Going on my adventurous trip to Reykjavic, I have captured some of the immense beauty of Iceland, visiting certain places like Gullfoss Waterfall, þingvellir (Thingvellir) and one of the geysers named Strokkur, these attractions are all within The Golden Circle.
The Golden Circle is a popular tourist route in South Iceland, covering about 300 km looping from Reykjavík into central Iceland and back. The three primary stops on the route are the national park Þingvellir, the waterfall Gullfoss (meaning "golden falls"), and the geothermally active valley of Haukadalur, which contains the geysers Geysir and Strokkur. Though Geysir has been inactive for a long time, Strokkur, on the other hand, continues to erupt at every 5-10 minutes interval.
The tectonic plates whose turbulent interactions formed Iceland, are the Eurasian tectonic plate and the North American tectonic plate. Spanning the Mid-Atlantic Ridge, Iceland emerged as a result of the divergent, spreading, boundary between these two plates and the activity of Iceland´s own hotspot or mantle plume. As the plates moved apart, excessive eruptions of lava constructed volcanoes and filled rift valleys. Subsequent movement rifted these later lava fields, causing long, linear valleys bounded by parallel faults. The divergence of the ridge started in the north about 150 million years ago and 90 million years ago in the south. These movements continue today, accompanied by earthquakes, reactivation of old volcanoes, and creation of new ones. Iceland is the largest island on the ridge because of the additional volcanism caused by the hot spot beneath the country, which moves slowly towards the northwest.
Iceland is one of the most dynamic volcanic regions in the world. Shaped by fierce natural forces, straddling the Mid-Atlantic Ridge where the activity of divergent tectonic plates brings heat and magma closer to the earth´s surface, Iceland holds enormous geothermal resources.
Informational sources: www.icelandontheweb.com
