Northern Ireland Chalk nomenclature (Ulster Cretaceous Province) - Ulster White Limestone Group: Post-Larry Bane Chalk Subgroup: Glenarm Chalk Formation: Difference between revisions
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Name | =====Name===== | ||
The Glenarm Chalk Member was first proposed in Fletcher (1967, 1977) and adopted in BGS publications subsequently. It is regarded as a formation herein. | The Glenarm Chalk Member was first proposed in Fletcher (1967, 1977) and adopted in BGS publications subsequently. It is regarded as a formation herein. | ||
=====Type section===== | |||
Type section | |||
Old quarry at Parishagh [D 304 156], half a mile northwest of Glenarm in the Midland Valley (East Antrim) Basin. | Old quarry at Parishagh [D 304 156], half a mile northwest of Glenarm in the Midland Valley (East Antrim) Basin. | ||
=====Primary Reference Section===== | |||
Primary Reference Section | |||
Cliff sections at White Rocks near Portrush and in the quarry at Larry Bane Head in the northern depositional basin. | Cliff sections at White Rocks near Portrush and in the quarry at Larry Bane Head in the northern depositional basin. | ||
| Line 19: | Line 12: | ||
At Kilwaughter [D354 008] and Ballycarry [J449 943]. | At Kilwaughter [D354 008] and Ballycarry [J449 943]. | ||
=====Formal subdivisions===== | |||
Formal subdivisions | |||
Includes the North Antrim Hardgrounds (of member status) and is informally divided into units A to D from the base. | Includes the North Antrim Hardgrounds (of member status) and is informally divided into units A to D from the base. | ||
=====Lithology===== | |||
Lithology | |||
Limestone (chalk), with flints ranging from small nodular at the base through nodular to tabular flints in the middle part of the sequence to massive nodular at the top. The Formation can be divided into four ‘Beds’ (A to D) by subdivision on bedding planes. In the North Antrim Basin the Formation includes two well-developed hardgrounds, the North Antrim Hardgrounds (of member? status) and the sequence is therefore incomplete. In the Midland Valley (East Antrim) Basin only limited wavy bedding and scattered green glauconitised pebbles indicate interrupted sedimentation. This area is regarded as the ‘standard’. | Limestone (chalk), with flints ranging from small nodular at the base through nodular to tabular flints in the middle part of the sequence to massive nodular at the top. The Formation can be divided into four ‘Beds’ (A to D) by subdivision on bedding planes. In the North Antrim Basin the Formation includes two well-developed hardgrounds, the North Antrim Hardgrounds (of member? status) and the sequence is therefore incomplete. In the Midland Valley (East Antrim) Basin only limited wavy bedding and scattered green glauconitised pebbles indicate interrupted sedimentation. This area is regarded as the ‘standard’. | ||
=====Definition of upper boundary===== | |||
Definition of upper boundary | |||
Weathered-out bedding plane below conspicuously shelly wavy-bedded chalk at the base of the conformable Garron Chalk Formation. | Weathered-out bedding plane below conspicuously shelly wavy-bedded chalk at the base of the conformable Garron Chalk Formation. | ||
=====Definition of lower boundary===== | |||
Definition of lower boundary | |||
Base delimited by a prominent weathered-out bedding plane immediately above the Altachuile Breccia (Bed) of the Ballintoy Chalk Formation. | Base delimited by a prominent weathered-out bedding plane immediately above the Altachuile Breccia (Bed) of the Ballintoy Chalk Formation. | ||
=====Thickness===== | |||
Thickness | |||
8.10m at the type area. | 8.10m at the type area. | ||
=====Distribution===== | |||
Distribution | |||
Maximum development in the East Antrim (Midland Valley) Basin and found over the Highland Border high and well developed in the North Antrim Basin. Becomes attenuated including several non-sequences and overstepped by younger formations across the Londonderry Shelf and in the Southern Uplands Belfast district. | Maximum development in the East Antrim (Midland Valley) Basin and found over the Highland Border high and well developed in the North Antrim Basin. Becomes attenuated including several non-sequences and overstepped by younger formations across the Londonderry Shelf and in the Southern Uplands Belfast district. | ||
=====Previous names===== | |||
Previous names | |||
Glenarm Chalk of Fletcher (1967) | Glenarm Chalk of Fletcher (1967) | ||
Glenarm Chalk Member. | Glenarm Chalk Member. | ||
=====Parent===== | |||
Parent | |||
Ulster White Limestone Group. | Ulster White Limestone Group. | ||
=====Age and biostratigraphy===== | |||
Age and biostratigraphy | |||
Upper Cretaceous, Campanian. Belemnitella mucronata Zone sensu lato. | Upper Cretaceous, Campanian. Belemnitella mucronata Zone sensu lato. | ||
=====References===== | |||
References | |||
Fletcher (1967, 1977). | Fletcher (1967, 1977). | ||
[[category:Northern_Ireland_Chalk_nomenclature_(Ulster_Cretaceous_Province)_-_Ulster_White_Limestone_Group:_Post-Larry_Bane_Chalk_Subgroup | | [[category:Northern_Ireland_Chalk_nomenclature_(Ulster_Cretaceous_Province)_-_Ulster_White_Limestone_Group:_Post-Larry_Bane_Chalk_Subgroup | 02]] | ||
Latest revision as of 13:13, 11 June 2014
Name
The Glenarm Chalk Member was first proposed in Fletcher (1967, 1977) and adopted in BGS publications subsequently. It is regarded as a formation herein.
Type section
Old quarry at Parishagh [D 304 156], half a mile northwest of Glenarm in the Midland Valley (East Antrim) Basin.
Primary Reference Section
Cliff sections at White Rocks near Portrush and in the quarry at Larry Bane Head in the northern depositional basin.
The sections around Glenarm in the Midland Valley Basin.
At Kilwaughter [D354 008] and Ballycarry [J449 943].
Formal subdivisions
Includes the North Antrim Hardgrounds (of member status) and is informally divided into units A to D from the base.
Lithology
Limestone (chalk), with flints ranging from small nodular at the base through nodular to tabular flints in the middle part of the sequence to massive nodular at the top. The Formation can be divided into four ‘Beds’ (A to D) by subdivision on bedding planes. In the North Antrim Basin the Formation includes two well-developed hardgrounds, the North Antrim Hardgrounds (of member? status) and the sequence is therefore incomplete. In the Midland Valley (East Antrim) Basin only limited wavy bedding and scattered green glauconitised pebbles indicate interrupted sedimentation. This area is regarded as the ‘standard’.
Definition of upper boundary
Weathered-out bedding plane below conspicuously shelly wavy-bedded chalk at the base of the conformable Garron Chalk Formation.
Definition of lower boundary
Base delimited by a prominent weathered-out bedding plane immediately above the Altachuile Breccia (Bed) of the Ballintoy Chalk Formation.
Thickness
8.10m at the type area.
Distribution
Maximum development in the East Antrim (Midland Valley) Basin and found over the Highland Border high and well developed in the North Antrim Basin. Becomes attenuated including several non-sequences and overstepped by younger formations across the Londonderry Shelf and in the Southern Uplands Belfast district.
Previous names
Glenarm Chalk of Fletcher (1967)
Glenarm Chalk Member.
Parent
Ulster White Limestone Group.
Age and biostratigraphy
Upper Cretaceous, Campanian. Belemnitella mucronata Zone sensu lato.
References
Fletcher (1967, 1977).