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Monze meteorite, Monze District, Southern Province, Zambiai
Regional Level Types
Monze meteoriteMeteorite Fall Location
Monze DistrictDistrict
Southern ProvinceProvince
ZambiaCountry

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Latitude & Longitude (WGS84):
15° 58' South , 27° 21' East
Latitude & Longitude (decimal):
Nearest Settlements:
PlacePopulationDistance
Monze30,257 (2012)38.0km
Mazabuka64,006 (2012)44.3km
Nakambala10,425 (2018)48.3km
Mindat Locality ID:
294602
Long-form identifier:
mindat:1:2:294602:6
GUID (UUID V4):
0


Ordinary chondrite (L6)
Fell, 5 October 1950, 4:10 hrs; meteorite shower

An enormously bright fireball was seen in several African countries and enormous thunderous booms preceded a predawn impact which left a large number of small meteoritic stones [often 3-5 cm in diameter] scattered over a considerable region of what is now Zambia's Southern Province. However, specimens began to be reported to the outside world and recovered only after a week or so had passed. In time a request was made by one Chief Chongo to report to England's King George, to wit: 'Please send a piece of star to My King, George, and tell him what has happened in my country and what has visited us, for I know that he will be interested." The chief then assisted in recovery efforts as many people were frightened by the dramatic events and the strange stones.

Variegated colors, shapes, and textures are visible in the often unevenly preserved greenish-greyish matrices. Most stones were covered by a brown-black fusion crust, but fresh surfaces were sometimes present. Compositionally, total iron contents (21.6 wt%), olivine composition (Fa25) and low Ca-orthopyroxene ('hypersthene') are characteristic of the L-chondrite geochemical group. Mineralogically the meteorite consists primarily of dominant olivine and accompanying pyroxene along with minor plagioclase/maskelynite, troilite, and Fe-Ni metal. Fe-Ni metal consists of mostly tiny grains containing kamacite, taenite, and/or plessite. Accessory chromite is also reported. Olivine has been fractured by shock and exhibits mosaic extinction. Preterrestrial shocks have also deformed most plagioclase or converted it into maskelynite.

The L-group of ordinary chondrites (relatively low in total iron) are the largest group of classified witnessed meteorite falls and account for ~45% of all well-classified meteorite falls. The L6 petrologic type accounts for ~ 70% of the L-group chondrites. 272 meteorite falls had been classified exactly as 'L6' chondrites by early June 2017.

A good number of stones have been kept at the Rhodes-Livingston Museum in Zambia and the Zimbabwe National Museum. At some time the British National History Museum (NHM) in London obtained over 50 of the stones weighing ~2.5 kg in total, still preserved in 2000.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


5 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 Diagram

Detailed Mineral List:

Chromite
Formula: Fe2+Cr3+2O4
'Fayalite-Forsterite Series'
Description: Olivine composition (Fa25) characteristic of the L-group ordinary chondrites.
Isocubanite
Formula: CuFe2S3
'Maskelynite'
Native Iron
Formula: Fe
Native Iron var. Kamacite
Formula: (Fe,Ni)
'Orthopyroxene Subgroup'
Description: Abundant Ca-poor orthopyroxene ('hypersthene') a defining characteristic of the well-equilibrated L6 ordinary chondrites.
'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
Description: Plagioclase is largely either deformed or converted to maskelynite.
Taenite
Formula: (Fe,Ni)
Troilite
Formula: FeS

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Native Iron1.AE.05Fe
var. Kamacite1.AE.05(Fe,Ni)
Taenite1.AE.10(Fe,Ni)
Group 2 - Sulphides and Sulfosalts
Isocubanite2.CB.55bCuFe2S3
Troilite2.CC.10FeS
Group 4 - Oxides and Hydroxides
Chromite4.BB.05Fe2+Cr3+2O4
Unclassified
'Maskelynite'-
'Fayalite-Forsterite Series'-
'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
'Orthopyroxene Subgroup'-

List of minerals for each chemical element

OOxygen
O ChromiteFe2+Cr23+O4
O Fayalite-Forsterite Series
O Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
NaSodium
Na Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mg Fayalite-Forsterite Series
AlAluminium
Al Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Si Fayalite-Forsterite Series
Si Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SSulfur
S IsocubaniteCuFe2S3
S TroiliteFeS
CaCalcium
Ca Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
CrChromium
Cr ChromiteFe2+Cr23+O4
FeIron
Fe ChromiteFe2+Cr23+O4
Fe Native IronFe
Fe IsocubaniteCuFe2S3
Fe Native Iron var. Kamacite(Fe,Ni)
Fe Taenite(Fe,Ni)
Fe TroiliteFeS
Fe Fayalite-Forsterite Series
NiNickel
Ni Native Iron var. Kamacite(Fe,Ni)
Ni Taenite(Fe,Ni)
CuCopper
Cu IsocubaniteCuFe2S3

Other Regions, Features and Areas containing this locality

AfricaContinent
African PlateTectonic Plate

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

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