yes
wind
Pumice would fit the description of a gas filled extrusive igneous rock that cools quickly.
Basalt cools fast because it is at the surface, where air carries heat away rather quickly.
glassy texture, hope this helps :)
True because my partner and i read a paragraph about lava and we are writing
They are cause because land heats and cools more quickly.
They are sea breezes.
alright, if it cools quickly it will form pumice because of the bubbles in it. if it cools slowly, it will form obsidian.
Land and sea breezes occur because of the different heating rates of land and sea. A sea breeze or onshore breeze is a gentle wind blowing from sea toward land. They develop when the land heats up and the air above the land rises, air then moves from the sea towards the land. A land breeze or offshore breeze, blowing from land to sea, is the reverse effect, caused when land cools more quickly than water in the evening.
Land and sea breezes occur because of the different heating rates of land and sea. A sea breeze or onshore breeze is a gentle wind blowing from sea toward land. They develop when the land heats up and the air above the land rises, air then moves from the sea towards the land. A land breeze or offshore breeze, blowing from land to sea, is the reverse effect, caused when land cools more quickly than water in the evening.
Andesite has small crystals because it cools quickly.
Land breezes are generic things. They don't have specific names. They blow at evening from the land to the sea, hence their name. They arise because the land cools down more quickly than the sea and so the air over the sea is warmer than that over the land. The air over the sea rises so the air from the land moves in to replace it.
because at night the sea cools slower than the land and the uneven heating causes it to bring the air to the sea. and vice versa for the day time and the night timeland breezes happen during the day because the temperature is higher, and land breezes at night when the temperature is lower.
wind
Mountain and valley breezes are other examples of local winds caused by an area's geography. Campers in mountains areas may feel warm afternoon quickly change into cold night soon after the sun sets. During the day, the sun warms the air along the mountain slopes. This warm air rises up the mountain slopes, creating a valley breeze. At nightfall, the air along the mountain slopes cools. This is cool air moves down the slopes into the valley, producing a mountain breeze.
Mountain and valley breezes are other examples of local winds caused by an area's geography. Campers in mountains areas may feel warm afternoon quickly change into cold night soon after the sun sets. During the day, the sun warms the air along the mountain slopes. This warm air rises up the mountain slopes, creating a valley breeze. At nightfall, the air along the mountain slopes cools. This is cool air moves down the slopes into the valley, producing a mountain breeze.
It depends on the time of day. The ground heats up and cools more quickly than the sea. When the ground has warmed up more than the sea then air moves towards the land from the sea and heads upwards in a thermal and then downwards again out to sea. At night the opposite happens, as the ground cools the cold air flows down to the sea and again upwards in a thermal. Night sea breezes are usually less windy than in the day as the sun is not pumping energy into the systemRead more: What_direction_does_a_sea_breeze_blow