What did scientists learn from the information found on seismographs? how deep the ocean is the structure of the earth's crust the depth and density of earth's layers the elements present in the interior

The correct answer is the depth and density of the Earth's layer.  

An instrument used for measuring seismic or earthquake waves is known as a seismograph. They are held in a very solid alignment, either on a concrete base or on the bedrock. The seismograph itself comprises a frame and a mass, which can move comparatively to it.  

A seismograph records and measures seismic waves, which move through the Earth as a consequence of an earthquake. Thus, it can provide information on the depth and density of the Earth's layers.  

well, you see. the answer to your question is quite simple. the thing that is big, powerful, and over 9,000 is your mom.

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]