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Pages 20-30

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From page 20...
... b . Thickness At leas t 6600 feet .
From page 21...
... 2 . Definit ion "The igneous rocks lie for the most part to the eas t of East Base and are compos ed of hornblende granite wh ich is somewhat variable in texture ; the mineral c�a ition , however , is uniform." (Knowles , 1945)
From page 22...
... 3 . Type sect ion a.
From page 23...
... b. Thickness 15 , 000 feet estimated; 4600 feet minimam �ade, F
From page 24...
... c . Evidence for age E lbow Formation A spec imen from Peeler ' s Pinnacle on the E ights Coast yielded lead-alpha age from z ircon of 150 ± 20 m.
From page 25...
... d . Relation to other units Conformably overlies E lliott Sandstone .
From page 26...
... c . Lithology Pink to buff cross -bedded , coarse-grained sands tone , with thick and thin interbedded conglomerate beds and minor thin red shaly beds in lower half.
From page 27...
... c . Lithology Quartz ite and marble (brecciated locally)
From page 28...
... 2 . Definit ion See Execut ive Committee red tuff " cross -bedding , intercalat ion of strata , and part ial raunding of volcanic fragments characterizes the grey tuff , which thus resembles a river depos it .
From page 29...
... grooves , 10-15 cent imeters in depth , apparently the result of abras ion by rock fragments imbedded in s lowly flowing glacier ice ." (Doumani , 707 )
From page 30...
... 2 . Definit ion "Overlying the basalt are three dis t inct rock units cons is ting of compacted , fine-grained volcanic fragments , or tuff .

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