Gemstones that are usually considered “precious stones” are diamonds, rubies, sapphires and emeralds. All other gemstones are considered “semi-precious” (i.e. agate, amber, amethyst, jade, pearl, etc.) #nspoli#cbpoli#capebreton#NovaScotia
These definitions date from the 1800s and they are subjective, not scientific. There is not universal agreement with them, but we mention them to point out that there is usually a distinction made between precious and semi-precious stones. #nspoli#cbpoli#capebreton#NovaScotia
Even the definition of gemstone isn’t clear. Many stones are considered gems but the term does not have a technical definition. #nspoli#cbpoli#capebreton#NovaScotia
Interestingly, some gemstones are not actually minerals. By definition, a mineral must be created inside the earth but a pearl’s coating is created in a mollusk and amber starts out as tree resin. Still, both pearl and amber are considered gemstones. #nspoli#cbpoli#NovaScotia
#NovaScotia doesn't have a history of commercial mining for gemstones but there are many that can be found, and there are many great places in t#NS for rockhounding. Small-scale gathering of gems is done to collect or sell them or to turn them into jewelry. #nspoli#cbpoli
Gemstones that can be found in #NovaScotia include agate, zeolite, garnet, amethyst, quartz crystals, anatase, rutile, cassiterite, sphalerite, phosphates and many others.
Let’s talk about agate since it was declared Nova Scotia’s provincial gemstone in 1999. #nspoli#cbpoli
Agate is a variegated (it has different colours) and banded form of quartz with a beautiful translucency. It is used for jewellery and as a collectible.
Agate is common in the basalt flows of the Jurassic Period in Nova Scotia. #nspoli#cbpoli#capebreton#NovaScotia
As supercontinent Pangea broke up 200 million years ago, lava came out of cracks in earth's crust and formed the Annapolis Valley’s North Mountain – it’s flood basalt, or long, continuous sheets of hardened lava overlying softer sandstone. #nspoli#cbpoli#capebreton#NovaScotia
Agates formed in cavities, called vesicles, in these ancient lava flows. Trapped gases in the lava later escaped, leaving hollow cavities or pockets behind. Cracks and seams (more cavities) in the basalt also formed as adjoining sections of lava cooled at different rates. #nspoli
These empty cavities filled with fluids rich in dissolved and suspended quartz molecules (silica), as well as other mineral impurities. Over time, the silica molecules began to form miniature fibrous microcrystals that attached to the sides of the cavities. #nspoli#cbpoli
During the filling-in process other mineral impurities collected, forming different bands.
This pattern repeated until the entire cavity was filled in, or until all the silica-rich solution was used up. The stones that formed in those cavities are the agates we find in #NS today.
For example, Fundy is world-famous for its zeolites, a group of about 40 related minerals. One of them, mordenite, is named for Morden, NS, where it was discovered in 1864. It's used to clean up chemical spills, in animal feed and for water treatment. #nspoli#cbpoli#NovaScotia
Waste dumps at former mines are often good spots for rockhounding too, but be safe. For example, we understand the former operators of the East Kemptville tin mine laid out their waste dump to facilitate rockhounding and it’s a great site for micro-minerals. #nspoli#cbpoli
Other neat spots include an old quarry at Bolyston, #Guysborough, that is known for really nice rose quartz crystals.
On Gerrish Mountain, near Five Islands, is the New Britain quartz crystal mine where, it is rumoured, the military extracted quartz crystals for radios in #WWII.
Regarding precious stones, there are corundum in Frenchvale, Cape Breton. They look like rubies (rubies are gem-quality corundum) but they don’t quite meet the technical specifications of rubies. #nspoli#cbpoli#capebreton#NovaScotia
Similarly, Nova Scotia has numerous beryl occurrences that look like emeralds (gem-quality beryl) but again, they don’t quite meet the technical specs. Still, they look like the real thing. #nspoli#cbpoli#capebreton#NovaScotia
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