ABSTRACT OF PROCEEDINGS. XI 



But the major portion of Eastern Queensland was a 

 geosynelinal not only in Pahtozoie times ])ut also through 

 most of the IMesozoic era. Folding iuoveuients in South- 

 Eastern Queensland have lasted even to the Tertiary. 

 Prof. Kiehards :\rr. W. H. Bryan, and Dr. E. O. :\rarks 

 toolc part in the su])se(juent discussion. 



Abstract op Proceedixgs, 26tii June, 1922. 



The Ordinary ^Monthly ^Meeting of the Royal Soeiety 

 of Queensland was held in the Geology Leetur;' Theatre of 

 the University at 8 p.m. on ^Monday. 26th June, li)22. 



The Pre.sident, Prof. 11. J. Priestley, :^.1.A., in the ehair. 



The minutes of the previous monthly n.ieetiug were 

 read and confirmed. 



^Ir. J. C. Me^Minn was proposed for ordinary luember- 

 ship. 



Drs. J. V. Duhig and A. H. 3Iarks were unanimously 

 elected as ordinary members. 



^Ir. C. T. White, P.L.8.. pointed out the desirability 

 of establishing an arboretum at Victoria Park, and moved 

 that the Secretary be instructed tc write to the City Council 

 and suggest that a project with this end in viev^- be 

 inaugurated. The motion was seconded by ]Mr. E. W. Bick, 

 supported by Prof. II. C. Richards. D.Sc, and carried 

 unanimously. 



On behalf of ^Ir. II. A. Longman. Dr. E. 0. ]\Iarks, 

 B.A., B.E., exhiliited a piece of sandstone from Adavale 

 showing obscure markings like impressions of the foot of a 

 kangaroo. Dr. ^larks also exhibited a specimen of slag 

 from Blount ^lorgan. 



^Ir. W. H. Bryan, M.Sc, exhibited an excellent speci- 

 men of foraminif eral limestone purchased by ]\liss C. Moxon 

 in Cairns. The polished faces showed well-preserved 

 sections of Fusulina japonica. which is the most character- 

 istic carboniferous foraminifer of Eastern Asia. 



In connnunicating his paper entitled, "The Geology 

 and Petrology of the Enoggera Granite and Allied 

 Intrusives, Part II., Petrology," Mr. Bryan gave a general 



