On Shaky Ground

2015 Map of Geological Fault Lines of Ireland
The Major Geological Fault Lines of Ireland

The large earthquake in Nepal this last week has been terrible for the people there, but most of us don’t know that in Millstreet, we actually live on a major fault line that was once as active as the any in the world. Referred to as the Killarney-Mallow Fault (KMF), it stretches from the Iveragh Peninsula in Kerry to the other side of Mallow and is the point where two continents were colliding. It is a reverse and thrust fault, and it resulted in folding of the rocks that created all the mountains of south of here.

This all happened 270 million years ago, so thankfully we get no serious earthquakes these days. The mountains were once almost three times as large, but they have since been weathered and scoured by glaciers during the ice ages, down to their current shapes, while the valleys have been filled in with debris.

Below are detailed maps and explanations and links to further detail: ==========

from CORK_GEOLOGY: Approximately 270 Ma during the Permian period a mountain-building event called the Variscan affected the rocks in Co. Cork. Two continents collided and the rocks were folded into a series of ridges (anticlines) and valleys (synclines) that have an east-west orientation. Across the ridges erosion as removed the younger rocks to expose the Old Red Sandstone while in the valleys the younger Carboniferous rocks still remain. By and large the rivers in Cork flow along the limestone synclines and in the west they have been drowned by seawater to form rias.

Geological Faults and Bedrock around Millstreet
Geological Faults and Bedrock around Millstreet (2006) – from Rathmore to Banteer and down to Carriganima (click the image for further detail). [ref] The blue strip is limestone. generally above that line the bedrock is of Shale and Sandstone, while below that is green/grey sandstonie, while Kilconey / Banteer have Old Red Sandstone.
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Fault Lines and Bedrock around Millstreet Town
A deatiled look at the geological Fault Lines and Bedrock around Millstreet Town. One fault line passes under the Bridge & Green Glens, while another passes under Tanyard Wood.
1859 Geological Survey of Millstreet - map
1859 Geological Survey of Millstreet by the British. the blue strip is limestone, the red is sandstone, the grey is of coal measures. Fault lines are white, and the yellow is alluvial fill. These surveys were concerned on coal & minreal extraction.
1882 Geological Survey of Millstreet - map
1882 Geological Survey of Millstreet by the British. It seems a bit more detailed than the 1859 survey. the blue strip is limestone, the red is sandstone, the grey is of medium coal measures. Fault lines are white, and the yellow is alluvial fill.
Probable Formation of Mountains south of the Killarney Mallow Fault Line - Meeke
Meere (1995) suggests that the fault line is caused by changes in stratigraphic thickness, and by a much harder rock (granite) down deep which forced the earth moving up from the south to buckle essentially make mountains

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Bits and Pieces:

  • The fault is referred to in places as the Killarney-Mallow Fault, and appears to be part of a longer line from Dingle to Dungarvan.
  • The maps are not entirely perfect. When reseeding one field in 2002, there was a very distinct dividing line down through the field – on one side a light red, and on the other side, a darker browner soil. one of the boundaries between soil types above runs through that field, bue in a slightly different spot/angle.
  • There have been no earthquakes locally in modern times (are we due one?). Update: actually an earthquake was reported in the Mallow / Kanturk area in 1868: “evere shocks of earthquake,
    followed by a loud rumbling noise, were felt at two places near Mallow, in Cork county. It is stated that houses were much shaken, furniture was broken, and the occupants of the houses were greatly terrified. “(reported in the Aberystwyth Observer, 31 October 1868)
  • The great Lisbon Earthquake of 1755 was felt along the Mallow-Killarney Fault line.
  • There has been much agreement & disagreement on the fault, but because  it all happened in the past we probably will never know.
  • I wish we had been taught local geology like this in school !
  • The old red Sandstone of parts of suoth west Cork and south Kerry is from a time when the area was closer to the equator and which were large sand dunes – part of a large desert.

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Links:

 

 

1 thought on “On Shaky Ground”

  1. Congratulations Michael on your excellent article.Local geology is a core section of Transition Year Geography in Millstreet Community School..vital that students appreciate the unique geology of western Duhallow.

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