Arrange the events to describe how a volcano forms and erupts. the plates move constantly. molten magma flowing beneath earth's surface finds its way out of the gaps. the mound cools down over thousands of years to form a mountain. the heap grows bigger and bigger as the volcano erupts, creating a huge mound. at times, the plates move away from each other, creating gaps. earth's crust is made up of huge slabs called plates. magma comes out of earth, creating a heap of lava, ash, and rocks.

Earths chest is made up of huge slabs called plates

Thé plates move constantly

At times the plates move away from each other creating gaps

Molten magma flowing beneath earths surface finds its way out of the gaps

Magma comes out of earth creating a heap of lava ash and rocks

The heap grows bigger and bigger as the volcano erupts creating a huge mound

The mound cools down over thousands of years to form a mountain

Explanation:

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a fossil fuel is a fuel formed by natural processes, such as anaerobic decomposition of buried dead organisms, containing energy originating in ancient photosynthesis.[1] the age of the organisms and their resulting fossil fuels is typically millions of years, and sometimes exceeds 650 million years.[2] fossil fuels contain high percentages of carbon and include petroleum, coal, and natural gas.[3] other commonly used derivatives include kerosene and propane. fossil fuels range from volatile materials with low carbon to hydrogen ratios like methane, to liquids like petroleum, to nonvolatile materials composed of almost pure carbon, like anthracite coal. methane can be found in hydrocarbon fields either alone, associated with oil, or in the form of methane clathrates.

the theory that fossil fuels formed from the fossilized remains of dead plants by exposure to heat and pressure in the earth's crust over millions of years was first introduced by andreas libavius "in his 1597 alchemia [alchymia]" and later by mikhail lomonosov "as early as 1757 and certainly by 1763".[4] the first use of the term "fossil fuel" was by the german chemist caspar neumann, in english translation in 1759.[5]

in 2017 the world's primary energy sources consisted of petroleum (34%), coal (28%), natural gas (23%), amounting to an 85% share for fossil fuels in primary energy consumption in the world.[6] non-fossil sources in 2006 included nuclear (8.5%), hydroelectric (6.3%), and others (geothermal, solar, tidal, wind, wood, waste) amounting to 0.9%.[7] world energy consumption was growing at about 2.3% per year. in 2015 about 18% of worldwide consumption was from renewable sources.[8]

unicellular organisms, like bacteria, are able to perform all life functions within one single cell. multicellular organisms need many different types of cells to carry out the same life processes. each of these special types of cells has a different structure that it perform a specific function.