fabric elements that are the product of tectonic processes. Linear is used in the sense that the orientation of the structure can be represented as a line in some sufficiently small neighborhood of any point in the material containig the fabric. Penetrative denotes that the fabric elements defining the structure are repeated at distances so small, compared with the scale of the whole?that they can be considered to pervade it uniformly and be present at every point (paraphrase of Turner and Weiss, 1963, p. 21)."	this vocabulary