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4.3 Sedl,.''',tology of the ColJbs ArtllForaat10n.<br />

The Middle Ordovidan volcanism 1n the Cobbs P,.en area is<br />

thOu&:t to have been very actIve bec"-""" the volcanics of tho: sUllmIerford<br />

Grnu;> an, dOlJinated by basic flows "od sublOuine pillo,,", basahs ",Ilh only<br />

minor IncerV.y"ted tuffs and agglomerate" (Harris, 196b). 1I0wever, In the<br />

, Squid Cove-Tilt Cov; aTea (f~g. 2), t"" voleanle gtratlgraphy of the<br />

Summerford Croup

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