The Sierra Nevada mountain range in Andalusia is a section of the Betic Cordillera and runs parallel to the Mediterranean sea for around 100km.
The temperature range is dramatic with the summits under snow for many months, followed by a hot Mediterranean style summer. This creates special microclimates across the exposed rocky summits, glacial lakes, sheer sided gorges, mixed oak woods, pine woods and fast rivers with wooded banks.
Declared a National Park in 1998 and encompassing an area of 86,208 hectares it is a popular destination throughout the year. It holds an exceptional variety of animal and plant life due to the combination of altitude and its proximity to the Mediterranean sea.
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These mountains were formed during the Tertiary Period (65 to 1.8 million years ago), at the same point as the Atlas Mountains in Morocco and the European Alps. This mountain building event is called the Alpine Orogeny. The uplift happened as the African plate moved northwards colliding with the Eurasian plate. The Sierra Nevada mountains consist of mainly metamorphic rocks such as Gneiss and Mica schist. Many of the rocks are juxtaposed and mixed up due to intense faulting and folding during the compression of the two tectonic plates.Continue reading The Sierra Nevada mountain range in Andalusia