Showing posts with label geology. Show all posts
Showing posts with label geology. Show all posts

Tuesday, 9 August 2011

9th August 2011 - 1 Moeraki Boulders in New Zealand

Inspiration

A photograph that caught my eye this morning on Google+ was a picture by . My initial reaction was "Whoa, that's amazing!" It's a lovely image in soft pastels of something I've never seen before. Fortunately Mr Sojka gives some background to his shots and explains that this is a broken Moeraki boulder on the Otago coast of New Zealand. I don't know the scale of the boulder from the shot, but it looks quite large to me. Quite how such large boulders could be just sitting there on the beach puzzled me so to google I went.

Description

The picture below shows unbroken boulders. Moeraki boulders are roughly spherical and up to 3m in diameter. They are covered in cracks called septaria.
Moeraki Boulders at Sunrise by Karsten Sperling via  Wikipedia Commons

Formation

Not to scale!
The Moeraki boulders started to form  in mud on the sea floor 60 million years ago. They are thought to have formed from the inside outward by the depositing of layers of mud, fine silt and clay which was them cemented together with calcite. Over 4.5-5 million years, they continued to grow while marine mud was deposited over them.

The cracks which taper off from the centre to the outer layer are taken as evidence that the surface was more rigid than the softer inside and so could not shrink as much. This is attributed to the differing amounts of calcite in the different layers.

There are several suggestions as to why the cracks formed:
  • dehydration of clay rich, gel rich or organic rich cores,
  • shrinkage of the boulder's cenre,
  • expansion of gases produced by decaying organic matter,
  • brittle fracturing or shrinkage of the interior by earthquake or compaction.
These cracks fill with brown or yellow calcite and, more rarely, quartz and ferrous dolomite when a drop in sea level allowed fresh groundwater to flow through the mud surrounding them.

They are exposed when the softer surrounding mudstone is eroded by the elements.

Sources

  1. AA Travel -Moeraki Boulders
  2. The Dinosaur Egg Boulders of Moeraki - Photos
  3. Wikipedia: Concretions
  4. Moeraki Boulders
  5. Trifter: Moeraki Boulders, South Island, New Zealand
  6. Wikipedia:Moeraki Boulders
  7. Encyclopedia of New Zealand - Moreraki Boulders

Thursday, 14 April 2011

14th April 2011 Weather and Earthquakes

Over a period of 10 million years, the Indian plate has increased its speed by 20%.  Scientists have created a model to explain this. Erosion from the monsoons has battered the eastern Himalaya Mountains which has lightened the load on that side of the plate.  This has caused the plate to rotate.

Discovery Magazine