Finnish impact structures11 impact structures (or craters) have been found in Finland so far. Impact structures are form when an asteroid or a comet collide with the planet Earth with cosmic speed (11-70 km/s). Kinetic energy of the projectile transform into pressure- or shockwave in fraction of second. In the impact point the target rock and the projectile will vaporize, melt and brecciate. Impact will produce a crater, which is 20-30 times larger that the impacted projectile.
Structure name Diam. km Age Ma Lat. Long. Lappajärvi 17 (17-23) 73.3 ±5.4 63°09'N 23°42'E Sääksjärvi 5 543 ±12 61°24'N 22°24'E Söderfjärden 5.5 (5-6) ~560 (540) 63°00'N 21°35'E Iso-Naakkima 3 (2-3) ~1200 (900-1200) 62°11'N 27°11'E Lumparn 9 (7-10) ~1000 (500-1200) 60°08'N 20°07'E Suvasvesi N 3.5 (1.5-5?) ~240/~780 ±10 62°41'N 28°11'E Karikkoselkä 1.3 (1.3-2.4?) ~250 (250-450) 62°13'N 25°14'E Saarijärvi 2.1 (1.4-2.1 ) 600-1980 65°17'N 28°25'E Paasselkä 10 (9-12.5 ) <1885 62°12'N 29°23'E Suvasvesi S 3.8 (3.5-4?) ~240/~780 ±10 ? 62°35'N 28°14'E Keurusselkä 11.5 (12-20?) <1880 (>1000?) 62°08'N 24°37'E |