Английская Википедия:Impact structures in Finland

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As of June 2018, 12 confirmed impact structures have been found in Finland. They are listed below, sorted by original diameter.

List of identified impact structures in Finland
Structure name Crater type Diameter (km) Depth (m) Age (Myr) Geologic period (epoch) Location Municipality Impact origin shown [Note 3] Notes
Original (estimate)

[Note 1]

Current Original (estimate)

[Note 1]

Current (buried structure) Current (solid surface)

[Note 2]

Min Max Best fit
Keurusselkä Complex 30[1] 14[2] 820[3] N/A 1141[4] 1161[4] 1150[4] Stenian Шаблон:CoordDec Keuruu / Mänttä-Vilppula 2004[5]

2010[6]

Heavily eroded, only remnants of central peak remain.
Lappajärvi Complex[7] 20[7] 17[7] 730[3] 137[8] 77.07[9] 78.63[9] 77.85[9] Cretaceous (Late) Шаблон:CoordDec Lappajärvi / Alajärvi / Vimpeli 1968[10]

1970[11]

1976 [12]

Preserved well, rim outside lake largely intact.
Paasselkä Complex?[7] 10[7] 590[3] 74[13] 229.2

[14][15]

232.8

[14][15]

231.0

[14][15]

Triassic (Late) Шаблон:CoordDec Savonlinna / Kitee 1999[16]

2003

2008[17]

Bay of Orivesi lake in Greater Saimaa.
Lumparn Complex[7] 9[7] 9[7] - 10[18] 570[3] 450[19] 1250[19] 580[19] Ectasian to Ordovician Шаблон:CoordDec Jomala / Lemland / Lumparland / Sund 1993[18]

1997

Bay of the Archipelago sea.
Söderfjärden Complex,[7] polygonal (hexagonal) 6.6[7] 6.6[7] 520[3] 55[8] 520[7] - 640[20] Cambrian (Early) Шаблон:CoordDec Vaasa / Korsholm / Malax 1978

1985

2013[21]

Extremely well preserved; rim nearly entirely intact, buried soon after impact, later exhumed. Dried bay of Kvarken.
Sääksjärvi Simple?[7] 5[7] 4.5[7] - 5[22] 480[3] 9.1[23] 544[22] 576[22] 560[22] Ediacaran Шаблон:CoordDec Kokemäki 1969[24]

1980

1997

Central part of the Sääksjärvi lake.
Suvasvesi N Complex?[7] 4[7][25] 450[3] 79.7[26] 88.1[26] 85[26] Cretaceous (Late) Шаблон:CoordDec Kuopio / Leppävirta 1995

1996[25]

Kukkarinselkä; open water in the Suvasvesi lake.
Suvasvesi S Simple?

Complex?

~4 450[3] 679[26] 727[26] 710[26] Cryogenian, possibly but unlikely Tonian Шаблон:CoordDec Kuopio / Leppävirta 2001[27]

2002[28] 2003

Haapaselkä; open water in the Suvasvesi lake.
Iso-Naakkima Simple[7] < 4[7] 2[7] - 3[29] 450[3] - 600[29] 160[29] N/A 900[30] 1200[30] Stenian or Tonian Шаблон:CoordDec Pieksämäki / Mikkeli 1993[29] Buried, only partly under the Iso-Naakkima lake
Saarijärvi Simple?[7] 3.4[7] 1.5[7][31] - 2[32] 420[3] 0[21] 541[21] Cambrian to Quaternary Шаблон:CoordDec Taivalkoski 1997[33]

1998[31]

2013[21]

Central part of the Saarijärvi lake.
Summanen Simple? 2.6[34] 640[3] 200[34] 41[35] 2.588[34][36] 1910[36] Orosirian to Neogene Шаблон:CoordDec Saarijärvi 2007[37]

2018[34]

Central part of the Summanen lake.
Karikkoselkä Simple[7] 3[7] 1.3[7] 640[3] 26[38] 230[39] 260[39] - 458[40] (Late) Ordovician to (Early) Triassic Шаблон:CoordDec Petäjävesi 1996[38]

1999[39]

2000

Open water in Petäjävesi lake

Note 1: The "original" crater dimensions are coarse estimates. Original depths were calculated using the given original diameter using the Impact: Earth! program.

