Wednesday, 13 July 2011

Spain Rocks

By Richard Morley

The snow capped peaks of the Gredos mountains. Part of the "Sistema Central" of Spain's Mountains.

I wrote recently in my post about the source of the Manzanares river that today’s tranquil landscape had been, a long, long time ago, a rather turbulent place. That while today the pink, or Rose Granite lends a colourful hue to the peaceful slopes of the Yelmo, at the time of its formation it was a place of volcanoes and heaving rivers of lava. It’s a nice place today because it’s been a gneiss place for ages. (Geological joke! – Look it up.)

 A (very) close up picture of the rose granite through which the young Manzanares runs.

The Manzanares’ source lies in the Sierra de Guadarrama, part of the central system of mountains that stretches from Portugal to just north of Madrid, incorporating the sierras of Gredos, Avilla,  and Guadarrama (among several others) and delineates the divide between northern Spain and the south. In geological terms they are quite young mountains. A famous mountaineer, when asked why he wanted to climb a mountain said, “Because it is there”. Me, I want to know why.

 The Iberian "Sistema Central" mountains running more or less West-East until terminating at the perpendicular Iberian system, formed 40 million years earlier when Spain faced in another direction.

Today we tend to think of dramatic geological events in terms of unpronounceable Icelandic volcanoes and havoc inducing tsunamis. That’s because they happen quickly; over days, or even hours. Most geological events happen much, much slower. For us, and the world in general, that’s a good thing. For Spain, it has been a blessing. The country that we know and love has taken a very long time to reach it’s present state. It has travelled – and will continue to do so. It has been subject to amazing forces – and still is. Geology has shaped the world and shaped us. We respond to our surroundings. Geologically, the country went it’s own way for eons. Historically, it did the same. Perhaps this says something about the tenacious spirit of the Spanish, of their, sometimes, fiery “carácter” , but also their more often seen tranquil nature.

Weathered peaks of the Pedriza in the Guadarrama mountains.

Let’s see the events unfold. (But in a really, really simplified form. I don’t want comments telling me that I have forgotten such and such an event. As an old tee-shirt of mine once said, “Geophysicists do it deeper!”, but here I am just scratching the surface.)

Cast your minds back to, oh, let’s say, 600 million years ago. We will have to speculate a bit. I’ve attempted to do the research, but, as I have discovered in a long career in one particular branch of earth studies, if there is one thing that geologists can’t agree on – it’s EVERYTHING! So, there are competing theories. Quite a few of them have had to be formulated relatively recently. After all, it’s just exactly one hundred years since Alfred Wegener,  noticing how the coastlines on opposite sides of the Atlantic fitted together like pieces of a jigsaw puzzle, published the first paper on how the world’s landmasses seemed to drift across the Earth’s surface. Perhaps because he was an astronomer and meteorologist and not a geologist many did not take his ideas seriously. Plus, there were competing theories (the discredited “expanding Earth”) and the fact that there seemed to be no driving mechanism behind the continental movements. They were still arguing about it in the early seventies when I was a student.

But it seems to go a bit like this. Prior to 600 million years ago the World’s landmasses had been forming and reforming into groups until on almost opposite sides of the globe two super continents, one called Gondwana and the other Laurasia, had come into being. Slowly they drifted together and at about 600 million years ago they met and formed the giant extra-super continent, Pangea.

Pangea looked like a letter C, or a very distorted 8. A bit like a knobbly Pac man figure facing right, it’s mouth agape. But think of the 8, bent into a C shape. Where the two halves of the 8 meet, or perhaps where Pac man’s tonsils could be, were a few independent landmasses which had been crushed together and bridged the gap between the two continents. They are known as the Avalonian, the Amorican, and the Iberian plates. You might like to bear in mind the “Iberian” plate. It’s sort of important in this article!

To the east, ie, within the Pac man’s gaping jaw, lay the Tethys sea.

Then several things happened. Firstly, the pressure of Gondwana pushing up into Laurasia compressed bits of the northern continent and pushed them upwards, forming mountains. Today, these mountains are so eroded it’s not easy, except by using reflective seismic techniques, (a bit like sonar on land) to find the evidence, but some can be found in Spain’s north west, on its corner with Portugal, in south east Galicia.

