Tysnes Island meteorite, Tysnesøya, Tysnes, Vestland, Norwayi
| Regional Level Types | |
|---|---|
| Tysnes Island meteorite | Meteorite Fall Location |
| Tysnesøya | Island |
| Tysnes | Municipality |
| Vestland | County |
| Norway | Country |
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Latitude & Longitude (WGS84):
60° 0' North , 5° 37' East
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Våge | 513 (2013) | 7.1km |
| Herøysund | 371 (2013) | 13.3km |
| Uskedalen | 717 (2014) | 15.6km |
| Fitjar | 1,280 (2014) | 19.0km |
| Dimmelsvik | 225 (2013) | 20.7km |
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
Local clubs are the best way to get access to collecting localities
| Club | Location | Distance |
|---|---|---|
| Haugaland Geologiforening | Førde i Hordaland | 44km |
Other Languages:
Norwegian:
Tysnesmeteoritten, Tysnesøya, Tysnes, Vestland, Norge
Ordinary chondrite, brecciated (H4)
Fell, 20 May 1884; 19.86 kg
After a fireball and an explosion, two stones of unequal size (18.95 kg; .91 kg) fell and were recovered. Initially, the meteorite did not seem to be have been of unusual interest with olivine (Fa20), pyroxene, troilite, meteoritic iron, and some glass as is more or less expected in ordinary chondrites. However, the meteorite reveals a dark/light structure with darker regions of a somewhat disparate chemistry and increasing disequilibrium. Interest heightened considerably, however, as an unusual clast with immiscible melt and, then, other unusual inclusions were found. The inclusions appear related to carbonaceous chondrites, but may sample ancient populations otherwise poorly represented in our collections. Here and there exotic fragments of both high temperature processes and of much cooler aqueous alteration have been reported.
Tysnes Island is one of 51 meteorites classified precisely as an H4 ordinary chondrite (high bulk iron, moderately equilibrated silicates) [as of Dec. 2015]. However, while this description may hold for most of the meteorite there are clearly some components with unusually different histories which have joined this superficially 'ordinary' chondrite somewhere along the way.
Tysnes Island is one of 7 witnessed ordinary chondrite falls to have been recovered in Norway. The main mass has been kept at the Mineralogical-Geology Museum in Oslo where most Norwegian meteorites are housed.
Fell, 20 May 1884; 19.86 kg
After a fireball and an explosion, two stones of unequal size (18.95 kg; .91 kg) fell and were recovered. Initially, the meteorite did not seem to be have been of unusual interest with olivine (Fa20), pyroxene, troilite, meteoritic iron, and some glass as is more or less expected in ordinary chondrites. However, the meteorite reveals a dark/light structure with darker regions of a somewhat disparate chemistry and increasing disequilibrium. Interest heightened considerably, however, as an unusual clast with immiscible melt and, then, other unusual inclusions were found. The inclusions appear related to carbonaceous chondrites, but may sample ancient populations otherwise poorly represented in our collections. Here and there exotic fragments of both high temperature processes and of much cooler aqueous alteration have been reported.
Tysnes Island is one of 51 meteorites classified precisely as an H4 ordinary chondrite (high bulk iron, moderately equilibrated silicates) [as of Dec. 2015]. However, while this description may hold for most of the meteorite there are clearly some components with unusually different histories which have joined this superficially 'ordinary' chondrite somewhere along the way.
Tysnes Island is one of 7 witnessed ordinary chondrite falls to have been recovered in Norway. The main mass has been kept at the Mineralogical-Geology Museum in Oslo where most Norwegian meteorites are housed.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
14 valid minerals.
