A PHOTOGRAIMIK' i<:PITOIVIK 265 
soulli-wcst — 10,000 (cci I sIkhiIJ (Iiiiik, hut all our survey 
angles wcro so aculc lliat ii is tlillu ull (o lix dicir tlis- 
lancx' exactly. To llir nor( li-vvt'S( was a liuc Mack caj^iH't,! 
peak where llic glacier left llie Tlatt-au. T!iis 1 called 
Mount Tryggve (Jran. 
We were clue back at Cape (Icolo^y ahoul (lie Slli, 
so 1 Icl 1 1 lial t Ills was our wesltan liniil . We s|HaU 
another clay surveyiui^; (lie nunalak antl collcclini'; luoie 
coal antl fossils, and lci( ahoul noon on (he 6lh iov our 
return lo the rcncle/vous. Wc reachcil our I'lai Iron 
Camp williout incident and devo(ed a tlay lo collccling 
and photograpliy. 
One ph()t(t^i;raph was an cpilonic of ihc pliysiotn-aphy 
of the re^Mou. I note llia( il shows ' Tin- ice fate, (he 
crevasses, the skauk, youn^i;' " calved 'M)er^';s, low moraines, 
ret real injj; glacier, high moraines, granite pavements, 
shear cracks in the bay ice, the ice toniMu-, the fatclled 
dills, cwm valleys, overllovv glacierels, hogback ridges, 
non-glaciated ]ieaks, the old glacier flood lloor, and the 
Junction of tlie granite and (lie dolcri(e/ All (his on a 
single ;j-pla(e negative ! 
l^ach day I, enlered up the met eorolo<'ical log. The 
clouds were describetl also, veiy ollrn l»y the word ovrrcd.sl . 
I5ut tliis afternoon we noticetl the sea rolling; in below 
us, gradually blotting ou( the bay, then the ice ((tugue 
and the headlands below. I was some distance away from 
the tent and before \ could re( u rn t lie cam p was com- 
pletely hidden. The ot hers also mana^'/'d (o get l)ack 
safely, but the cohl and the high (lilfs round (he Mat Iron 
made it a nasty place to be lost in I he h>g. We c^aild d(j 
