. British Antarctic expedition, 1907-9, under the command of Shackleton : reports on the scientific investigations ; geology. oast by way of Clear Lake and Coast Lake, while the main valley continues as abroad depression filled with morainic material in a north and south direction. (SeePlate XLI. Fig. 1.) Two lakes near Cape Barne, Sunk Lake and Deep Lake,appear to be situated in a continuation of the same valley, whilst the other im-portant grooves appear to run more or less parallel with this one, as, for instance,that which the tripartite Terrace Lake occupies. (See Plate XLI. Fig. 2.)
. British Antarctic expedition, 1907-9, under the command of Shackleton : reports on the scientific investigations ; geology. oast by way of Clear Lake and Coast Lake, while the main valley continues as abroad depression filled with morainic material in a north and south direction. (SeePlate XLI. Fig. 1.) Two lakes near Cape Barne, Sunk Lake and Deep Lake,appear to be situated in a continuation of the same valley, whilst the other im-portant grooves appear to run more or less parallel with this one, as, for instance,that which the tripartite Terrace Lake occupies. (See Plate XLI. Fig. 2.) The remaining lakes or tarns are situated in the depressions which are essentiallycharacteristic results of the phase of denudation which is so typically illustrated angles and craggy projections have been rounded by the Great Ice Sheet, and amantle of morainic matter of varying thickness has been deposited on top of thecountry rock, while through this mantle bosses of the more resistant types of kenyteproject here and there. Green Lake. Green Lake lies about half-way between Blacksand Beach and i •^i-** ii^Sitf*. .>*^-V^^ -*~^
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