The Japanese traditionally use natural sharpening stones (referred to as
tennen toishi) wetted with water, as using oil on such a stone reduces its effectiveness. The geology of Japan provided a type of stone which consists of fine silicate particles in a clay matrix, somewhat softer than
novaculite. Besides this
clay mineral, some sedimentary rock was used by the Japanese for whetstones, the most famous being typically mined in the
Narutaki District just north of
Kyoto along the Hon-kuchi Naori stratum. There were many individual mines which produced stone from one of the three stratums in the region, many sought after for specific reputations such as Ohira Uchigumori, Hakka Tomae, and Nakayama stones. Historically, there are three broad grades of Japanese
toishi (sharpening stones): the
ara-to, or "rough stone", the
naka-to or "middle/medium stone" and the
shiage-to or "finishing stone". There is a fourth type of stone, the
nagura, which is not used directly. Rather, it is used to form a cutting slurry on the
shiage-to (early finishing stone) or
awasedo (late finishing stone), which are often too hard to create the necessary slurry. Converting these names to absolute grit size is difficult as the classes are broad and natural stones have no inherent "grit number". As an indication,
ara-to is probably (using a non-Japanese system of grading grit size) 500–1000 grit. The
naka-to is probably 3000–5000 grit and the
shiage-to is likely 7000–10000 grit. Current synthetic grit values range from extremely coarse, such as 120 grit, through extremely fine, such as 30,000 grit (less than half a
micrometer abrasive particle size). ==Diamond plate==