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Trama

Trama, pikor tamaina handia duten sedimentuak dira: legarraren eta harearen tamainako partikulak dituzten sedimentuak, alegia. Partikula horiek meteorizazio fisikoaren eraginez sortzen dira, eta, sarritan, matrizearekin batera ageri dira arroketan. Trama eta matrize kantitateek arroken ehunduraren paketatzea baldintzatzen dute, eta horren araberako hainbat sailkapen egiten da (ikus, adibidez, kareharriaren sailkapena).

Ikus, gainera

Kanpo estekak

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