Remete cave

I now describe the material of the Remete cave, situated only 10 m lower than the rock shelter of Remetehegy. It was found in a similar mineral to the previous material, ca. 10 m above the stream, where I excavated in the summer of 1949 on behalf of Vertes. During this work, about 6-7 m of humus was removed, followed by (a) a reddish-brown layer, (b) yellow loessy clay, (c) reddish-brown Pleistocene clay again. Remains of the following species (with numbers of specimens) were found (Janossy, 1953b, and subsequent identifications) ... 

The layer of the Remete cave which already contained the field mouse Apodemusy characteristic of the Holocene is unequivocally younger than the material of the rock shelter of Remetehegy. Since I was rather a beginner at the time of excavation and used somewhat obsolete methods, the material is not suited for further conclusions. 

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See also in sourсe #XX -- [ ]

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