Appley Bridge meteorite, Wrightington, West Lancashire, Lancashire, England, UKi
Regional Level Types | |
---|---|
Appley Bridge meteorite | Meteorite Fall Location |
Wrightington | Civil Parish |
West Lancashire | Borough |
Lancashire | County |
England | Constituent Country |
UK | Country |
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Latitude & Longitude (WGS84):
53° 34' 59'' North , 2° 43' 0'' West
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Appley Bridge | 5,270 (2018) | 0.7km |
Shevington | 5,195 (2011) | 2.0km |
Parbold | 3,904 (2018) | 3.7km |
Skelmersdale | 38,944 (2011) | 5.3km |
Coppull | 9,014 (2018) | 6.0km |
Mindat Locality ID:
269101
Long-form identifier:
mindat:1:2:269101:8
GUID (UUID V4):
66abcbf6-052b-484e-9ba7-7f61886428fa
Ordinary chondrite, veined (LL6, br; S2; W0)
Fell, 13 Oct 1914; 15 kg
During the evening a fireball appeared, detonations were heard, and the next day a meteoritic stone was recovered at Halliwell farm. Upon inspection the meteorite exhibits a recrystallized texture dominated by olivine, orthopyroxene, and lesser amounts of plagioclase. Relic chondrules, chondrule fragments, and metal grains are set within a fine-grained matrix. Opaques include Fe-Ni metal (including rare Co-rich wairauite), troilite with other sulfides, and chromite. Troilite is more abundant than Fe-Ni metal. Other phases are reported as well. Brecciation, veins, and undulatory extinction in olivine are consistent with moderate shock (S2), but some features may have been annealed so as to mask actual peak shock pressures which the meteoroid experienced during its preterrestrial eons. The reported cosmic ray exposure (CRE) age (1.2 Ma) is unusually short for chondritic meteorites. The short CRE age suggests relatively a recent disruption of a 'daughter' asteroid during the long journey between formation on an original asteroidal parent body, fragmental disruptions, and eventual earth impact for the Appley Bridge meteoroid.
Total iron (~20 wt%), olivine composition (Fa31), and oxygen isotopes indicate classification as an LL chondrite (very low bulk iron). LL chondrites are the smallest of the 3 major groups of ordinary chondrites with their 87 witnessed falls representing somewhat less than 10% of all recognized meteorite falls (early January 2016).
Some of the mass was apparently lost during events between impact and the institutional acquisition by scientists of 10.9 kg. However, the main mass has remained with the Museum of Natural History in London (8.69 kg in 2000).
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
12 valid minerals.
Meteorite/Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
ⓘ Chromite Formula: Fe2+Cr3+2O4 |
ⓘ Copper Formula: Cu |
ⓘ Diopside Formula: CaMgSi2O6 Description: Composition — Wo44.0Fs10.0En46.0, Binns (1970). References: |
ⓘ 'Fayalite-Forsterite Series' Description: Composition — Fa31 (Mason, 1962) & Fa31.4 (Rubins, 1990). References: |
ⓘ Ilmenite Formula: Fe2+TiO3 |
ⓘ Iron Formula: Fe |
ⓘ Iron var. Kamacite Formula: (Fe,Ni) |
ⓘ Isocubanite Formula: CuFe2S3 |
ⓘ Mackinawite Formula: FeS |
ⓘ 'Orthopyroxene Subgroup' Description: Orthopyroxene Composition — Fs25.2En73.0Wo1.8, Binns (1970). References: |
ⓘ Pentlandite Formula: (NixFey)Σ9S8 |
ⓘ 'Plagioclase' Formula: (Na,Ca)[(Si,Al)AlSi2]O8 |
ⓘ Taenite Formula: (Fe,Ni) |
ⓘ Tetrataenite Formula: FeNi |
ⓘ Troilite Formula: FeS References: |
ⓘ Wairauite Formula: CoFe Description: Wairauite (37 wt% Co) |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 1 - Elements | |||
---|---|---|---|
ⓘ | Copper | 1.AA.05 | Cu |
ⓘ | Iron | 1.AE.05 | Fe |
ⓘ | var. Kamacite | 1.AE.05 | (Fe,Ni) |
ⓘ | Taenite | 1.AE.10 | (Fe,Ni) |
ⓘ | Tetrataenite | 1.AE.10 | FeNi |
ⓘ | Wairauite | 1.AE.15 | CoFe |
Group 2 - Sulphides and Sulfosalts | |||
ⓘ | Pentlandite | 2.BB.15 | (NixFey)Σ9S8 |
ⓘ | Isocubanite | 2.CB.55b | CuFe2S3 |
ⓘ | Troilite | 2.CC.10 | FeS |
ⓘ | Mackinawite | 2.CC.25 | FeS |
Group 4 - Oxides and Hydroxides | |||
ⓘ | Chromite | 4.BB.05 | Fe2+Cr3+2O4 |
ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
Group 9 - Silicates | |||
ⓘ | Diopside | 9.DA.15 | CaMgSi2O6 |
Unclassified | |||
ⓘ | 'Fayalite-Forsterite Series' | - | |
ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
ⓘ | 'Orthopyroxene Subgroup' | - |
List of minerals for each chemical element
O | Oxygen | |
---|---|---|
O | ⓘ Chromite | Fe2+Cr23+O4 |
O | ⓘ Diopside | CaMgSi2O6 |
O | ⓘ Ilmenite | Fe2+TiO3 |
O | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Na | Sodium | |
Na | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Mg | Magnesium | |
Mg | ⓘ Diopside | CaMgSi2O6 |
Al | Aluminium | |
Al | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Si | Silicon | |
Si | ⓘ Diopside | CaMgSi2O6 |
Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
S | Sulfur | |
S | ⓘ Isocubanite | CuFe2S3 |
S | ⓘ Mackinawite | FeS |
S | ⓘ Pentlandite | (NixFey)Σ9S8 |
S | ⓘ Troilite | FeS |
Ca | Calcium | |
Ca | ⓘ Diopside | CaMgSi2O6 |
Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Ti | Titanium | |
Ti | ⓘ Ilmenite | Fe2+TiO3 |
Cr | Chromium | |
Cr | ⓘ Chromite | Fe2+Cr23+O4 |
Fe | Iron | |
Fe | ⓘ Chromite | Fe2+Cr23+O4 |
Fe | ⓘ Ilmenite | Fe2+TiO3 |
Fe | ⓘ Iron | Fe |
Fe | ⓘ Isocubanite | CuFe2S3 |
Fe | ⓘ Iron var. Kamacite | (Fe,Ni) |
Fe | ⓘ Mackinawite | FeS |
Fe | ⓘ Pentlandite | (NixFey)Σ9S8 |
Fe | ⓘ Taenite | (Fe,Ni) |
Fe | ⓘ Tetrataenite | FeNi |
Fe | ⓘ Troilite | FeS |
Fe | ⓘ Wairauite | CoFe |
Co | Cobalt | |
Co | ⓘ Wairauite | CoFe |
Ni | Nickel | |
Ni | ⓘ Iron var. Kamacite | (Fe,Ni) |
Ni | ⓘ Pentlandite | (NixFey)Σ9S8 |
Ni | ⓘ Taenite | (Fe,Ni) |
Ni | ⓘ Tetrataenite | FeNi |
Cu | Copper | |
Cu | ⓘ Copper | Cu |
Cu | ⓘ Isocubanite | CuFe2S3 |
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