Rauðaskál

Background

History & Background

Rauðaskál, literally translating to 'Red Bowl' and commonly referred to as the 'Apple Crater,' is a volcanic crater formed through explosive eruptions in Iceland's geologically active past. Its distinct red and orange hues are a result of oxidized iron in the volcanic scoria, while the vibrant yellow-green is attributed to mosses that have colonized the nutrient-rich volcanic soil over time. Situated in the southern Icelandic highlands, Rauðaskál is a prominent feature within a region known for its intense volcanic activity. Its proximity, just 6 km, to the formidable Hekla Volcano, often called the 'Gateway to Hell' in medieval times, underscores its position in a landscape shaped by powerful geological forces. This area is a prime example of Iceland's continuous formation on the Mid-Atlantic Ridge, where new land is constantly being created. While specific dates for Rauðaskál's formation are not widely detailed in common records, its morphology and fresh appearance suggest a relatively recent formation in geological terms. Its significance lies not only in its striking visual appeal but also as a living laboratory for understanding volcanic processes and the subsequent colonization of new land by pioneering plant species like mosses, making it a captivating site for both geologists and nature enthusiasts.

Rauðaskál is a volcanic crater in the Hekla area, distinguished by strongly coloured scoria and other volcanic material on its slopes. The informal nickname 'Apple Crater' appears in some travel descriptions but is not necessary to understand the site. Access is through exposed highland terrain where road and weather conditions can change quickly, so current conditions should be checked before travel.