Introduction:
East of Reykjavik lies a mountain named Hengill. Hengill was formed from a Palagomite tuff and its highest point is around 800 metres above sea level. Hengill is a central volcano and has a giant magma chamber beneath it.
Fact:
Columnar jointing is always a joy to observe in rocks in the field. Stumbling upon perfectly geometric columns of rock can only be described as magical. Even the most austere scientist might find herself (or himself) gaping in awe at the flawless shapes and wondering if men or Gods carved those immaculate columns.
Getting there:
The south coast of Iceland has so much to offer you. We start by driving south on Highway 1. We explain to you the geology of Iceland and show you many of the amazing and exciting places that have emerged in Iceland in both the past and present.
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