Rocks are formed from the chemical compounds known as minerals - metal-silicates, carbonates, sulphates etc.
You will also find secondary emplacement of minerals in fractures or other cavities in existing rocks, creating geodes, veins (including ore-bodies) etc.
Yes, mineral veins are often formed when minerals from a solution deposit within fractures or faults in rocks. This usually occurs when mineral-rich fluids flow through cracks and fissures in the Earth's crust and deposit minerals as the fluids cool and/or react with surrounding rock. Over time, this process can lead to the formation of mineral veins.
The mineral is called garnet. It is commonly used as an indicator mineral in metamorphic rocks to determine the temperature and pressure conditions under which the rock formed, due to its specific stability range.
Minerals can occur in various modes, including as crystals within rocks, as grains or nodules in sedimentary rocks, as veins cutting across rocks, or as disseminated particles within a rock mass. The mode of occurrence depends on the geological processes that formed the mineral deposit and can provide insights into the mineral's formation history and geological context.
A long narrow deposit of a mineral in rock is typically referred to as a vein. Veins are formed when minerals are transported by fluids and deposited in cracks or fissures within existing rock formations. These deposits can be valuable sources of various minerals and metals.
Yes! It is rock that is not ore, but surrounds the ore.
An ore is a naturally occurring material from which a metal or valuable mineral can be extracted, while a lode is a deposit of ore found in a fissure or crack within a rock formation. Essentially, a lode is a layer or vein of ore within a larger mineral deposit.
The homophone for "load" is "lode." A "lode" is a mineral deposit found in a rock formation.
Yes, mineral veins are often formed when minerals from a solution deposit within fractures or faults in rocks. This usually occurs when mineral-rich fluids flow through cracks and fissures in the Earth's crust and deposit minerals as the fluids cool and/or react with surrounding rock. Over time, this process can lead to the formation of mineral veins.
The word you are looking for is "vein." A vein is a deposit or mass of a particular mineral embedded within a rock or the Earth's surface.
You can call it "Ore" or even "Mineral deposit"!
Overburden soil refers to the layer of soil and rock that sits above a mineral deposit or bedrock. It needs to be removed during mining or excavation activities to access the desired materials underneath. The overburden soil is usually of lower economic value compared to the underlying mineral deposits.
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The mineral is called garnet. It is commonly used as an indicator mineral in metamorphic rocks to determine the temperature and pressure conditions under which the rock formed, due to its specific stability range.
Minerals can occur in various modes, including as crystals within rocks, as grains or nodules in sedimentary rocks, as veins cutting across rocks, or as disseminated particles within a rock mass. The mode of occurrence depends on the geological processes that formed the mineral deposit and can provide insights into the mineral's formation history and geological context.
The conditions under which the rock forms, such as temperature, pressure, and the composition of the mineral-rich fluid, can influence how long it takes for minerals to form within a rock. The rate of cooling and crystallization of magma or lava can also affect the timing of mineral formation within a rock. Additionally, factors like the presence of nucleation sites or impurities in the rock can impact the speed of mineral growth.
A long narrow deposit of a mineral in rock is typically referred to as a vein. Veins are formed when minerals are transported by fluids and deposited in cracks or fissures within existing rock formations. These deposits can be valuable sources of various minerals and metals.