Definition: A section of the Earths's crust that is demarcated by faults or flexures. In the movement of the crust, a massif tends to retain its internal structure while being displaced as a whole.
Known occurrences, collected specimens and observations of Ameerega boehmei Lötters, Schmitz, Reichle, Rödder & Quennet 2009. View this species on GBIF