Chysoprase found in the streams of Newfane Vermont – Image courtesy of John Betts Fine Minerals<\/p><\/div>\n

Chrysoprase forms from oxidized nickel impurities imparting a green color to the material. The source of this nickel is from rocks geologists call ultramafic. These ultramafic rocks were metamorphosed to form the serpentinite at the deposit. These rocks are from very deep in the earth and have a chemistry that differs quite a bit from other igneous rocks. Often these ultramafic rocks are very rich in magnesium, calcium, and iron. They are also frequently poor in silica and rich in elements like chromium and nickel. When these rocks are exposed to water as well as a tiny amount of heat ad pressure, they break down and form serpentinite. The metals leach into silica and other minerals giving them their color.<\/p>\n

Collecting-<\/p>\n

Most of the collecting at this site will be done in the stream, stream banks, or riverside outcrops. Collecting involves getting into the stream bank and flipping over rocks. You might want to bring a shovel or hand rake to remove material from the stream bottom. Inspect material carefully for anything interesting and keep an eye out for anything with a bright green color. Place anything you want to keep in a sturdy bucket. Heavy waterproof boots or waders are a must in colder months. When it’s warmer wear some waterproof shoes to protect your feet from the rough bottom. Bring a hammer and chisel in care you want to break open anything you find to inspect it further.<\/p>\n

Directions-<\/p>\n