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Meteorite 1891Observed at Oschansk, Russia. Date: 1891
The Esquel pallasite
Pallasite slabThe Esquel pallasite, composed of gem-quality olivine crystals embedded in metal. Pallasites are perhaps the most beautiful of all meteorites. Specimen held at the Natural History Museum, London
Estherville MeteroriteMeteorite section BM 53764, Estherville, 2.727kg from the Natural History Museums Mineralogy Department
Wold meteorite landing sitePen and ink sketch showing an obelisk marking the landing site of the Wold Meteorite, Yorkshire, 1812. Image from the Sowerby Collection by Gerrit van Spaendonck
Estherville MeteoriteMeteorite section BM 53764, Estherville, 2.727kg from the Natural History Museums Mineralogy Department
The Estherville mesosiderite formed after a catastrophic collision between two asteroids. Mesosiderites are an irregular jumble of metal grains and angular pieces of rock
Variety of tektites
The Stannern achondrite see 35502A piece of the Stannern achondrite which is thought to have originated on the asteroid Vesta
The Canyon Diablo meteoriteThe cut, polished and etched surface of the Canyon Diablo meteorite reveals its high iron content
The Beardsley H5 ordinary chondriteBeardsley fell in Kansas, U.S.A in 1929. Its fine-grained texture, with poor chondrule resolution indicate that it has experienced thermal metamorphism
The Abee EH4 enstatite chondriteAbee fell in Canada in 1953. The cut surface clearly shows the metal-rich and brecciated texture of Abee
Vigarano CV3 chondriteThis carbonaceous chondrite meteorite fell in Italy in 1910. It has clearly delineated chondrules or small granules
Parnallee LL3. 6 ordinary chondriteParnallee fell in India in 1857. The cut surface clearly shows well-delineated chondrules and slightly larger clasts
Interstellar diamondsThis specimen is known as the Allende meteorite. When viewed under a transmission electron microscope it shows formations of tiny interstellar diamonds
Brownfield (1973) H3. 7 ordinary chondriteThis meteorite fell in Texas in 1937. It has very small chondrules, plus highly-reflective metal and sulphide grains can easily be picked out
MeteoritesAn artists impression of a falling group of meteorites
Cold Bokkeveld meteorite photomicrographThin section of the carbonaceous chondrite in the petrological microscope, showing a near circular chondrule about 1mm in diameter. The fall was in Cape Province in 1838
Stone meteoriteThis meteorite is unmelted and is therefore known as a chondrite. Specimen held at the Natural History Museum, London
Stony-iron meteoriteThis meteorite is the product of atmospheric melting, as are stony achondrites. Specimen held at the Natural History Museum, London
Mayo Belwa, African meteoriteThis meteorite formed in a similar way to some igneous rocks in the Earth, and not by condensation of dust from nebular gas. Image from From Behind The Scenes (1987) by Dr Lawrence Mound
Microscope image of the Johnstown diogenite. Diogenites are coarse grained and composed primarily of one mineral, pyroxene. Field of view is 2.5mm across
Shergottite Sayh al Uhaymir 008, found in Oman in 1999. Shergottites are silicate rocks that are divided into four subgroups. This specimen is about 10cm long
Microscope image of chondrite showing chondrules, typical of primitive meteorites. Horizontal field of view, 3.3mm
Slice of the lunar meteorite Northwest Africa 482A slice of lunar meteorite Northwest Africa 482. This meteorite is very rich in the feldspar mineral anorthite, which give it its pale colour
Microscope image of the Zagami shergottite. The fractures in the pyroxene mineral grains and the paler patches of glass show that the rock has been shocked. Field of view is 5mm
Slab of the Lueders meteoriteA slab of the IAB iron meteorite Lueders showing the size, shapes and distribution of silicate inclusions. The slab is about 10cm wide
The Estherville mesosiderateThe Estherville mesosiderite formed after a catastrophic collision between two asteroids. Mesosiderites are an irregular jumble of metal grains and angular pieces of rock
Microscope image of the Brachina meteorite, the type specimen of the Brachinite meteorites. Brachinites are composed mostly of olivine with minor amounts of pyroxene and plagioclase
Microscope image of the Lodran meteorite. This meteorite is the type specimen of the Lodranite meteorites. The lodranites are related to the acaplucoites but are more course-grained
The Sioux County eucritePhotograph of the Sioux County eucrite, which is thought to have originated on the asteroid 4 Vesta. The sample weighs 153g
The Bustee aubritePhotograph of the Bustee aubrite, a light-coloured meteorite containing brown oldhamite crystals
Piece of the Henbury iron meteoriteA pice of the Henbury iron meteorite, 28cm across, which once formed part of an asteroids core
Optical microscope image of the Barwell (Type 6) chondrite. This meteorite has experienced a significant amount of heating
On the Origin of the Pallas Iron and Others Similar to itThe title page of Ernst Chladnis book On the Origin of the Pallas Iron and Others Similar to it, and on Some Associated Natural Phenomena, which was published in 1794
Optical microscope image of the Parnallee (Type 3) chondriteAn optical microscope image of the Parnallee (Type 3) chondrite that has experienced little heating. The chondrules are clear and well-defined. The field of view is 5mm
The Beddgelert (H5) ordinary chondritePhotograph of the Beddgelert (H5) ordinary chondrite, clearly showing flecks of iron-nickel metal
The Parnalle ordinary chondriteThe Parnallee ordinary chondrite, part of the Parnallee meteorite that fell in India in 1857
The Barwell meteorite, showing a rock frgament formed by melting of a pre-existing planetary body; this indicates that plantesimals were present when chondrules formed
Textures of different chondrule types in the Etihudna (L4) ordinary chondrite (field of view 4mm)
Porphyritic olivine and pyroxene chondruleMicroscopic image of a porphyritic olivine and pyroxene chondrule from the Palmyra (L3) ordinary chondrite (the chondrule is about 1.8mm across)
Radial pyroxene chondruleMicroscope image of a radial pyroxene chondrule from the ALH 88036 (H3.4) ordinary chondrite. The chondrule is about 2mm across
Ivuna meteoriteThe Ivuna carbonaceous chondrite. This type of meteorite is the richest in volatile elements
Partially fusion-crusted stoneA 294g (10oz) partially fusion crusted stone from the Camel Donga eucrite strewn field. The orange/brown staining on the black, fusion crusted surface is staining from the local soil
Siena meteorite stoneOne of the stones of the Siena meteorite shower, which fell over Siena, Italy in 1794
Chergach meteorite
British Meteorites, postcard setEnvelope containing a set of 5 postcards published by the Natural History Museum in 1922
Meteoric stone, LauntonOne of a series of 5 postcards featuring British meteorites produced and sold by the museum in the 1920s