http://inspire.ec.europa.eu/codelist/LithologyValue/sedimentaryRockINSPIRE Registry teamJRC-INSPIRE-SUPPORT@ec.europa.euhttp://inspire.ec.europa.eu/registry2015-08-18 17:30 PM CEST2015-08-18 17:30 PM CESTsedimentary rockRock formed by accumulation and cementation of solid fragmental material deposited by air, water or ice, or as a result of other natural agents, such as precipitation from solution, the accumulation of organicMaterial, or from biogenic processes, including secretion by organisms.http://inspire.ec.europa.eu/codelist/LithologyValue/genericConglomerate2015-08-18 18:03 PM CEST2015-08-18 18:03 PM CESTgeneric conglomerateSedimentary rock composed of at least 30 percent rounded to subangular fragments larger than 2 mm in diameter; typically contains finer grained material in interstices between larger fragments. If more than 15 percent of the fine grained matrix is of indeterminant clastic or diagenetic origin and the fabric is matrix supported, may also be categorized as wackestone. If rock has unsorted or poorly sorted texture with a wide range of particle sizes, may also be categorized as diamictite.http://inspire.ec.europa.eu/codelist/LithologyValue/genericMudstone2015-08-18 18:03 PM CEST2015-08-18 18:03 PM CESTgeneric mudstoneSedimentary rock consisting of less than 30 percent gravel-size (2 mm) particles and with a mud to sand ratio greater than 1. Clasts may be of any composition or origin.http://inspire.ec.europa.eu/codelist/LithologyValue/genericSandstone2015-08-18 18:03 PM CEST2015-08-18 18:03 PM CESTgeneric sandstoneSedimentary rock in which less than 30 percent of particles are greater than 2 mm in diameter (gravel) and the sand to mud ratio is at least 1.http://inspire.ec.europa.eu/codelist/LithologyValue/hybridSedimentaryRock2015-08-18 18:03 PM CEST2015-08-18 18:03 PM CESThybrid sedimentary rockSedimentary rock that does not fit any of the other composition/genesis categories. Sedimentary rock consisting of three or more components which form more than 5 percent but less than 50 precent of the material.