Wold Newton meteorite

Wold Cottage
On display in the Natural History Museum, London
Type	Chondrite
Class	Ordinary chondrite
Group	L6
Country	United Kingdom
Region	Yorkshire, England
Coordinates	54°8′02.4″N 0°24′45.3″W / 54.134000°N 0.412583°W / 54.134000; -0.412583Coordinates: 54°8′02.4″N 0°24′45.3″W / 54.134000°N 0.412583°W / 54.134000; -0.412583
Observed fall	Yes
Fall date	13 December 1795, 3 p.m.
TKW	56 lb (25 kg)

The Wold Cottage meteorite (also called the Wold Newton meteorite) fell near Wold Cottage farm in 1795, a few miles away from the village of Wold Newton in Yorkshire, England.

The stone fell at around 3 o'clock, on 13 December 1795. Landing within a few yards of ploughman John Shipley. It created a crater approximately 1 yard (0.91 m) across, and embedded itself in the underlying chalk rock to a depth of 7 inches (180 mm), passing through 12 inches (300 mm) of topsoil. The fall was observed by several people, who described a dark body passing through the air. As discovered at its landing point, the stone was warm and smoking; several people reported sounds of explosions as it fell. The owner of the land was Major Edward Topham, a well-known public figure, an ex-soldier, playwright and newspaper proprietor; he publicised the find and exhibited the meteorite publicly at Piccadilly in London.

The stone initially weighed 56 pounds (25 kg).James Sowerby, a naturalist, acquired the meteorite in 1804. The meteorite was later acquired by the British Museum in 1835.

The meteorite can nowadays be seen in the Natural History Museum in London.

Early analyses recorded two parts of the stone, an earthy part, and a malleable part. The earthy part analysed as containing silicon, magnesium, iron, and a small amount of nickel, of which some parts of the iron and nickel were in the elemental state; the earthy substance was similar to kaolin (weathered feldspar), but relatively tough. The malleable parts also contained iron and nickel, the majority iron. A form of iron pyrites (iron sulphur compound) was also reported present. Modern science records the meteorite as a L6 ordinary chondrite.

The Wold Cottage meteorite was the largest meteorite observed to fall in Britain, and is the second-largest recorded in Europe (after the Ensisheim meteorite). The meteorite and evidence given about its fall contributed to the debate concerning whether extraterrestrial matter existed or not, and towards the early scientific study of meteorites.