— Ch. 1 · Stone And Sea —
Öland.
~4 min read · Ch. 1 of 6
The island of Öland stretches across the Baltic Sea, separated from the mainland by the Kalmar Strait. It covers an area that makes it the second-largest Swedish island while remaining the smallest traditional province in the nation. Over 26,000 people call this land home today. The landscape is defined by a unique limestone pavement known as Stora Alvaret. This geological feature dates back to the Ordovician period between 540 and 450 million years ago. The bedrock beneath consists mainly of Cambrian sandstone and alum chert. A specific trilobite species named Eccaparadoxides oelandicus was discovered here and named after the island itself. The climate presents considerable temperature differences between summer and winter. Air warms over surrounding landmasses during the day but retains heavy maritime features at night. Two main weather stations monitor these conditions on the northern and southern edges.
Ancient Graves
Archaeological evidence indicates the island was settled about 8000 BC. Settlers from the mainland migrated across an ice bridge that connected the island during the early Stone Age. Habitation occurred at least as early as 6000 BC when Stone Age settlements appeared at Alby. Burial grounds from the Iron Age through the Viking Age remain visible at Gettlinge and Hulterstad. These sites include stone ships along the perimeter ridge. Nineteen Iron Age ringforts have been identified on the island. Only one, Eketorp, has been completely excavated so far. That single excavation yielded over 24,000 artifacts for researchers to study. Around 900 AD, Wulfstan of Hedeby referred to the island as Eowland. Earlier mentions exist in the Anglo-Saxon poem Widsith regarding the tribe known as the Eowans. Scholars point to a possible mention by Tacitus in 98 AD calling them the Aviones.