The geologists
state that they indicate a columnar structure, the tops of the columns
being weathered out.
The specimens we saw were very perfect. Had some interesting
instruction in geology in the evening. I should not regret a stay
here with our two geologists if only the weather would allow us to
get about.
This morning the wind moderated and went to the S.E.; the sea
naturally fell quickly. The temperature this morning was + 17 deg.;
minimum +11 deg.. But now the wind is increasing from the S.E. and it is
momentarily getting colder.
_Thursday, March_ 23, A.M.--No signs of depot party, which to-night
will have been a week absent. On Tuesday afternoon we went up to
the Big Boulder above Ski slope. The geologists were interested,
and we others learnt something of olivines, green in crystal form
or oxidized to bright red, granites or granulites or quartzites,
hornblende and feldspars, ferrous and ferric oxides of lava acid,
basic, plutonic, igneous, eruptive--schists, basalts &c. All such
things I must get clearer in my mind. [19]
Tuesday afternoon a cold S.E. wind commenced and blew all night.
Yesterday morning it was calm and I went up Crater Hill. The sea
of stratus cloud hung curtain-like over the Strait--blue sky east
and south of it and the Western Mountains bathed in sunshine, sharp,
clear, distinct, a glorious glimpse of grandeur on which the curtain
gradually descended.
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