Difference between revisions of "Hydrogeology of Wales: Permo-Triassic and Jurassic aquifers - South Wales"

From Earthwise
Jump to: navigation, search
[unchecked revision][unchecked revision]
Line 1: Line 1:
 
 
 
 
{|
 
{|
 
| [[Image:directLinkImage]]
 
| [[Image:directLinkImage]]
Line 9: Line 6:
  
 
The Triassic strata that lie to the east of Porthcawl comprises marginal basal facies deposited in a shallow coastal environment ('''Plate P802431'''). Lithologies include sandstone, conglomerate and subordinate dolomitised limestone. The conglomerates do not crop out and have poor recharge potential.
 
The Triassic strata that lie to the east of Porthcawl comprises marginal basal facies deposited in a shallow coastal environment ('''Plate P802431'''). Lithologies include sandstone, conglomerate and subordinate dolomitised limestone. The conglomerates do not crop out and have poor recharge potential.
 
  
  
 
The younger Mercia Mudstone Group comprises massive red-brown dolomitic mudstones with gypsum either in veins or retained as nodules. The uppermost part of the sequence, the Blue Anchor Formation comprises grey dolomitic mudstones and siltstones, and the Penarth Group, which is nowhere thicker than 12 m, grades from calcareous marls and marly limestones to sandstone near Bridgend where small potable groundwater supplies have been obtained. Typical yields range up to 8 l s<sup>-1</sup> in the Cardiff area where the water has a bicarbonate concentration of up to 500 mg l<sup>-1</sup>.
 
The younger Mercia Mudstone Group comprises massive red-brown dolomitic mudstones with gypsum either in veins or retained as nodules. The uppermost part of the sequence, the Blue Anchor Formation comprises grey dolomitic mudstones and siltstones, and the Penarth Group, which is nowhere thicker than 12 m, grades from calcareous marls and marly limestones to sandstone near Bridgend where small potable groundwater supplies have been obtained. Typical yields range up to 8 l s<sup>-1</sup> in the Cardiff area where the water has a bicarbonate concentration of up to 500 mg l<sup>-1</sup>.
  
 +
The Jurassic Blue Lias Formation is essentially an aquitard although seeps can occur where fractures intercept the ground surface at low elevations.
  
  
The Jurassic Blue Lias Formation is essentially an aquitard although seeps can occur where fractures intercept the ground surface at low elevations.
+
[[Category:Hydrogeology of Wales|Hydrogeology of Wales]]
</div> <div>Retrieved from ‘[http://nercbgskwxmediawiki/mediawiki/index.php?title=Hydrogeology_of_Wales:_Permo-Triassic_and_Jurassic_aquifers_-_South_Wales&oldid=8896 http://nercbgskwxmediawiki/mediawiki/index.php?title=Hydrogeology_of_Wales:_Permo-Triassic_and_Jurassic_aquifers_-_South_Wales&oldid=8896]’ </div>  <div>[[Special:Categories|Category]]:
+
 
+
* [[Category:Hydrogeology of Wales|Hydrogeology of Wales]]
+
</div>
+

Revision as of 15:36, 21 August 2013

File:DirectLinkImage
Triassic Blue Anchor Formation exposed in cliffs at St Mary's Well Bay, south of Penarth. P802431.

The Triassic strata that lie to the east of Porthcawl comprises marginal basal facies deposited in a shallow coastal environment (Plate P802431). Lithologies include sandstone, conglomerate and subordinate dolomitised limestone. The conglomerates do not crop out and have poor recharge potential.


The younger Mercia Mudstone Group comprises massive red-brown dolomitic mudstones with gypsum either in veins or retained as nodules. The uppermost part of the sequence, the Blue Anchor Formation comprises grey dolomitic mudstones and siltstones, and the Penarth Group, which is nowhere thicker than 12 m, grades from calcareous marls and marly limestones to sandstone near Bridgend where small potable groundwater supplies have been obtained. Typical yields range up to 8 l s-1 in the Cardiff area where the water has a bicarbonate concentration of up to 500 mg l-1.

The Jurassic Blue Lias Formation is essentially an aquitard although seeps can occur where fractures intercept the ground surface at low elevations.