#NovaScotia had its first two gold rushes in the second half of the 1800s, in the same era that gold rushes happened in California (1848-1855) and the Yukon (1896-1899). But #NS’ #gold deposits were very different from the ones mined in California and the Yukon. #nspoli#cbpoli
Most #NovaScotia#gold is in quartz veins that started forming 400 million years ago as North Africa and North America started colliding. Sub-sea sediments were squished between the tectonic plates, upthrusted and folded as they turned into rock. This allowed fluid... #nspoli
...to leach gold from rock deep underground and flow into cracks in rock closer to surface, forming veins of quartz and gold as the fluid eventually cooled and hardened. The #MooseRiver gold mine and other deposits along the eastern shore currently being explored formed this way.
The deposits that triggered gold rushes in California and the Yukon were placer deposits (aka alluvial), meaning the gold was concentrated in ancient river sediments after being eroded from bedrock gold deposits. #nspoli#novascotia#gold
Water eroded the rock and gold and carried the eroded sediments downhill until they settled out. This concentrated the gold in one area, creating placer deposits.
That's why a classic image of prospectors is someone using a pan to find #gold in rivers and streams. #nspoli
They scooped up water and gravel in a pan, swirled it around and the gold, which is very heavy, settled on the bottom of the pan while the lighter gravel and dirt washed over the side. This was a simple but effective small-scale method of extracting the #gold. #nspoli#novascotia
Nova Scotia has some placer gold but very little compared to places like California and the Yukon. The reason is Nova Scotia was repeatedly covered with glaciers in the past 100,000 years, until the last ice age ended 10,000 years ago. #nspoli#novascotia#gold
The glaciers dragged sediments and rocks along with them as they moved, scattering the gold of any placer deposits that existed prior to the glaciers. #nspoli#novascotia#gold
California and the Yukon, on the other hand, were not as heavily glaciated as Nova Scotia was. They had many more thousands of years of stream erosion than Nova Scotia, and this liberated huge quantities of gold from bedrock deposits... #nspoli#novascotia#gold
...Their placer deposits were mainly left intact because they had less glaciation, so they were just waiting to be discovered in the 1800s. #nspoli#novascotia#gold
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For example, an e-car has 183 pounds of copper wiring in it because copper is used in every major component from the motor to the inverter and the electrical wiring. There is about four times more copper in an e-car than in a car with an internal combustion engine.
There are about 400 electric cars on Nova Scotia roads - a total of over 73,000 pounds of copper!
An electric car uses 25-50 grams of silver, so Nova Scotia’s 400 e-cars contain about 15,000 grams of it.
Concrete is a mixture of aggregates and paste. The aggregates are sand and gravel or crushed stone; the paste is water and portland cement. (The terms cement and concrete are often used interchangeably, but cement is actually an ingredient of concrete... #nspoli
...Cement is the glue that holds concrete together.)
Reinforced concrete means the concrete is poured over a frame, usually steel bars, that give the structure greater strength. #nspoli
The short answer is yes, sinkholes are real but no, they are not a major risk and should not prevent you from enjoying outdoor activities.
Most natural sinkholes are caused by groundwater naturally eroding rocks like gypsum, salt and limestone which are water-soluble. #nspoli
The water erodes the rock, leaving an underground cavern. Eventually, the weight of the rock and earth above the cavern causes the sinkhole to form. Sinkholes can form either gradually (i.e. a small depression appears and perhaps grows larger over time) or by sudden collapse.
The New Campbellton coal mine was opened in 1862 by Charles J. Campbell, a former Member of Parliament, Member of the Legislative Assembly and executive council member. The community had been named Kelly’s Cove but was changed to New Campbellton in 1862 in honour of Mr. Campbell.
A sample of New Campbellton’s coal was sent to the 1865 Dublin Exhibition and “was very favorably noticed by the Judges,” according to a report. #nspoli#cbpoli#novascotia#capebreton#nshistory
Mining built #NovaScotia! #Halifax was founded in 1749 and its first court house is reported to have been built by 1754 on the northeastern corner of Buckingham + Argyle streets. After the building burned in 1789, the courts were temporarily housed in various buildings. #nspoli
In April 1851 a bill to provide Halifax with a county court house was passed. Mr. H.G. Hill, a prominent #Halifax architect, prepared a plan for a wooden building.
However, since the records of the county, wills, deeds and other papers of public office were... #nspoli#novascotia
...to be stored in the court house, it was important that the building be fire-proof. Also, a number of serious fires in #Halifax in 1857 led to the passage of a bylaw that required large buildings be made of stone or brick, so Hill's plans for a wooden building were abandoned.
The Sullivan Creek #coal mine, before and after!
It's one of several mines reclaimed around #AlderPoint#CapeBreton in the late 1900s/early 2000s - examples of how mining makes temporary use of land and then land can be used other ways. #nspoli#cbpoli#novascotia@JaimeBattiste
The first mine in the area was the Scotia Mine, or #NovaScotia Steel & Coal Company No. 4 Colliery, on Toronto Road, which operated on the Sydney Main (Harbour) Seam from 1915 to 1921. #nspoli#cbpoli#novascotia@JaimeBattiste
Coal quality and structural issues (including water inflow) plague the Harbour Seam west of Florence so upon closure of the colliery, production on the Harbour Seam was limited to the Company’s No. 3 Colliery in Florence, which had opened in 1902... #nspoli#cbpoli#novascotia