WHOLE VOL. SKELETAL REMAINS OF EARLY MAN — HRDLICKA 303 



ADDITIONAL LITERATURE 



DiECK, W. Das Gebiss des diluvialen Homo monstcricnsis Hauseri und seine 

 Rekonstruktion. Odontologisk Tidskrift, No. 3, 1923. 



Klaatsch, H. Der primitive Mensch der Vergangenheit und der Gegenwart. 

 Verhandl. Ges. d. naturf. Arzte, 80 Ver., Vol. I, p. 95, Koln, 1908. 



. Die Fortschritte der Lehre von der Neandertalrasse. Ergeb. Anat. u. 



Entwicklungsgesch., Vol. 17, 1907; Wiesbaden, 1908. 



. Das Gesichtsskelett der Neandertalrasse und der Australier. Ver- 

 handl. anatom. Ges., 1908. 



AND Hauser. Homo monstcricnsis Hauseri. Arch. Anthrop., Vol. 7, 



p. 287, 1909. 



— AND Hauser. Die neuesten Ergebnisse der Palaontologie des Menschen 

 und ihre Bedeutung fiir das Abstammungsproblem. Z. Ethnol., Vol. 41, 



p. 537, 1909- 



— AND Hauser. Kraniomorphologie und Kraniotrigonometrie. Arch. 



Anthr., Vol. 8, pp. 1-23, 1909. 

 ScHUCHHARDT. Die ncuc Zusanimensetzung des Schadels von Homo mous- 



fcriensis Hauseri. Prahist. Zeitschr., Vol. 4, p. 443, 1912. 

 ViRCHOVv, H. Z. Ethnol., p. 580, 1909. 

 . Die Aurignac-Rasse und ihre Stellung im Stamnibaum der Menschheit. 



Z. Ethnol., Nos. 3-4, 1910. 

 . Homo anrignacicnsis Hauseri. Prahist. Zeitschr., Vol. I, pp. 273, 285, 



1910. 

 — . Z. Ethnol., p. 1407, 1916. 



THE GALILEE SKULL 



In 1925, the British School of Archeology in Jerusalem decided 

 upon the exploration of certain caves in Galilee, and the work was 

 entrusted to Mr. F. Turville-Petre who, during a previous season, 

 had made a preliminary survey of the area. The main site explored 

 by Mr. Petre during the year was what is now often referred to as 

 the " Galilee Cave " and in this cave, at the depth of 6^ feet, towards 

 the lower limit of a paleolithic horizon, were found parts of a ne- 

 anderthaloid human skull. The main details of the discovery, since 

 published,* are as follows : 



Entering the ravine of the Wadi el 'Amud and walking some 150 m. up stream, 

 a cave known as the Mugharet-el-Zuttiyeh is to be seen high up in the cliffs to 

 the north of the stream. The stream at this point is not more than 3 m. wide, 

 and the width of the ravine from base to base of the cliffs might be estimated 

 at about 15 m. The cave, a natural limestone formation, is situated at the base 

 of a precipitous wall of rock, facing southwest ; the cliff, which rises to a height 

 of some 20 m. above the entrance, renders it inaccessible from the plateau above ; 



^ Turville-Petre, P., Researches in Prehistoric Galilee, 1925-1926. 

 Keith, Sir Arthur, A report on the Galilee Skull. British School of Archae- 

 ology in Jerusalem. London, 1927. 



