Coaiilri/ Soiifli of Yorrd. 285 



soiiK' c)t' the I;ii<j[cT onus iiioii- remote I'i'oiii the valley heads are 

 probaljly due to \varj)in<_' alter tlie development of the valleys. 



There is no neeessity to rej^ar<l the late depression, known to 

 have occurred in the Yarra valley, as uniformly affecting a lar<;e 

 area. Imt rather as part of a movement which acted unequally in 

 different places even a short distance apart. 



