Resumen de El paleokarst cuaternario de Alcubilla del Marqués (Soria).

M. C. Ramos Martín, Gaspar Alonso Gavilán

• The paleokarst of Alcubil[a del Marqués (Soria) is a portion of karstic building which has been eliminated by erosion. During karstic active stage, carbonatic (stalactite, stalagmite, cave popcorn) and siliciclastic (fluvial bars) sediments were developed