Note 2: "Current solid surface" topography is calculated from the deepest floor (regardless whether it is underwater or on dry land) to highest rim crest; other depth values give the depth of the floor in relation to the original terrain, thus excluding the rim and/or central uplift.

Note 3: Evidence for impact origin for a given structure is often provided in several publications. The year column includes some publications where some evidence of impact origin was provided even though an impact was not necessarily suggested by the authors; somewhere an impact was suggested even though the proof wasn't conclusive; and somewhere definite proof was provided.

General note 1: Crater sizes and shapes vary according to local differences. For example, depending on where you measure the crater diameter the result may vary (craters are seldom perfect circles). This is affected by, e.g., impact angle (low < 5-10 degree impact angles cause more elliptical craters) and local zones of weakness (may cause the crater to become polygonal).

General note 2: On Earth the (theoretical) transition diameter between simple and complex craters is 2 – 4 km. Such small craters may be either end member or some intermediate form, and thus the given dimension estimates may be off. The depth may be off by ~50 %.

References

Шаблон:Reflist

  1. Шаблон:Cite journal
  2. Шаблон:Cite journal
  3. 3,00 3,01 3,02 3,03 3,04 3,05 3,06 3,07 3,08 3,09 3,10 3,11 Шаблон:Cite web
  4. 4,0 4,1 4,2 Шаблон:Cite journal
  5. Шаблон:Cite journal
  6. Шаблон:Cite journal
  7. 7,00 7,01 7,02 7,03 7,04 7,05 7,06 7,07 7,08 7,09 7,10 7,11 7,12 7,13 7,14 7,15 7,16 7,17 7,18 7,19 7,20 7,21 7,22 7,23 7,24 7,25 Шаблон:Citation
  8. 8,0 8,1 Шаблон:Cite web
  9. 9,0 9,1 9,2 Шаблон:Cite journal
  10. Шаблон:Cite journal
  11. Шаблон:Cite journal
  12. Шаблон:Cite book
  13. Шаблон:Cite web
  14. 14,0 14,1 14,2 Шаблон:Cite journal
  15. 15,0 15,1 15,2 Шаблон:Cite journal
  16. Шаблон:Cite journal
  17. Шаблон:Cite journal
  18. 18,0 18,1 Шаблон:Cite journal
  19. 19,0 19,1 19,2 Шаблон:Cite journal
  20. Шаблон:Cite journal
  21. 21,0 21,1 21,2 21,3 Шаблон:Cite journal
  22. 22,0 22,1 22,2 22,3 Шаблон:Cite journal
  23. Шаблон:Cite web
  24. Шаблон:Cite journal
  25. 25,0 25,1 Шаблон:Cite journal
  26. 26,0 26,1 26,2 26,3 26,4 26,5 Шаблон:Cite journal
  27. Шаблон:Cite journal
  28. Шаблон:Cite journal
  29. 29,0 29,1 29,2 29,3 Шаблон:Cite journal
  30. 30,0 30,1 Шаблон:Cite journal
  31. 31,0 31,1 Шаблон:Cite journal
  32. Шаблон:Cite book
  33. Шаблон:Cite journal
  34. 34,0 34,1 34,2 34,3 Шаблон:Cite journal
  35. Шаблон:Cite web
  36. 36,0 36,1 Шаблон:Cite journal
  37. Шаблон:Cite book
  38. 38,0 38,1 Шаблон:Cite journal
  39. 39,0 39,1 39,2 Шаблон:Citation
  40. Шаблон:Cite journal