gengiplötur

Gengiplötur, also known as gengiplata or gengiplatafjall, is a type of volcanic rock formation found in Iceland. It is characterized by its distinctive appearance, which consists of a series of steep-sided, cone-shaped hills or mountains, often arranged in a line or cluster. These formations are the result of repeated volcanic eruptions that occurred over a long period of time.

The term "gengiplötur" translates to "step plates" in English, referring to the stepped or terraced appearance of the rock layers. The formations are typically composed of basaltic lava flows, which are common in Iceland due to the country's location on the Mid-Atlantic Ridge. The lava flows solidify quickly upon contact with water or air, creating the steep-sided cones.

Gengiplötur are often found in the highlands of Iceland, particularly in the regions of Snæfellsnes, Snæfellsnes peninsula, and the Westfjords. They are a popular destination for hikers and nature enthusiasts due to their unique landscape and the opportunity to observe the geological processes that shaped them. The formations are also of scientific interest, as they provide insights into the volcanic activity and tectonic movements that have shaped Iceland over millions of years.