black
Pink granite typically has a white or light gray streak. The streak color is determined by the mineral composition of the rock, and in the case of pink granite, the dominant minerals such as feldspar and quartz contribute to this lighter streak. This characteristic helps in identifying the rock and distinguishing it from other types of granite.
Jupiter is the largest planet because of it's position in the Solar System. It is located past what is known as the "frost line" [See related link] where it was possible for hydrogen to condense into solid ice grains. because - the then Jupiter - had the "Lions" share of free hydrogen, it grew to an immense size.
it is made out of igneous granite
Mars is the fourth planet from the Sun in our solar system, so it's not the biggest, second biggest, or third biggest planet. The biggest planet is Jupiter, followed by Saturn (second biggest), and then Uranus and Neptune (third and fourth biggest respectively), before we get to Mars.
what does the granite rock look like
Granite does not have rounded grains but contains interlocking grains. An example of a rock with rounded grains is a sandstone.
Large grains, and crystals
Granite is a type of igneous rock that typically has interlocking mineral grains without visible gaps. These interlocked grains give granite its characteristic strength and durability, making it a popular choice for countertops and building materials.
Granite is the rock composed mainly of quartz and potassium feldspar grains.
no
Granite is actually made of mineral grains that are stuck together and solidified. It appears that the name "granite" comes from the based word "grain".
Yes. The grains can be microscopic, as in sandstone, or quite large, as in granite.
Granite typically has a coarse-grained texture, meaning that the individual mineral grains are large enough to be seen with the naked eye. The grains in granite are usually interlocking, giving the rock its strong and durable structure.
The biggest rocks are unfractured granite batholiths.
Granite is a dense, non-porous rock with visible mineral grains. Pumice is a light rock filled with holes left by gas bubbles and generally no visible grains.
They are eather fine grain or course grain. Granite are course Grain, Basalts are fine grains.
The colour of granite does in fact change. For example it will change during the weathering process where feldspar minerals will change to clay minerals such as kaolinite. If the degree of weathering is high this can significantly alter the colour of the granite.