The basal conglomerates are made up of hard sandstone which contains angular grains.
2.
This basal conglomerate contains quartzite clasts that lack any known equivalents in the Grand Canyon region.
3.
This basal conglomerate is typically composed of gravel that is locally derived from either the underlying Temple Butte Limestone or Muav Limestone.
4.
The lowest part of the Nankoweap Formation consists of a basal conglomerate that is composed chiefly of gravel derived from the Cardenas Basalt.
5.
The Bangor Formation overlies the Minfordd Formation and it underlies the Llanberis Slates and is a similar lithology to the Minfordd Formation excepting the basal conglomerate.
6.
The basal rocks of the Minfordd Formation contain clasts of granite, vein quartz, quartzitic sandstone, quartzose schists and were thought to be Cambrian basal conglomerate.
7.
The basal conglomerate is cut into sections by the faults and can be traced in a general eastwards direction from the village to the hill top 3 km away.
8.
In marine environments, rudites were deposited along shorelines as part of beaches, as basal conglomerates during marine transgressions, and in the deep sea by slumps and turbidites.
9.
The upper contact is a disconformity that typically consists of nearly horizontal surfaces with little or no relief and overlain locally by a basal conglomerate within the overlying Redwall Limestone.
10.
Its upper contact is a disconformity that characteristically is a nearly horizontal surface with little or no relief . ( In the Grand Canyon, the upper disconformity forms a horizontal platform at the top of the Redwall Limestone . ) Locally, the bottom unconformity of the Redwall Limestone contains a basal conglomerate that directly rests upon this bottom unconformity.
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