Northern Province Chalk nomenclature - Hunstanton Formation: Difference between revisions
Created page with " Name The term Hunstanton Formation is defined herein. It is a modification of a number of previous names given to the beds with a distinctive red colour (in part), below ..." |
No edit summary |
||
| Line 1: | Line 1: | ||
=====Name===== | |||
Name | |||
The term Hunstanton Formation is defined herein. It is a modification of a number of previous names given to the beds with a distinctive red colour (in part), below a strongly developed erosion surface and of Albian age (known to be of Lower Cenomanian age as defined by Mitchell, 1995 in the ‘Cleveland Basin’) found below a strongly developed erosion surface beneath the Chalk Group (and from which it is now specifically excluded). | The term Hunstanton Formation is defined herein. It is a modification of a number of previous names given to the beds with a distinctive red colour (in part), below a strongly developed erosion surface and of Albian age (known to be of Lower Cenomanian age as defined by Mitchell, 1995 in the ‘Cleveland Basin’) found below a strongly developed erosion surface beneath the Chalk Group (and from which it is now specifically excluded). | ||
=====''Type section''===== | |||
''Type section'' | |||
Hunstanton Cliff [TF 6725 4130 to TF 6786 4238], north Norfolk (Owen, 1995; Gallois, 1994). | Hunstanton Cliff [TF 6725 4130 to TF 6786 4238], north Norfolk (Owen, 1995; Gallois, 1994). | ||
=====''Primary Reference Section''===== | |||
''Primary Reference Section'' | |||
South Ferriby Quarry [SE 9915 2045], Lincolnshire (Gaunt et al., 1992). | South Ferriby Quarry [SE 9915 2045], Lincolnshire (Gaunt et al., 1992). | ||
=====Formal subdivision===== | |||
Formal subdivision | |||
None herein. The Hunstanton Formation as defined by Mitchell (1995a) describing the thick succession at Speeton in the Cleveland Basin is divided into five members. These are in ascending order the Queens Rocks Member, Speeton Beck Member, Dulcey Dock Member, Weather Castle Member and the Red Cliff Hole Member. | None herein. The Hunstanton Formation as defined by Mitchell (1995a) describing the thick succession at Speeton in the Cleveland Basin is divided into five members. These are in ascending order the Queens Rocks Member, Speeton Beck Member, Dulcey Dock Member, Weather Castle Member and the Red Cliff Hole Member. | ||
=====''Lithology ''===== | |||
''Lithology '' | |||
Rubbly to massive chalks with marl bands; typically pink to brick-red in colour (due to disseminated hematite), but locally upper part grey due to secondary alteration of the iron minerals. The lower part of the formation is commonly weakly sandy. | Rubbly to massive chalks with marl bands; typically pink to brick-red in colour (due to disseminated hematite), but locally upper part grey due to secondary alteration of the iron minerals. The lower part of the formation is commonly weakly sandy. | ||
=====''Definition of upper boundary''===== | |||
''Definition of upper boundary'' | |||
Erosion surface, locally developed as a hardground, overlain by nodular chalk (lowest Cenomanian) of Paradoxica (or Sponge) Bed or (in Cleveland Basin) Crowe’s Shoot Member (Mitchell, 1995a); this horizon (the base of the Lower Chalk in Norfolk, or elsewhere of the Ferriby Formation) may or may not correspond with the upper limit of red chalks. | Erosion surface, locally developed as a hardground, overlain by nodular chalk (lowest Cenomanian) of Paradoxica (or Sponge) Bed or (in Cleveland Basin) Crowe’s Shoot Member (Mitchell, 1995a); this horizon (the base of the Lower Chalk in Norfolk, or elsewhere of the Ferriby Formation) may or may not correspond with the upper limit of red chalks. | ||
=====''Definition of lower boundary ''===== | |||
Sharp or (apparently) gradational boundary of marly chalks with ferruginous sandstones of Carstone Formation or (in Cleveland Basin) with mudstone of Speeton Clay Formation; commonly marked by a line of phosphatic nodules (burrow-fills). | |||
=====''Thickness''===== | |||
''Thickness'' | |||
c. 1 m at type section in Norfolk, typically 3 m in Lincolnshire and south Yorkshire, thinning over Market Weighton High but expanding up to an estimated c. 30 m in Cleveland Basin with c. 24 m exposed in the cliffs at Speeton. | c. 1 m at type section in Norfolk, typically 3 m in Lincolnshire and south Yorkshire, thinning over Market Weighton High but expanding up to an estimated c. 30 m in Cleveland Basin with c. 24 m exposed in the cliffs at Speeton. | ||
