Envia
Inici  >  Temes  >  arquitectura

schist


Identification code: 300011626
Español: esquisto | Català: esquist



Alternative term/s

  • schists

Anotations

Scope note:

General term for a group rocks, the constituent minerals of which have assumed a position in more or less closely parallel layers due to metamorphic action. They comprise layers of lamellar minerals, such as mica, chlorite, talc, hornblende, and graphite. Quartz is often present as a secondary mineral. Schists are formed at high temperatures from shale, clay, or mud. They cleave easily along the foliated planes. Schists are usually named for their predominant mineral constituent, such as mica schist, hornblende schist, chlorite schist, and talc schist. The exception occurs when a schist is named for an unusual mineral constituent such as garnet schist, tourmaline schist, and glaucophane schist.

Web resources
Powered by: TemaTres 1.5
Avís legal | Accessibilitat | Política de galetes | Sobre gencat | © 2000 The J. Paul Getty Trust. © Generalitat de Catalunya