As the southern continent pushed against Laurasia, it subducted, meaning it slid underneath. This, as today can be seen around the Pacific’s rim, leads to volcanic activity. This can be seen in ancient volcanoes found in Spain’s northeast, but in the centre, where the Iberian plate was thin and weak, a great intrusion of magmatic rock oozed to swell into a huge globule of granite. It is as if the rivers of fire from hell rose to the surface and, in fact, we call that action “Plutonism”, named for Pluto, the ancient Roman god of the underworld. That’s what I was gazing at in the last post. But 600 million years ago it didn’t break the surface, so at the time there was little evidence of what was going on below. On the Avalonian plate, however, there was huge amounts of violent volcanic activity, which had already been going on for 100 million years and would continue for another 100 million.

Moving forward in time this volcanic activity would lead to a splitting of the left hand side of Pangea. (Incidentally, I write of left and right rather than east or west, north or south, because even though geologists speak of “Laurasia”, “Amorica”, even “Euro-America”, those land masses were nowhere near their present geographical locations – and after which they are named. (Laurasia became, after the splitting off of north America, Eurasia.) All of what I am writing happened when these land masses where deep in the southern ocean. Spain at that time was thought to be around 55º south of the equator and probably not in its current orientation relative to north and south. Events are hard to construct from the historical carousel of continental drift. But not impossible.)

But I digressed.

The splitting off of the left hand side of Gondwana led to the formation of South America. Parts of Avalonia are found in the British Isles south of Scotland and continue through northern Europe. Other parts are found in eastern Canada, from where it took its name from the Avalonian peninsular in Newfoundland.

For the next 250 million years the great continent drifted northwards. 450 million years ago the Tethys sea began to close. So, as Pac man’s mouth slowly closed, the land mass of Laurasia turned clockwise. In the middle of this upheaval the two plates of Iberia and Amorica thrust together. Amorica is the land mass where today you find France, and you will think that Iberia and France, were, from that moment on, like co-joined twins tumbling around in the centre of global activity. But wait, there’s a twist, very literally, to their tale. But that’s for later. Right now, well 450 million years ago, extensive mountains were being built by the squeezing of the plates. The remains of this mountain building can be found today in Portugal, Galicia and Northern France. (Remember that little fact!)

Meanwhile Iberia and Amorica were passing though tropical regions. During this time they became great jungles of vegetation which died and their remains laid down in great belts of carboniferous strata. That’s coal to you and me. The coal is found in seams between layers of limestone and sandstone showing that the landmasses were alternately above sea-level (and covered in trees) and below sea-level, where oozing sand from eroding land and the shells of sea creatures created intervening limestone and sandstone strata. The bodies of those sea creatures, the soft parts, decomposed to give us oil. The great explosion for this was after the carboniferous, mainly during the Triassic and Jurrasic periods.
 Limestone strata found in the Cordillera Iberica near Soria in northeast Spain.

It was in the Jurrasic, around 180 million years ago, that Pangea began to split up. The Tethys sea was closing rapidly. The Indian plate was sliding across to bump into asia. The Antarctic plate, with Australia and New Zealand still attached headed southward. They didn’t have far to go! The major landmasses were still travelling northwards. Laurasia, soon to become Eurasia with the loss of North America, was revolving clockwise. What was left of Gondwana, basically Africa, was continuing to push north and the two joined landmasses of Armorica and Iberia were rolled anti-clockwise and to the left between them.

The theory of much of what I have written is pretty common knowledge these days. The Discovery channel and others present documentaries about how these giant plates; the Pacific Plate, the African Plate and so on, are rolling around the earth. These giant plates are, in fact, “cratons”, meaning they are composed of lots of smaller plates that seem to have permanently joined together; the completed parts of a jigsaw puzzle, if you like. It is where the constituent plates rub against each other that we get seismic activity like earthquakes and volcanoes.

Iberia swivels under France to open up the Bay of Biscay.

For many millions of years the Amorica-Iberian landmass had formed a bridge between Northern Laurasia and Southern Gondwana. About 120 years ago they made their choice and Amorica, with its twin, became a craton of Eurasia. But the forces that had split North America away, first a volcanic rift then the spread of the Atlantic ocean, were pulling on Iberia and the clockwise motion of Eurasia was pulling on Amorica. Eventually they swung apart, but hinged at their southern extremity. This is the, literal, twist in the tail. As Amorica moved north and clockwise, Iberia twisted anticlockwise under it. The resulting gap opened to become the Bay of Biscay and about 65 million years ago, when the Iberian swing terminated by crashing into  southern France, the beginnings of the Pyrenees were formed.

