To what, under which conditions?
2691- Solid slate. 1290-1450- Broken slate. 1362- Pulverized slate. 2691- Solid slate. 1290-1450- Broken slate. 1362- Pulverized slate.
To clean slate, mix a bit of lemon juice, vinegar, and baking soda and make a paste. Rub the mixture on the slate and then rinse off.
The object will accelerate.
If you increase the force on an object acceleration increases . As F = m*a, where F = Force , m = mass of the object & a = acceleration
The slate or slate changes into schist
it melts
Slate is a type of metamorphic rock that does not have the ability to change or adapt to weather conditions. It is a durable material often used in roofing or as a writing surface due to its resistance to weathering.
When slate is heated, it expands due to the thermal energy causing the mineral grains to separate. This expansion can lead to cracks or breakage in the slate. Additionally, heating slate can alter its mineral composition and structure, affecting its physical and chemical properties.
Slate typically fractures along flat, thin planes due to its foliated structure, creating smooth surfaces. This type of fracture is known as "conchoidal fracture," which results in thin, sharp fragments when the slate is broken.
The process is called Metamorphosis of Rocks. When the slate goes under the conditions of high pressure and heat it changes to schist or gneiss. Type of slate decide whether it gonna be schist or gneiss.
Slate flooring tile offers durability, a natural and unique appearance, easy maintenance, and can increase the value of your home.
Phyllite is a type of metamorphic rock that comes from adding heat, pressure, and/or chemically active fluids to slate. Slate is the parent, or originial, type of rock from which the phyllite forms. It could also be said that slate recrystallizes into phyllite. Slate is also a metamorphic rock that starts out as the sedimentary rock called shale. Therefore, phyllite comes from slate, which comes from shale. Phyllite is different from slate because it has been metamorphosed more. As a result, the straight lines/planes (called foliation) that slate breaks along, are absent in phyllite, which is distinctly wavy in appearance. If more metamorphism is applied to phyllite, it recrystallizes into schist.
Slate is a popular choice for roofing due to its durability, longevity, and fire resistance. It also offers a natural, elegant appearance that can enhance the overall aesthetics of a building. Additionally, slate is low maintenance and can withstand harsh weather conditions.
The most common roofing slates is Welsh slate. This type of slate has been used for many years and is very common around many houses in the UK. Slate is very common due to how well it reacts to weather conditions.
Slate starts as clay. Thhrough erosion and nature, the clay can change to shale or slate. Shale happens when layers upon layers are of clay and sediment are piled together and held in place with something very very heavy. Slate is altered shale that had low heat and not very much pressure put on it. It takes thousands of years for slate to change. Slate can be any color but is mostly found in gray or black. When it is broken, it splits into layers.
Slate forms under high temperatures and pressure, typically around 200 to 700 degrees Celsius. These conditions cause the original clay minerals in shale to recrystallize into a low-grade metamorphic rock known as slate.