90% of Europes's natural slate used for roofing originates from the slate industry in Spain,[1] with the region of Galicia being the primary source of production.
Slate is a fine-grained metamorphic rock that splits into thin, smooth-surfaced layers. Metamorphic rock is rock which was once igneous or sedimentary and has been subsequently subjected to heat and pressure in varying degrees thereby altering its composition, structure and appearance. It is used extensively in the building industry, particularly for roofing tiles. The production of slate is estimated at 4 million tons per year.[2]
Galicia is situated on the North West coast of Spain, just above Portugal, and is subdivided into the four provinces of A Coruña, Pontevedra, Lugo and Ourense.
The main areas of slate production are:-
See main article: History of Galicia.
The early history of the region has been shaped by a variety of key cultures and influences:-
4500 – 1500BC The Megalithic culture was the first major influence in the region. They were noted for their skills in construction and architecture, and the remains of thousands of tombs (or dolmens) can be found in the region.
1500 – 700BC There was a substantial increase in trade with the rest of Europe during the Bronze Age, prompted largely by developments in metallurgy.
800 – 500 BC During this period the region was heavily influenced by Celtic culture, and caestros (circular fortified areas atop a hillside, surrounded by a moat) became a common sight.
137BC The first Roman to enter the area was Decimus Junius Brutus.
410AD Galicia fell to the Suevi (or Suebi) German tribe, following the fall of the Roman Empire, and they formed the first post Roman medieval kingdom in Europe.
584AD Galicia was invaded by the Visigothic King Leovigild
711 – 718AD The Moors attempted to gain control over Galicia, as they had done the rest of Spain, but with little success.
739AD The Moors were defeated by Alfonso I of Asturias and Galicia became integrated into the kingdom of Asturias
835AD Relics said to originate from the Apostle St James (James, son of Zebedee) were discovered in Santiago de Compostela, and the area became one of the most important pilgrimage sites in the Christian world. This remains one of the heritage sites for which the region is renowned even today.
The Northern region of Spain has been subjected to periods of magmatic activity with volcanism, and this has led to the region's unique geological development in respect of slate.
Slate deposits are over 500 million years old, having been formed during the Cambrian, Ordovician and Silurian periods of the Palaeozoic era.
Essentially, slate forms when the clay minerals in shale are put under increased pressure with high temperatures. The clay starts to revert to the mica minerals which cause the rock to grow hard with pronounced cleavage) directions. It is this cleavage which enables slate to be broken along flat, even planes.
A large variety of colours and textures of slate can be produced, and the final product depends largely on the tectonic environment, the source of the sedimentary material, and the physical/chemical conditions prevalent during the sedimentation process.
As the sedimentary deposits were compacted, water was squeezed out, hence turning clay minerals into mica, and then solid mudstone. The subsequent mountain building compaction which occurred over the next few million years resulted in an even stronger rearrangement and planar orientation of the minerals. This means that in true slate the cleavage plane is very different from the original bedding plane[4] and led to the well developed cleavage for which the region is famous.[5]
The Galician slate industry is a major employer in the region and in the main slate is extracted from surface quarries. The process is as follows:[6]
Since slate is a naturally occurring product, different kinds of slate are subject to varying chemical and mineral compositions, determined largely by the geological characteristics of the quarry from which it was mined.[7]
An important use of Spanish slate is as a roofing material, often being specified by building professionals as a result of its aesthetic appearance and durability characteristics. Slate is particularly suitable as a roofing material as it has an extremely low water absorption index of less than 0.4%. Its low tendency to absorb water also makes it very resistant to frost damage and breakage due to freezing.
The nature of slate as a natural organic product results in a wide variety of qualities being available worldwide. An important way of determining the differences, and degree of quality, is through the use of country certification, or quality marks.
The CE mark certifies that a product has met the EU requirements for consumer safety, health and environmental issues.[8] All Spanish Slate bears this mark.
There are further national and international standards that can be applicable to slate, and give information as to the quality levels reached. Some of these are:-
Typically Spanish slate tiles are fixed using a hook fixing method, as opposed to the more predominant nail fixing used elsewhere in the world. The benefits of hook fixing are [11]
Dr Joan Walsh, a consultant geologist, writes in her article “Natural Slate: a Green Roofing Medium”,[12] that natural slate offers strong benefits over other roofing materials in terms of carbon emissions and reduced environmental impact.
In addition, the quarrying of Spanish slate does not involve any chemical processes, and usually only local water is used to keep cutting machinery cool.
After quarrying regional authorities often dictate that the landscape is returned as much as possible to its original state, and waste rock left as part of the extraction process is returned adjacent to the quarry. But often waste rock is abandoned near small villages, riversides or even burying many historical heritage sites.[13] [14]