=====Distribution===== | |||
Distribution | |||
Present throughout Yorkshire (including the Cleveland Basin where it attains its maximum development) and Lincolnshire and extends southwards to its type locality of Hunstanton on the north Norfolk coast. | Present throughout Yorkshire (including the Cleveland Basin where it attains its maximum development) and Lincolnshire and extends southwards to its type locality of Hunstanton on the north Norfolk coast. | ||
=====''Previous names''===== | |||
''Previous names'' | |||
Red Chalk (see definition in Southern Province section) | Red Chalk (see definition in Southern Province section) | ||
=====Hunstanton Limestone===== | |||
Hunstanton Limestone | |||
Hunstanton Red Rock | Hunstanton Red Rock | ||
=====Hunstanton Chalk Formation===== | |||
Hunstanton Chalk Formation | |||
Hunstanton Red Chalk Formation (Owen, 1995 and Mortimore et al., 2001) | Hunstanton Red Chalk Formation (Owen, 1995 and Mortimore et al., 2001) | ||
Hunstanton Chalk Member (Wood and Smith, 1978). | Hunstanton Chalk Member (Wood and Smith, 1978). | ||
=====Parent===== | |||
Parent | |||
Stand alone formation beneath and excluded from the definition of the Chalk Group. | Stand alone formation beneath and excluded from the definition of the Chalk Group. | ||
=====''Age and biostratigraphy ''===== | |||
''Age and biostratigraphy '' | |||
Lower Cretaceous, middle to upper Albian. | Lower Cretaceous, middle to upper Albian. | ||
=====''References''===== | |||
''References'' | |||
Owen (1995); Mitchell (1995a). | Owen (1995); Mitchell (1995a). | ||
[[Category:Northern_Province_Chalk_nomenclature | 01]] | [[Category:Northern_Province_Chalk_nomenclature | 01]] | ||
Revision as of 15:38, 4 February 2014
Name
The term Hunstanton Formation is defined herein. It is a modification of a number of previous names given to the beds with a distinctive red colour (in part), below a strongly developed erosion surface and of Albian age (known to be of Lower Cenomanian age as defined by Mitchell, 1995 in the ‘Cleveland Basin’) found below a strongly developed erosion surface beneath the Chalk Group (and from which it is now specifically excluded).
Type section
Hunstanton Cliff [TF 6725 4130 to TF 6786 4238], north Norfolk (Owen, 1995; Gallois, 1994).
Primary Reference Section
South Ferriby Quarry [SE 9915 2045], Lincolnshire (Gaunt et al., 1992).
Formal subdivision
None herein. The Hunstanton Formation as defined by Mitchell (1995a) describing the thick succession at Speeton in the Cleveland Basin is divided into five members. These are in ascending order the Queens Rocks Member, Speeton Beck Member, Dulcey Dock Member, Weather Castle Member and the Red Cliff Hole Member.
Lithology
Rubbly to massive chalks with marl bands; typically pink to brick-red in colour (due to disseminated hematite), but locally upper part grey due to secondary alteration of the iron minerals. The lower part of the formation is commonly weakly sandy.
Definition of upper boundary
Erosion surface, locally developed as a hardground, overlain by nodular chalk (lowest Cenomanian) of Paradoxica (or Sponge) Bed or (in Cleveland Basin) Crowe’s Shoot Member (Mitchell, 1995a); this horizon (the base of the Lower Chalk in Norfolk, or elsewhere of the Ferriby Formation) may or may not correspond with the upper limit of red chalks.
Definition of lower boundary
Sharp or (apparently) gradational boundary of marly chalks with ferruginous sandstones of Carstone Formation or (in Cleveland Basin) with mudstone of Speeton Clay Formation; commonly marked by a line of phosphatic nodules (burrow-fills).
Thickness
c. 1 m at type section in Norfolk, typically 3 m in Lincolnshire and south Yorkshire, thinning over Market Weighton High but expanding up to an estimated c. 30 m in Cleveland Basin with c. 24 m exposed in the cliffs at Speeton.
Distribution
Present throughout Yorkshire (including the Cleveland Basin where it attains its maximum development) and Lincolnshire and extends southwards to its type locality of Hunstanton on the north Norfolk coast.
Previous names
Red Chalk (see definition in Southern Province section)
Hunstanton Limestone
Hunstanton Red Rock
Hunstanton Chalk Formation
Hunstanton Red Chalk Formation (Owen, 1995 and Mortimore et al., 2001)
Hunstanton Chalk Member (Wood and Smith, 1978).
Parent
Stand alone formation beneath and excluded from the definition of the Chalk Group.
Age and biostratigraphy
Lower Cretaceous, middle to upper Albian.
References
Owen (1995); Mitchell (1995a).