Meteorite/Rock Types Recorded
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ Augite Formula: (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| ⓘ Augite var. Fassaite Formula: (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
| ⓘ Chromite Formula: Fe2+Cr3+2O4 References: |
| ⓘ Dolomite Formula: CaMg(CO3)2 |
| ⓘ Enstatite Formula: Mg2Si2O6 Description: Rare grain (En90Wo4). |
| ⓘ 'Fayalite-Forsterite Series' Description: Olivine Composition (Fa20) characteristic of H chondrites [But Fa 15.6 in dark fractions reported by McSween & Lipschutz (1980)]. |
| ⓘ 'Glass' References: |
| ⓘ Graphite Formula: C Description: Graphite-magnetite aggregates are found. |
| ⓘ Isocubanite Formula: CuFe2S3 |
| ⓘ Magnesite Formula: MgCO3 Description: Carbonates are indicative of preterrestrial hydrous activity. |
| ⓘ Magnesite var. Breunnerite Formula: (Mg,Fe)CO3 Description: Carbonates are indicative of preterrestrial hydrous activity. |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 References: |
| ⓘ Native Copper Formula: Cu |
| ⓘ Native Iron Formula: Fe Description: Kamacite in dark fractions unequilibrated. References: |
| ⓘ Native Iron var. Kamacite Formula: (Fe,Ni) Description: Kamacite in dark fractions unequilibrated. References: |
| ⓘ 'Orthopyroxene Subgroup' References: |
| ⓘ 'Pyroxene Group' Formula: ADSi2O6 |
| ⓘ Pyrrhotite Formula: Fe1-xS Description: In Carbonaceous clasts. |
| ⓘ Schreibersite Formula: (Fe,Ni)3P |
| ⓘ Taenite Formula: (Ni,Fe) Description: Taenite in light fractions is much more equilibrated than in dark fractions. |
| ⓘ Troilite Formula: FeS |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Copper | 1.AA.05 | Cu |
| ⓘ | Native Iron | 1.AE.05 | Fe |
| ⓘ | var. Kamacite | 1.AE.05 | (Fe,Ni) |
| ⓘ | Taenite | 1.AE.10 | (Ni,Fe) |
| ⓘ | Schreibersite | 1.BD.05 | (Fe,Ni)3P |
| ⓘ | Graphite | 1.CB.05a | C |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Isocubanite | 2.CB.55b | CuFe2S3 |
| ⓘ | Pyrrhotite | 2.CC.10 | Fe1-xS |
| ⓘ | Troilite | 2.CC.10 | FeS |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Chromite | 4.BB.05 | Fe2+Cr3+2O4 |
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Magnesite | 5.AB.05 | MgCO3 |
| ⓘ | var. Breunnerite | 5.AB.05 | (Mg,Fe)CO3 |
| ⓘ | Dolomite | 5.AB.10 | CaMg(CO3)2 |
| Group 9 - Silicates | |||
| ⓘ | Enstatite | 9.DA.05 | Mg2Si2O6 |
| ⓘ | Augite | 9.DA.15 | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| ⓘ | var. Fassaite | 9.DA.15 | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
| Unclassified | |||
| ⓘ | 'Fayalite-Forsterite Series' | - | |
| ⓘ | 'Pyroxene Group' | - | ADSi2O6 |
| ⓘ | 'Orthopyroxene Subgroup' | - | |
| ⓘ | 'Glass' | - | |
List of minerals for each chemical element
| C | Carbon | |
|---|---|---|
| C | ⓘ Dolomite | CaMg(CO3)2 |
| C | ⓘ Graphite | C |
| C | ⓘ Magnesite | MgCO3 |
| C | ⓘ Magnesite var. Breunnerite | (Mg,Fe)CO3 |
| O | Oxygen | |
| O | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| O | ⓘ Chromite | Fe2+Cr23+O4 |
| O | ⓘ Dolomite | CaMg(CO3)2 |
| O | ⓘ Enstatite | Mg2Si2O6 |
