Sanukite

Sanukite is a natural volcanic rock from Japan, a black, dense and very hard glassy andesite (a kind of bronzite andesite). It is named after Sanuki, the old name of Kagawa Prefecture, and is found mainly around Goshikidai and on Kanayama and Shiroyama in Sakaide, Kagawa, and in the Nijōsan area on the Osaka–Nara border. When struck it rings with a clear, metallic tone, so it is locally called "kankan-ishi".

Products made with this material

Category
Category
Color
Color

Colors are read from each product’s main photo.

Bead diameter (mm)
Bead diameter (mm)

Only round beads with a verified diameter. A product matches when its stated size range overlaps yours, limits included; a material matches when any of its round sizes does.

Price (USD)
Price (USD)
Availability

Showing 1 of 1 products

Full material guide
Material facts

What the material is, where it comes from or how it is made, identification and care, from the cited sources.

Properties

Nature Natural volcanic (igneous) rock
Rock type Bronzite andesite; glassy andesite to dacite with 2 % or less phenocrysts
Minerals Phenocrysts usually of olivine and orthopyroxene (rarely hornblende, augite, plagioclase); groundmass of glass with fine orthopyroxene and magnetite and almost no plagioclase
Color Black; weathered surfaces grey to white
Geologic age Miocene, about 13 million years old

Origins & sources

Sanukite formed from lava erupted during volcanic activity in the Seto Inland Sea region about 13 million years ago; it caps the mesa-like hills of northern Kagawa such as Goshikidai and Yashima. Known sources are very few: around Goshikidai, Kanayama and Shiroyama in Sakaide, the Nijōsan area on the Osaka–Nara border, and a few other places. The best-sounding sanukite comes only from a very limited area near Kokubudai on Goshikidai. Related "sanukitoid" rocks occur in the Setouchi volcanic belt from eastern Kyushu to Aichi Prefecture.

Identification

Sanukite is black, dense and hard, with fewer visible crystals (phenocrysts) than ordinary basalt or andesite. When broken it gives sharp edges and shell-like (conchoidal) fractures, and when tapped it gives a high, metallic, ringing sound with a pleasant resonance. Weathered pieces from Goshikidai can take unusual grey-to-white surface forms described as worm-eaten, rotten-wood, pine-cone or katsuobushi (dried-bonito) shapes.

Care

Not collected yet

History & culture

History

Sanukite was used for stone tools in Kagawa from about 30,000 years ago until the end of the Yayoi period about 1,700 years ago, mainly as cutting blades, arrowheads and stone knives. At the Palaeolithic sites excavated during construction of the Seto Ōhashi Bridge (about 130,000 pieces at Yoshima-Seihō and about 350,000 at Hazashima), nearly 98 % of the stone tools and fragments were sanukite. In 1891 the German petrologist Weinschenk named the rock "Sanukit" after Sanuki; according to the Geological Society of Japan he studied samples that Naumann, the first professor of geology at Tokyo Imperial University, had taken back to Germany, while the Kagawa University Museum says Weinschenk came to Japan to study it. The English form "sanukite" became the international name. The Geological Society of Japan lists it as the representative rock of Kagawa Prefecture.

Cultural meanings

Not collected yet

Traditional beliefs

Because of its ringing tone, sanukite has long been called "kankan-ishi" in Sanuki, and since the Edo period it has also been known as "keiseki" (chime stone). It has been used for stone xylophones and other musical instruments and for signalling, and sanukite pieces are sold as local souvenirs.

Sources

Collected Oct 23, 2026