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Forest of Dean 2011. North Lake District 2016. The fossils are preserved by pyrite/geothite which is thought to be due to pore waters permeating the specimen and envelopment by bacteria which create a covering over the outside of the carcass causing a micro-environment in which mineralisation of tissues can occur i.e. bacterial sealing . The talk was accompanied by superb photographs and SEM pictures of the fossils but also by the escapades that Bob and partners undertook in order to study them.

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Home | Mid Wales Geology Club | midwalesgeology.org.uk Reviews

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Forest of Dean 2011. North Lake District 2016. The fossils are preserved by pyrite/geothite which is thought to be due to pore waters permeating the specimen and envelopment by bacteria which create a covering over the outside of the carcass causing a micro-environment in which mineralisation of tissues can occur i.e. bacterial sealing . The talk was accompanied by superb photographs and SEM pictures of the fossils but also by the escapades that Bob and partners undertook in order to study them.

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1 about us

2 programme

3 sunday 8th april

4 read past news

5 dolomite / quartz

6 the silurian

7 read it now

8 publications

9 read them here

10 compendium

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Home | Mid Wales Geology Club | midwalesgeology.org.uk Reviews

https://midwalesgeology.org.uk

Forest of Dean 2011. North Lake District 2016. The fossils are preserved by pyrite/geothite which is thought to be due to pore waters permeating the specimen and envelopment by bacteria which create a covering over the outside of the carcass causing a micro-environment in which mineralisation of tissues can occur i.e. bacterial sealing . The talk was accompanied by superb photographs and SEM pictures of the fossils but also by the escapades that Bob and partners undertook in order to study them.

INTERNAL PAGES

midwalesgeology.org.uk

1

Member's Gallery | Mid Wales Geology Club

http://midwalesgeology.org.uk/member-gallery.php

A collection of images submitted by members of the group. These are pics of a Tetrapod Trackway on Valentia Island, South West Ireland, which is evidence of the first incursions of our vertebrate ancestors onto dry land, breathing air and walking on four limbs. (They are, of course, unrelated to "Dynosaur footprints", which came 100 plus million years later! These are some 385 million years old, dating from the Middle Devonian (Our Old Red Sandstone times). Other animals left traces too:. Assorted initia...

2

Long Weekend 2013 | Mid Wales Geology Club

http://midwalesgeology.org.uk/longweekend2013.php

Annual Summer Weekend - South Pembrokeshire 7-10th of June 2013. Orielton Field Studies Centre. Leader Sid Howells. There are also brachiopods (productids), solitary corals (Caninia), large crinoid ossicles and very large worm casts (Palaeophycus? Much discussion has not reached agreement, or even consensus. Some of the blocks are bus sized, some of rock crushed much finer. Welshpool's Geological Heritage Project. The Annual Long Summer Weekend. Land of my Fathers. Cone in Cone Nodules. Site designed and...

3

Annual Long Summer Weekend | Mid Wales Geology Club

http://midwalesgeology.org.uk/longweekend.php

The Annual Long Summer Weekend. On Nylands Hill, 2009 - Mendips. Charlie points out part of a duplex, a series of overlapping thrusts. The grey rocks here can be seen overlapping. 2004 - Pembrokeshire Coast. A chemistry lesson at Parys Mountain. The acidic water dissolves even motor cars, all except for the rubber tyres. 2005 - Anglesey. Very rarely we might get a wet day, but we don't mind! Searching for the unusual mineral riebeckite in the microgranite boss at Mynytho. 2007 - Lleyn Peninsula.

4

Events Programme 2016 | Mid Wales Geology Club

http://midwalesgeology.org.uk/programme.php

Events marked with the map icon are field trips. Day Field Trips are nearly always held on a Sunday. Unless otherwise stated, meetings start at 7:15pm (tea/coffee and biscuits) with talks at 7:30pm at Plas Dolerw, Milford Road, Newtown. AGM followed by a short talk by Roy McGurn - The Anthropocene: a new epoch in the making. Guest speaker: Prof. Jerry Davies - Sea level Change in the Geological Past: recognising the record in the rocks. Nesscliffe and the Shropshire Triassic Leader Tony Thorp. November 1...

5

Home | Mid Wales Geology Club

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Mid Wales Geology Club. Boots left behind at the local YHA. The famous Bowder Stone: not an erratic but a fallen block. Group at Derwentwater looking towards Castle Crag. Members at the Bowder Stone. Surface of granite pluton in River Caldew. Walking the Rosthwaite moraines. Our next event will be on Wednesday the 17. Of August, where guest speaker David Pannett from the Shropshire Geological Society will present his talk Glacial Features in the Severn Basin. 2016 Annual Weekend Field Trip Lake District.

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midwalesgeology.org.uk

Home | Mid Wales Geology Club

Forest of Dean 2011. North Lake District 2016. The fossils are preserved by pyrite/geothite which is thought to be due to pore waters permeating the specimen and envelopment by bacteria which create a covering over the outside of the carcass causing a micro-environment in which mineralisation of tissues can occur i.e. bacterial sealing . The talk was accompanied by superb photographs and SEM pictures of the fossils but also by the escapades that Bob and partners undertook in order to study them.

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