http://www.chebucto.ns.ca/ccn/info/Environment/FPPP/history.html WebConstruction activities have exposed sulphide-bearing slates of the Halifax Formation in southern mainland Nova Scotia. Under atmospheric conditions the sulphides break down and cause acid rock drainage (ARD) which adversely affects local ecosystems. These effects have been a major problem at the Halifax International Airport,
Bluestone Formation of the Halifax Group: Metamorphosed …
Webarea consists of Goldenville Formation metawacke and some slate, overlain by Halifax Formation slate and thin bedded silty metawacke. The two units have been folded into tight sub-vertical regional en echelon folds (Fig. 2). Grade of regional metamorphism is lower greenschist except in the north along the West River - St. Mary's Fault where residence square pey berland
Rip-rap & rusty rocks in Halifax, N.S. – Jessica
WebHalifax Formation- Highly foliated metawacke and slates. Commonly sulphide (pyrite) bearing. ... BP-ARD-5 Halifax Formation Pyritic Slate . The most up to date geology map of the Black Point area is associated with the GSC Bulletin 383 by J.D. Hill, 1991. Mapping completed by Erdene geologists of the Goldenville and Halifax WebThe bedrock geology under Oathill Lake is part of the Halifax Formation slate. This formation consists of slate with minor interbedded quartzite. A major issue of the Halifax Formation pyritic slates is its associated acid drainage potential. When exposed to air and moisture sulphides in the rock react and creat a weak sulphuric acid. WebMagnetic Susceptibility of Halifax Formation Slates at the Halifax International Airport: Correlation with Potential for Acid Drainage (PDF - 9.6 Mb) The disruption by excavation or quarrying of sulphide-rich slate units of the Halifax Formation of the Meguma Group of Nova Scotia leads to oxidation of the sulphides and generation of acid drainage. residences shreveport