| O | ⓘ Magnesite | MgCO3 |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Magnesite var. Breunnerite | (Mg,Fe)CO3 |
| O | ⓘ Fayalite-Forsterite Series | |
| O | ⓘ Pyroxene Group | ADSi2O6 |
| O | ⓘ Augite var. Fassaite | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
| Na | Sodium | |
| Na | ⓘ Augite var. Fassaite | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
| Mg | Magnesium | |
| Mg | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Mg | ⓘ Dolomite | CaMg(CO3)2 |
| Mg | ⓘ Enstatite | Mg2Si2O6 |
| Mg | ⓘ Magnesite | MgCO3 |
| Mg | ⓘ Magnesite var. Breunnerite | (Mg,Fe)CO3 |
| Mg | ⓘ Fayalite-Forsterite Series | |
| Mg | ⓘ Augite var. Fassaite | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
| Al | Aluminium | |
| Al | ⓘ Augite var. Fassaite | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
| Si | Silicon | |
| Si | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Si | ⓘ Enstatite | Mg2Si2O6 |
| Si | ⓘ Fayalite-Forsterite Series | |
| Si | ⓘ Pyroxene Group | ADSi2O6 |
| Si | ⓘ Augite var. Fassaite | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
| P | Phosphorus | |
| P | ⓘ Schreibersite | (Fe,Ni)3P |
| S | Sulfur | |
| S | ⓘ Isocubanite | CuFe2S3 |
| S | ⓘ Pyrrhotite | Fe1-xS |
| S | ⓘ Troilite | FeS |
| Ca | Calcium | |
| Ca | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Ca | ⓘ Dolomite | CaMg(CO3)2 |
| Ca | ⓘ Augite var. Fassaite | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
| Ti | Titanium | |
| Ti | ⓘ Augite var. Fassaite | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
| Cr | Chromium | |
| Cr | ⓘ Chromite | Fe2+Cr23+O4 |
| Fe | Iron | |
| Fe | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Fe | ⓘ Chromite | Fe2+Cr23+O4 |
| Fe | ⓘ Native Iron | Fe |
| Fe | ⓘ Isocubanite | CuFe2S3 |
| Fe | ⓘ Native Iron var. Kamacite | (Fe,Ni) |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Pyrrhotite | Fe1-xS |
| Fe | ⓘ Schreibersite | (Fe,Ni)3P |
| Fe | ⓘ Taenite | (Ni,Fe) |
| Fe | ⓘ Troilite | FeS |
| Fe | ⓘ Magnesite var. Breunnerite | (Mg,Fe)CO3 |
| Fe | ⓘ Fayalite-Forsterite Series | |
| Fe | ⓘ Augite var. Fassaite | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
| Ni | Nickel | |
| Ni | ⓘ Native Iron var. Kamacite | (Fe,Ni) |
| Ni | ⓘ Schreibersite | (Fe,Ni)3P |
| Ni | ⓘ Taenite | (Ni,Fe) |
| Cu | Copper | |
| Cu | ⓘ Native Copper | Cu |
| Cu | ⓘ Isocubanite | CuFe2S3 |
Other Regions, Features and Areas containing this locality
Eurasian PlateTectonic Plate
- CaledonidesOrogenic Belt
EuropeContinent
Norway
- ⭔HordalandCounty
ScandinaviaRegion
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References
Mason, Brian (1963) Olivine composition in chondrites. Geochimica et Cosmochimica Acta, 27 (10) 1011-1023 doi:10.1016/0016-7037(63)90062-0
Rubin, Alan E. (1990) Kamacite and olivine in ordinary chondrites: Intergroup and intragroup relationships. Geochimica et Cosmochimica Acta, 54 (5) 1217-1232 doi:10.1016/0016-7037(90)90148-e
Krot, Alexander N., Rubin, Alan E. (1994) Glass-rich chondrules in ordinary chondrites. Meteoritics, 29 (5) 697-707 doi:10.1111/j.1945-5100.1994.tb00787.x

Tysnes Island meteorite, Tysnesøya, Tysnes, Vestland, Norway