Apr 292011
 
Crinoid Fragments

Time to catch up on some blogging. For a start, I’ll go back to March 12, when myself and a group of volunteers from GeoConservation Staffordshire restored the exposure of the Milldale Limestone at Sparrowlee Cutting on the Hamps and Manifold Geotrail.


Before geoconservation

Before geoconservation

After geoconservation

After geoconservation

The restored cutting revealed a small thrust fault (climbing upwards to the right from the rucksack – above) and a localised pocket of crinoid debris (below) in the Milldale Limestone that probably haven’t seen the light of day since the Manifold Valley Railway was active in the in 1920s.

Crinoid Fragments

Crinoid Fragments

Location Map

Sparrowlee cutting, stop 28.

 
Rock Garden

Rock garden

This month’s accretionary wedge is being hosted by John Van Hoesen over at Geological Musings in the Taconic Mountains, who muses how geologists have incorporated geology into their homes, offices and gardens. My rock collection has been banished from the house and incorporated into an alpine rock garden at the front of the house, where a pocket-sized area on a steepish slope doesn’t lend itself to much else.

Rock Garden

The beauty of having a rock collection like this is that it brings back so many memories of places visited and geology seen.

Rock Garden

In this corner are the folds, including a flow folded rhyolite from Pembrokeshire, Wales and refolded folds from Loch Leven in Scotland. Behind are pegmatitic gabbro from Pembrokeshire, a gabbroic dreikanter from the Atacama desert from Chile, a water-lain tuff from the Lake District of England and a Welsh Old Red Sandstone conglomerate.

Rock Garden

Here are a siderite nodule from Pembrokeshire, blue john from Derbyshire, England, larvikite from Norway and rose quartz.

Rock Garden

Around the back, the acer has just come into leaf on the ‘pebble beach’. Most of the pebbles amongst the ferns and strawberry plants are actually glacial erratics collected from the local soil as we live on the edge of a glacial meltwater channel. They are mostly Triassic quartzite pebbles, but also include Carboniferous limestones and Lake District granites.

 
20110401Blackpool

The 2.2 Blackpool Earthquake was recorded at Keele University, Staffordshire. Our ‘Schools Seismometer‘ record had to be heavily filtered to get rid of the background noise.

We also had a Guralp 6TD recording and its record is here (with thanks to Sam Toon).

Information from the British Geological Survey.

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