Hanging Rocks Formation

From Wikipedia, the free encyclopedia
Jump to navigation Jump to search
Hanging Rocks Formation
Stratigraphic range: Ediacaran 557–550 Ma[1]
TypeFormation
Unit ofMaplewell Group
Sub-unitsHallgate and Sliding Stone Slump Breccia Members
Underlies
OverliesBradgate Formation[2]
Thickness50 m (164 ft)[1]
Lithology
PrimaryTuff
OtherGraywacke
Location
RegionLeicestershire
CountryUnited Kingdom
Type section
Named forBradgate Park

The Hanging Rocks Formation is a geologic formation in Leicestershire, and is the youngest and smallest of the Maplewell Group and the larger Charnian Supergroup which it is a part of. Due to this, and the fact that the rocks are not well exposed at both the top and base,[1] there have been no Ediacaran fossils found to date, unlike the two underlying Bradgate and Beacon Hill Formations.

Dating

[edit | edit source]

Despite the poor exposure of the formation, scientists were able to collect zircon crystals from the lower parts of the formation, allowing them to perform zircon U–Pb dating, which recovered a date of 556±6.4 Ma, close to the Bradgate Formations top age of 557 Ma. It is noted that the top of the formation is capped at a zircon age of roughly 550 Ma,[1] which is just before the first formations of the Nama assemblage were deposited.

Lua error in mw.title.lua at line 392: bad argument #2 to 'title.new' (unrecognized namespace name 'Portal').

References

[edit | edit source]
  • Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  1. ^ a b c d Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  2. ^ a b Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  3. ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).