Blade 3.06" (77.7mm)
Handle 4.13" (104.9.5mm)
Overall open 7.19" (182.6mm)
William Henry's patent-pending Wave Damascus features a core in ZDP-189 (HRC 67) or VG-10 (cryo-tempered to a hardness of HRC 61) for superior sharpness and edge retention over time. The core of the blade is clad with alternating layers of stainless steel and nickel silver. The billet, 45 layers in all, is patterned with a custom die to create the undulating waves that emerge across the bevels of the blade. This material can be dark-etched for contrast, or etched and re-polished for a more subtle pattern.
The name diamond is derived from the ancient Greek αδάμας (adámas), "proper", "unalterable", "unbreakable". Diamonds have a long history as beautiful objects of desire. In the first century AD, the Roman naturalist Pliny stated: “Diamond is the most valuable, not only of precious stones, but of all things in this world.”
The world’s love of diamonds had its start in India, where diamonds were gathered from the country’s rivers and streams. Some historians estimate that India was trading in diamonds as early as the fourth century BC.
The popularity of diamonds has risen since the 19th century because of increased supply, improved cutting and polishing techniques. Aside from our jewelry collection, William Henry also inlays diamonds in pocketknives, pens, and money clips.
William Henry uses beautiful sections of the Gibeon Meteorite, which fell in prehistoric times in Namibia. It was named after the nearest town: Gibeon
The fragments of the meteorite in the strewn field are dispersed over an elliptical area 171 miles long and 62 miles wide; it was discovered by the local Nama people and used by them to make tools and weapons.
In 1836 the English captain J. E. Alexander collected samples of the meteorite and sent them to London. There John Herschel analyzed them and confirmed for the first time the extraterrestrial nature of the material.
The Gibeon meteorite is composed of an iron-nickel alloy containing significant amounts of cobalt and phosphorus. The crystal structure of this meteorite provides a fine example of the Widmanstätten patterns: these figures of long nickel-iron crystals are of extraterrestrial origin, and cannot occur naturally on earth. As a purely natural material, the patterns may include small inclusions, distinctive and unique to each item we produce.