by looseing the soil you have no idea
Some are produced by the eruption of magma (eg volcanoes), others are produced after the magma has cooled to rock. As magmatic rocks are usually hard they resist erosion and cause features such as Arthur's seat or escarpments. Granitic magma gives rise to Tors (such as those on Dartmoor or the Seyshells)
They're hard AND the float on magma.
no, it's molten rock, as in lava....
Magma is underground, when it reaches the surface it becomes lava. So solidified magma is really lava. The lava flow is the liquid lava as it goes down the mountain, when hard its just hardened lava. Magma is underground, when it reaches the surface it becomes lava. So solidified magma is really lava. The lava flow is the liquid lava as it goes down the mountain, when hard its just hardened lava.
When magma crystallizes, igneous rocks are formed. The type of igneous rock that is formed depends on the chemical composition of the magma and the rate at which it cools.
magma or lava.
Some are produced by the eruption of magma (eg volcanoes), others are produced after the magma has cooled to rock. As magmatic rocks are usually hard they resist erosion and cause features such as Arthur's seat or escarpments. Granitic magma gives rise to Tors (such as those on Dartmoor or the Seyshells)
They're hard AND the float on magma.
no, it's molten rock, as in lava....
the crust is hard liquid magma (lava)
no it is made up of lava and magma and also has volcano
well in volcanoes is magma, which when it is no longer in the volcano, is lava. and when a volcano is explosive, in the magma is silica. and silica makes the magma really sticky and thick. in a volcano, the magma comes out of vents at the top. and when magma with silica tries to comes out, it gunks up the vents to where they are clogged and nothing can get out of them. so when this happens, pressures pushes hard to try and get the magma out. then it pushes REALLY hard and it comes out even bigger and destructively! but when there is no silica in the magma, the magma just drizzles out of a volcano but its nonexplosive. hope this helps. and i know this is true. we just learned it in science class. I'm 11 years old but i am certain this is the correct accusation.
Rising tone is when the tone of a sentence rises at the end of the sentence. This is often done in a question - You know her, don't you?It is hard to illustrate here but you could draw a flat line above the first part of the sentence, then from the word don't the line would rise up a little, indicating rising tone
Magma is underground, when it reaches the surface it becomes lava. So solidified magma is really lava. The lava flow is the liquid lava as it goes down the mountain, when hard its just hardened lava. Magma is underground, when it reaches the surface it becomes lava. So solidified magma is really lava. The lava flow is the liquid lava as it goes down the mountain, when hard its just hardened lava.
It is hard not to hate especially when you been harassed or bullied because of who you are. Rising above this means that you don't act like the people who have harassed or bullied you. When people treat you or someone you love cruelly, it is very hard to not hate them. Hate is a complete waste of time. A natural reaction would be to seek vengeance. Vengeance is hate just in a different form. Getting even with those who have hurt you does not lessen the pain you have been subjected to. So much energy and time goes into hating others. There are better ways to use your time and energy than hating them back. People who hate are emotionally immature. They are not adults in their behavior. In the end "Rising above the hate" means that you are better than those who hate. Also "rising above the hate" can be interpreted as not getting in the emotional gutter that haters live.
When magma crystallizes, igneous rocks are formed. The type of igneous rock that is formed depends on the chemical composition of the magma and the rate at which it cools.
Because the magma is erupted into the cold water, the outside of the flow quickly cools and solidifies into a hard shell which causes the backside flow to seek a new, less resistant pathway. When the flow is pinched off before re-routing, a bulbous pillow shaped, rapidly cooling blob is formed. Most of the ocean floor laying under layers of sediment and sedimentary rock, is formed from masses of pillow lavas (basalt).