 NASA photograph of the Pyrenees. Notice the compression folds as Iberia was pushed into Armorica.

A glance at the geological map above shows the continuation of the north-south oriented western Iberian mountains continuing oriented east-west in Brittany and Normandy in northern France. Geologists have used paleomagnetism, a technique that indicates the original  magnetic orientation of rocks when they were formed.  I used to think the similarity between those two parts of Europe was their love of cider, but it obviously goes much deeper – and further back – than that!

Europe basically had now taken the shape we are familiar with.

But things did not stop there. Africa, divested of south America, India, Antarctica, continued, and continues, to move north, still pushing into Europe.  With Europe now more or less in its current position this northern movement of Africa exerted such pressure that ridges of mountains were formed all over the place. The mechanism is known as the “Alpine Orogeny” (mountain building) and, obviously, the European Alps are its main manifestation, but it is responsible for the rolling south downs of England, the Apennines in  Italy and the Atlas mountains in Morocco, Algeria and Tunisia. In Spain this action is responsible for the Cantabrian mountains, including the Picos de Europa in Asturias and the Sierra Nevada in Andalucía.

 The black lines represent the fold lines, showing how Iberia was squeezed while the plate rotated in its travels.

Squeezed at both ends the centre of Spain buckled like a sheet of paper. Mountain ranges rose, then collapsed. There is evidence that much of this time was spent below sea-level, with the peaks of the ranges existing as island chains. Signs of this are shown in layers of sedimentary rock around the slopes of the Guadarrama chain in the central system, but not at their summits. And the “Plate” of Iberia is also a craton, made up of smaller plates. It is through such a gap between plates that the Granite mass of the Pedriza finally pushed its way to the surface – and beyond – around 25 million years ago – hundreds of millions of years after it originally formed.

 Elevation model of the central system and it's location on a general map of the Iberian peninsular. Notice how the land is raised higher to the north of the mountain range.

The Tethys sea had completely closed up at its eastern end by the land masses of India and the Arabian plate, what we now call the middle east. What’s left of that early sea is the Mediterranean. By any standard the Mediterranean is a substantial body of water. It has a surface area of 2.5 million square kilometres, an average depth of 1500 metres. It nearly 3000 kilometres from end to end and around a thousand wide, not including its sub seas; the Adriatic, the Aegean and so on. It borders 21 countries and has many important sea routes.

Imagine it empty.

Slightly less than 6 million years ago that happened. In an event named the “Messinian Salinity”,  after the city of Messina in Sicily. Africa’s relentless push actually closed the access of the Atlantic through the straits of Gibraltar. Within a thousand years, apart from a few very salty lakes, some more than 3Km below present day sea levels, the Mediterranean was dry. And it stayed that way for nearly 700,000 years! The fossil record shows evidence that animals used the dried up sea bed to migrate between the two continents.  The mineral record, achieved by studying core drilling samples show typical shore line mineralogy from the sea bed hundreds of kilometres from modern day shorelines.

Almost as abruptly, in geological time-speak, as it had begun, 5.3 million years ago, due to yet more geological shifting, waters once again poured through the straits in an event called the Zanclean Flood. Zanclean is the name geologists give to that era which begins the modern geological age. Geological studies show that the straits of Gibraltar were not the only water course open. There was one through Morocco and another across the Betic Plain, around modern day Seville. (Think Betis football club!)

 These carried water of a much higher volume than is carried over Niagara Falls today, and over a drop of several kilometres. Some scientists have proposed that the rate of flow was as much as a billion cubic metres per second and the Mediterranean refilled in as little as a few months to two years, with water levels rising ten metres a day. (To compare: Niagara’s rate of flow is just under 2000 cubic metres per second.) However, Niagara’s waters come from the narrow confines of the Niagara river, the waters pouring into the Mediterranean had the force of the entire Atlantic ocean behind them.

