Clifton Quarry, Windsor, Hants Co., Nova Scotia, Canada
|Latitude & Longitude (WGS84):||44° 59' 24'' North , 64° 8' 16'' West|
|Latitude & Longitude (decimal):||44.99000,-64.13778|
|Köppen climate type:||Dfb : Warm-summer humid continental climate|
A lost locality that was collected by Henry How (howlite) in the mid/late 1800s. On the Clifton Estate, site of the Haliburton House. The site was a gypsum quarry with some borates and other evaporite minerals.
How referred to the minerals as:
glauber salt (mirabilite)
This was the first Canadian occurrence for each of these minerals. It was the second known occurrence worldwide of ulexite.
The quarry occupied both sides of what is now Clifton Ave. The east side was filled in in the mid 1900s and is now built over. The west side is now flooded and is a lake.
Commodity ListThis is a list of exploitable or exploited mineral commodities recorded at this locality.
6 valid minerals.
This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.
Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org
323.2 - 358.9 Ma
|Wentworth Station, Miller Creek, MacDonald Road and Elderbank Formations|
Age: Mississippian (323.2 - 358.9 Ma)
Stratigraphic Name: Wentworth Station Formation; Miller Creek Formation; MacDonald Road Formation; Elderbank Formation
Description: Gypsum, minor siltstone, marine limestone, and dolostone (Viséan (Holkerian), B subzone fauna and spores); includes the Wentworth Station Formation, Miller Creek Formation, MacDonald Road Formation, and Elderbank Formation
Reference: Kippie, J.D. (compiler), B.E. Fisher, J.C. Poole. Geological Map of the Province of Nova Scotia, Scale 1:500 000. Nova Scotia Department of Natural Resources.