Random Formation

Random Formation
Stratigraphic range: Early Cambrian PreꞒ Ꞓ O S D C P T J K Pg N
Bonavista Fm and others[4]
Overlies	Chapel Island Fm (conformably, Burin Peninsula) Crown Hill Formation (conformably, Random Island)[5]
Thickness	From a few metres to 250 m[6]
Lithology
Primary	Herringbone-crossstratified white arenites
Other	Grey-green silts and shales
Location
Region	Newfoundland
Country	Canada
Type section
Named for	Random Island
Bedrock distribution of the Random Formation

The Random Formation is a rock unit in

Its white arenitic sandstones are very distinctive, recognizable from their herringbone cross-stratification that denotes the influence of storm systems. Interbedded green-grey sands and silts represent an intertidal setting.^[5]

Spatial distribution

It is widespread throughout Newfoundland unlike its underlying units. It was deposited in intertidal mud flats to subtidal setting, then (later) near the bottom of an open marine shelf.^[11]

The top of the unit intergrades with the overlying strata.^[10]

Stratigraphy

Some studies^[1] assign the Random Formation as the lowest unit of the Adeyton Group, but strictly it is below that group.^[5]

It overlies the Chapel Island formation, which contains the Precambrian/Cambrian boundary.^[12]

The unit is often strongly folded.^[5]

Age

The formation is difficult to date, but is considered Precambrian, as it lies unconformably under the Bonavista Formation and conformably above Ediacaran strata.^[2] It does sit above the Chapel Island Formation on the Burin peninsula meaning that, at that location, the lower boundary is in the Lower Cambrian. Inarticulate brachiopods have been found in its upper strata, dating these to the late early or even early mid Cambrian.^[10]

However, it is likely that the unit is