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Chondrule Collection

Background imageChondrule Collection: The Murchison CM2 carbonaceous chondrite

The Murchison CM2 carbonaceous chondrite
Murchison fell in September 1969, in Victoria, Australia. It is rich in indigenous (i.e. not terrestrial contaminant) amino acids and other organic molecules

Background imageChondrule Collection: The Beardsley H5 ordinary chondrite

The Beardsley H5 ordinary chondrite
Beardsley fell in Kansas, U.S.A in 1929. Its fine-grained texture, with poor chondrule resolution indicate that it has experienced thermal metamorphism

Background imageChondrule Collection: The Abee EH4 enstatite chondrite

The Abee EH4 enstatite chondrite
Abee fell in Canada in 1953. The cut surface clearly shows the metal-rich and brecciated texture of Abee

Background imageChondrule Collection: Vigarano CV3 chondrite

Vigarano CV3 chondrite
This carbonaceous chondrite meteorite fell in Italy in 1910. It has clearly delineated chondrules or small granules

Background imageChondrule Collection: Parnallee LL3. 6 ordinary chondrite

Parnallee LL3. 6 ordinary chondrite
Parnallee fell in India in 1857. The cut surface clearly shows well-delineated chondrules and slightly larger clasts

Background imageChondrule Collection: Brownfield (1973) H3. 7 ordinary chondrite

Brownfield (1973) H3. 7 ordinary chondrite
This meteorite fell in Texas in 1937. It has very small chondrules, plus highly-reflective metal and sulphide grains can easily be picked out

Background imageChondrule Collection: Microscope image of chondrite

Microscope image of chondrite showing chondrules, typical of primitive meteorites. Horizontal field of view, 3.3mm

Background imageChondrule Collection: Optical microscope image of the Barwell (Type 6) chondrite

Optical microscope image of the Barwell (Type 6) chondrite. This meteorite has experienced a significant amount of heating

Background imageChondrule Collection: Optical microscope image of the Parnallee (Type 3) chondrite

Optical microscope image of the Parnallee (Type 3) chondrite
An 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

Background imageChondrule Collection: The Parnalle ordinary chondrite

The Parnalle ordinary chondrite
The Parnallee ordinary chondrite, part of the Parnallee meteorite that fell in India in 1857

Background imageChondrule Collection: The Barwell meteorite

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

Background imageChondrule Collection: Textures of different chondrule types

Textures of different chondrule types in the Etihudna (L4) ordinary chondrite (field of view 4mm)

Background imageChondrule Collection: Porphyritic olivine and pyroxene chondrule

Porphyritic olivine and pyroxene chondrule
Microscopic image of a porphyritic olivine and pyroxene chondrule from the Palmyra (L3) ordinary chondrite (the chondrule is about 1.8mm across)

Background imageChondrule Collection: Radial pyroxene chondrule

Radial pyroxene chondrule
Microscope image of a radial pyroxene chondrule from the ALH 88036 (H3.4) ordinary chondrite. The chondrule is about 2mm across

Background imageChondrule Collection: Ivuna meteorite

Ivuna meteorite
The Ivuna carbonaceous chondrite. This type of meteorite is the richest in volatile elements

Background imageChondrule Collection: Barred olivine chondrule

Barred olivine chondrule from the Palmyra ordinary chondrite (the chondrule is about 1.2mm across)


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