We love getting questions about mining, minerals and geology! We were asked about Nova Scotia’s version of the San Andreas Fault - the Cobequid-Chedabucto Fault System!
Nova Scotia has two halves geologically... #nspoli#cbpoli#NovaScotia#CapeBreton
#NovaScotia has 2 halves geologically: The northern half came from Europe and the southern half from Africa. The Cobequid-Chedabucto Fault System is where they collided 400 million years ago. This caused earthquakes, melted rocks+concentration of minerals like #gold+zinc. #nspoli
People sometimes think of it as a single fault that cuts the province in half. In fact, it's a fault zone or system, not a single fault. There are several large parallel, or nearly parallel, faults that collectively make up the system. #nspoli#cbpoli#NovaScotia#CapeBreton
The faults usually consist of what we call “fault gouges” - crushed and ground-up rock, sometimes a couple hundred metres thick, produced by friction between the two sides when a fault moves. Regional-scale faults like this are large and complex. #nspoli#cbpoli#NovaScotia
The rock on the left is part of a fault gouge that looks like gravel but is actually solid bedrock because the tectonic plates’ movement ground up the rock but it later solidified again. It extends for about 400 metres along the highway. #nspoli#cbpoli#NovaScotia#CapeBreton
The faults weather more easily than solid rock because they have been fractured and weakened by pressure and movement. (While weathering and erosion are similar processes, they are not the same thing. #nspoli#cbpoli#NovaScotia#CapeBreton
Weathering degrades a rock without changing its location. Erosion, on the other hand, causes rocks, or particles of rock, to be carried away from their original locations and deposited elsewhere. #nspoli#cbpoli#NovaScotia#CapeBreton
For example, water getting into a rock and splitting it when it freezes is weathering because the rock stays in place. Water carrying pebbles and sand down a river is erosion because the location of the pebbles and sand changes.) #nspoli#cbpoli#NovaScotia#CapeBreton
Unlike California’s San Andreas Fault, which is very active because the North American and Pacific tectonic plates rub against each other as the North American plate moves westward several centimetres per year, the Cobequid-Chedabucto Fault System is mostly stable. #nspoli
Movement at faults is caused by stresses in the earth’s crust, i.e. the North American and Pacific tectonic plates rubbing against each other generates tremendous pressure, causing earthquakes at the San Andreas Fault to relieve the stress. #nspoli#cbpoli#NovaScotia#CapeBreton
The Cobequid-Chedabucto Fault System does not have those sorts of stresses so the system is stable. Fortunately for us, Nova Scotia’s geology is much calmer now than it was 400 million years ago! #nspoli#cbpoli#NovaScotia#CapeBreton
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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