The Siljan Ring is a prehistoric
meteorite impact structure located in
Dalarna County, central
Sweden, formed approximately 377 million years ago during the Late
Devonian period by an
asteroid collision that created one of the largest known craters on
Earth, measuring
about 52 kilometers in diameter and ranking as Europe's biggest impact feature.[1][2]The structure, now heavily eroded over geological time, features a slightly elevated central uplift surrounded by a ring-shaped
graben depression that encompasses several lakes, including the prominent Lake Siljan—the largest
body of water in the region—and Lake Orsa, connected by a narrow river.[2] This topography remains visible from
satellite imagery, highlighting the crater's circular outline amid forested and rural landscapes.[3]Geologically, the Siljan Ring formed in ancient I-type granites dating back 1,700 million years, with the impact event causing extensive fracturing, shock metamorphism, and the emplacement of impact melt rocks like pseudotachylite and vein quartz.[4] Deep drilling efforts, including a 6.8-kilometer borehole in the 1980s at the Gravberg site, have revealed a vertical profile through these granites interspersed with diabase sills, evidence of post-impact hydrothermal activity with fluids heated to 100–300°C in the upper 2 kilometers, and
deeper fracture zones indicating water penetration up to over 6 kilometers.[4] Earlier exploratory drilling in the late 1960s provided initial insights into the subsurface, uncovering fractured rocks potentially habitable by ancient microbial life.[2]Scientific studies have further illuminated the site's significance: a 2019
analysis of drill cores identified microbial
methane accumulation from hydrocarbons in matured
shale source rocks, mobilized by subsurface
bacteria.[5] More recently, in 2021, researchers discovered fossilized fungi dating to about 39 million years ago at depths exceeding 500 meters, indicating that the crater's fractures have supported eukaryotic life in the
deep biosphere over tens of millions of years.[6]
In 2025, investigations revealed unexpectedly high natural methane emissions from the Siljan Ring lakes—up to 300 times greater than typical freshwater systems at certain hotspots—puzzling scientists and raising concerns about underreported greenhouse gas contributions from such geological features.[7] These findings underscore the Siljan Ring's role in understanding ancient impacts, deep biosphere dynamics, and modern environmental processes.