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TEA [102]
3 years ago
14

In what way does renewable energy differ from nonrenewable energy?

Geography
2 answers:
Alla [95]3 years ago
4 0

Answer:

mark brainliest

Explanation:

Nonrenewable energy resources, like coal, nuclear, oil, and natural gas, are available in limited supplies. This is usually due to the long time it takes for them to be replenished. Renewable resources are replenished naturally and over relatively short periods of time.

Free_Kalibri [48]3 years ago
3 0

Answer:

Most important difference is that renewable energy are energy that are replenished after usage on a human time scale  while non renewable energy are not replenish after usage . it takes eons. This energy source are limited

Explanation:

Renewable energy are natural source of energy that are usually clean. These energy source are easily replenished on a human time scale even after prolonged excessive usage. Generally, this energy are produced from sources that do not deplete when used and are replenished on a human scale.  Examples of renewable sources of energy are sunlight , wind energy , hydro thermal, geothermal and biomass.

<h2>While </h2>

Nonrenewable energy are energy that are usually refereed to as dirty source of energy because of the negative impact it has on the environment . These energy source are limited and are not replenished by natural process on a human time scale. This energy is a source of energy that will eventually run out. This energy source are not replenished with the speed at which they are been consumed. New supplies of this energy takes eons(thousand or millions of years). Examples of non renewable energy sources is fossil fuels like coal, gas and oil.    

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A rupture in Rodinia 750 million years ago formed a passive margin in the eastern Pacific Northwest. The breakup of Pangea 200 million years ago began the westward movement of the North American plate, creating an active margin on the western continent. As the continent drifted West, terranes were accreted onto the west coast. The timing of the accretion of the insular belt is uncertain, although the closure did not occur until at least 115 million years ago.Other Mesozoic terranes that accreted onto the continent include the Klamath Mountains, the Sierra Nevada, and the Guerrero super-terrane of western Mexico.80 to 90 million years ago the subducting Farallon plate split and formed the Kula Plate to the North. This formed an area in what is now Northern California, where the plates converged forming a Mélange. North of this was the Columbia Embayment, where the continental margin was east of the surrounding areas.Many of the major batholiths date from the late Cretaceous. As the Laramide Orogeny ended around 48 million years ago, the accretion of the Siletzia terrane began in the Pacific Northwest. This began the volcanic activity in the Cascadia subduction zone, forming the modern Cascade Range, and lasted into the Miocene. Events here may relate to the ignimbrite flare-up of the southern Basin and Range. As extension in the Basin and Range Province slowed by a change in North American Plate movement circa 7 to 8 Million years ago, rifting began on the Gulf of California.

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Answer:

As given as under.

Explanation:

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