User:Arose04/sandbox

Uses and Locations (added to original "uses" section)

There are various outcrops located in the towns surrounding Dedham including Franklin and Medfield. The general area of dedham granite stretches from Dedham MA down to Franklin MA including Medfield MA and parts of Norwood MA. Westwood MA and the surrounding area has outcrops that are typically not Dedham granite despite being surrounded by it.

Geological History

The Dedham Granite was formed during the Ediacaran Period of the Precambrian era about 610 million years ago and is one of the oldest rocks in the Boston basin. Dedham granites to the south and west of the basin are older outcrops from around 630 million years ago, while outcrops to the north of the basin are younger and closer to 596 million years old. The dedham granite formed do the the interactions of two land structures - the Avalon microcontinent and the Gondwana supercontinent. There was an early collision along the Bloody Bluff Fault that damaged the continental shelf of the Gondwana supercontinent. During the collision large amounts of magma came from the Avalon volcanic chain and swallowed the edge of the continental shelf which created deposits of Dedham granite throughout Massachusetts. Some outcrops on the Avalon terrane were formed differently, through magma intrusion during the Precambrian era.

During this time the supercontinent, Pangea, was still in tact. This is why there are also deposits of Dedham granite found in Africa since the formation of the rock occurred before the major continental movement.

Geological Makeup Dedham Granite is a pink to gray medium to coarse grained igneous rock. It is phaneritic, meaning that the crystals are corse enough to be seen with the naked eye. It is a two mica granite which means there are amounts of both muscovite mica and sericite present. There are also large amounts of quartz and Feldspar (mainly K-feldspar). There are deposits of epidote and chlorite throughout some samples of Dedham Granite. Typically these deposits manifest as green colored veins throughout the rock. Veins typically enter rocks as hydrothermals when the minerals in the granite were crystallized from hot water or other hot liquids passing through the rock. For Dedham granite alterations of K-feldspar and plagioclase feldspar allow for the formation of the epidote/chlorite vein. Dedham granite typically lacks a magnetic pull meaning that it contains amounts of ilmenite and lacks magnetite.