What is your favourite place to do field work?” is the question Dave Schumaker at Geology News is asking as last this month’s Accretionary Wedge.

I am extremely lucky having a job that allows me out into the field occasionally, even if at the minute it is just down the road. In my top five I would have to include the Atacama Desert of Chile, Iceland, Colorado and the Alps but at number one has to be the Spanish Pyrenees.


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I’ve been many times, as a postgraduate demonstrator and lecturer on undergraduate field courses and twice as a field assistant to a Ph.D. student. However, I’ve not been back in a long time, so apologies in advance for the scans of twenty year old slides.

The Spanish Pyrenees is a classic place to teach geology. The Spanish side (unlike the French side) is arid so there is excellent exposure, and, unlike the Alps, they are not too high and much of the geology is accessible from the roadside (with a suitable loose definition of road).

The geology shows a superb interrelationship of sedimentation and tectonics with the sediments eroded from the high Pyrenees being progressively deformed as the mountain front advances.

Riglos

Riglos 2

Turbidites

The variety of geology is also stunning from vertical bedding to trace fossils.

Vertical bedding

trace fossils

The local cuisine is excellent with chorizo, pyrenean mountain cheese and local wild boar washed down vino tinto. The only exception to this is breakfast (sweet cake is not my favourite at the best of times) but we did manage to train a cafe owner in Jaca in the art of bacon and egg butty making.

Of all the places in the Spanish Pyrenees I think my favourite has to be the Ordesa National Park. From the olistostromes at Torla to the climb up to Monte Perdido is the most spectacular walk I have ever done. The views from the top are absolutely breathtaking.

cylindro

ordesa

One day I shall return.

 

Keele Hall

A fine winter’s day on Keele University campus. This is Keele Hall, the ancestral home of the Sneyd family, whose estate now hosts Keele University.

So where is the geology angle I hear you ask? Well, first, the formal gardens in the foreground are the site of the first geology department at Keele. Keele was used a a base for American and Polish soldiers in the Second World War, with officers living in the Hall itself and the lesser ranks billeted in huts built around the grounds. After the war the Hall and huts formed the basis of Britain’s first post-war university. Two huts had been built where the formal gardens lay and one became the geography building, the other geology. Eventually the departments had new buildings built for them and the formal gardens were restored.

The grounds of the Hall, designed by William Emes, are still being restored and currently a series of lakes are being drained and de-silted. In the upper lake this operation has revealed a glacial erratic boulder.

Glacial Erratic

The site manager let me go an have a look at it (you can probably see my wellie tracks from the far bank) and hammer a bit off. It is a dolerite (or diabase for our North American cousins) boulder probably from the Lake District some 200km to the North.

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