At the bottom of the sea or ocean
Calcite is often found at the bottom of an evaporite deposit because it is less soluble in water compared to other evaporite minerals like halite or gypsum. As the water evaporates, these less soluble minerals tend to precipitate out first and settle at the bottom of the evaporite layer.
Halite, which has a Mohs hardness of 2.5, can scratch minerals that are softer than it on the hardness scale. This means it can scratch talc (hardness 1) and gypsum (hardness 2). However, it would not be able to scratch minerals like calcite (hardness 3) or any harder minerals.
Cold dry air
Cold dry air
halite is a good insulator for electric current..
Calcite is often found at the bottom of an evaporite deposit because it is less soluble in water compared to other evaporite minerals like halite or gypsum. As the water evaporates, these less soluble minerals tend to precipitate out first and settle at the bottom of the evaporite layer.
You can distinguish these minerals by testing their physical properties such as taste (halite is salty), hardness (calcite scratches easily with a knife, halite is soft, fluorite is harder), and fluorescence (fluorite exhibits fluorescence under UV light). Additionally, you can use a hand lens to examine their crystal shapes or conduct a streak test to observe their powder color.
At 27 degrees Fahrenheit, the precipitation would likely fall as snow.
Calcite crystals will effervesce in vinegar, quartz will not. Quartz will scratch calcite. The opposite is not true. Quartz and calcite have different crystal structures and different specific gravities. The list goes on, but if you are trying to distinguish them, the above should help.
Cold dry air
Cold dry air
Quartz, with a hardness of 7, will scratch calcite, with a hardness of 3.
The calcite deposits would likely have undergone metamorphism, transforming into marble due to the high heat and pressure. Marble is a metamorphic rock formed from limestone or dolomite, which are composed primarily of calcite. This process changes the mineral composition and texture of the rock.
A small drop of hydrochloric acid or vinegar would fizz on calcite, not on quartz.Also, quartz has a Mohs hardness of 7 whereas calcite has a hardness of 3. Quartz doesn't have cleavage but calcite has rhombohedral cleavage (skewed square). If the piece of mineral breaks along perfect lines, then it's most likely calcite not quartz. One more thing, if you put the clear calcite on print, like that in a book, you will see a double image through the crystal, an example of double refraction.
Halite is a cleavage because it splits evenly, but fracture would mean it breaks irregularly.
In theory you could in a laboratory if you establish conditions conducive to rapid precipitation and crystallising of the calcite - but I don't know why you would need to when it's easier to analyse natural ones!
Ice crystals and snow pellets are the types pf precipitation that would likely be from the falling cumulus clouds with a ground air temperature of 14 C.