Of course, that was not the end of Spanish seismic activity. Since written records began there has been a long history of seismic destruction. To mention the more famous – or infamous, there is the Lisbon earthquake of 1775. It struck in the morning of All Saints day, November the 1st. Its six and a half minute duration caused huge fissures to open up in the city centre and the sea water receded from the harbour revealing long forgotten wrecks.  Forty five minutes later the water returned as a tsunami. Estimates tell of between 60,000 to 100,000 dead and the complete destruction of the city.

 These staples were used to repair a crack in the Church in La Alberca, Salamanca. The crack opened after shock waves from the Lisbon earthquake reached the town. La Alberca is some 330 km distant from Lisbon.

In 1884 the town of Arenas de Rey was struck by an earthquake reckoned to be around 7 on the Richter Scale. Eight hundred people were killed and a further 1500 injured. 14,000 homes were destroyed.

I take no joy from the fact that, following reading a few reports, I posted on my Facebook page on May 1st this year that Spain could expect a major earthquake “soon”. Twelve days later the town of Lorca was rocked by a severe earthquake that killed eight, injured many and rendered many families homeless.

Earthquakes, having been part of my life for so many years, means that I often get asked to speak about them. By coincidence, I was doing just that on the 12th of August 2007 when news came in that there had been a mild(ish) earthquake in Ciudad Real.

I shouldn’t have been surprised. I monitor the website of the Spanish geographic institute which reports on all quakes around the Iberian Peninsular. You can see it here

That’s the downside of living on top of active geology. The advantages have been enormous. Spain’s mineral wealth is huge. The chemical reactions that occur within molten rock produce some useful stuff, like gold (4000kgs annually), silver (20,000kgs annually), feldspar (600,000 tons annually – that’s what all that granite gives you, as well as expensive kitchen tops) and of course historically Spain has been the world’s number one producer of Mercury from the mines at Almadén, which have produced 250,000 tons since Roman times.

The carboniferous era laid down coal in Galicia and Asturias. Current reserves suggest there is 530 million tons waiting to be mined, but apparently the work there is difficult. The damned geology gets in the way! Erosion of rock over the millennia has led to Spain being pretty much self-sufficient in sand and gravel, and the limestone deposits means that cement production is nearly all home grown. Years of shallow submergence, particularly during the Messinian salinity has given Spain untold quantities of gypsum. If you look at the map of the Messianian refilling above you will see the town of Sorbas marked. The Mediterranean used to flood and then recede in this shoreline area, leaving behind each time more minerals, known as evaporates (for obvious reasons), including gypsum,  that would later be mined. Used in building everywhere (plaster walls and ceilings, fairground plaster of Paris statuettes!) Spain is Europe’s largest producer and the second largest in the world.

There’s iron, bauxite, and a long list of other minor stuff. Not much oil sadly. Some oil shale which kept the power stations of Spain running for many years  and a small field off the coast of Cantabridgia.

And all that mountain building has given Spain super fertile slopes for grapes and olives, not to mention the skiing. After Switzerland, Spain is the most mountainous country in Europe.

The continents will keep moving. Some think that Iberia will become so squashed by Africa’s relentless push that it will be squeezed out into the Atlantic like a geological zit. Perhaps it will become an island drifting who knows where. I read one report that suggested in 30 million years it will be somewhere near where Iceland is now. That’s a long time. You don’t have to pack the winter wear just yet, but enjoy the ride!

Just as a serendipitous postscript I was amused to find a shop specialising in "Geological Jewellery" (if there is such a thing!). Many long eJstablished businesses like to boast of their year of foundation. They are never going to beat this place.   
Find decorative geodes, fossil fashion, minerals and meteorites 72, C/Hermosilla. (Near Goya metro.)


  1. Richard: Great explanation. When we were in Nepal in April we had a retired geology professor who told us of similar things to explain the Himalayan mountains and all of the rocks they have in Nepal. And how the Indian plate pushing north is continuing to push up the Himalayans (if I remember correctly). As always, thanks for an interesting read and further education about Spain.

  2. Amazing shots! Thank you for sharing this article about rocks in Spain. I hope I will experience climbing those rocks someday. Have a great day!

  3. Interesting, as always. I don't know how you find the time to put so much effort and research into your articles.

  4. Thanks you for sharing this wonderful and helpful article. I appreciate you making this article available. Have a great day! Marie Greenhalgh