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Historians use coins, inscriptions, and manuscripts for reconstructing the history of ancient period. Very few original manuscripts are available and manuscripts which are available are the reproduction of scribes and some times information provided in these sources are not reliable. As scribe fails to understand the information given in the Historical text which led to the misinterpretation of facts. And moreover there is a lack of continuity as text do not follow time line.

In Medieval period use of paper to issue Royal orders began instead of inscriptions. As paper has less durability than inscription caused the discontinuity in the availability of historical source.

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Anonymous

4y ago

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Is the lehmann discontinuity 220 km beneath the Gutenberg discontinuity?

No, the Lehmann discontinuity is believed to be located between 220 km and 260 km beneath the Earth's surface. The Gutenberg discontinuity, on the other hand, sits at a depth of around 2,900 km.


The seismic discontinuity at the base of the crust is known as?

The seismic discontinuity at the base of the crust is known as the Mohorovičić discontinuity, or Moho for short. It marks the boundary between the Earth's crust and the underlying mantle, where seismic waves experience a sudden change in velocity.


How is the crust separated from mantel?

The crust and the mantle are separated by the Mohorovičić discontinuity, also known as the Moho. This is a boundary that marks the change in composition and density between the Earth's crust and mantle. Seismic waves help scientists study and understand this separation.


mohorovicic discontinuity?

interface between the crust and the upper mantle


Is Gutenberg discontinuity and Conrad discontinuity same!?

No, the Gutenberg discontinuity and the Conrad discontinuity are not the same. The Gutenberg discontinuity refers to the boundary between the Earth's crust and the underlying mantle, located at a depth of about 30 to 50 kilometers. In contrast, the Conrad discontinuity is the boundary within the crust, separating the upper crust from the lower crust, typically found at depths of about 10 to 20 kilometers. Both discontinuities are important in understanding the Earth's internal structure, but they occur at different depths and represent different geological layers.

Related Questions

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The Discontinuity Guide was created in 1995.


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Corroborated sources of historical evidence. (APEX) !/


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The Discontinuity Guide has 357 pages.


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The "sources of equipment" I understand it as where did he get the equipment from?


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The Mohorovičić Discontinuity, also called the Moho Discontinuity, was named for Andrija Mohorovičić, the Croatian seismologist who first identified it in 1909.


What word will you get when you unscramble this word dustointinyic?

The unscrambled word is discontinuity.


What are the 2 classifications of historical sources?

The two classifications of historical sources are primary sources and secondary sources. Primary sources are original, first-hand accounts of an event or topic, while secondary sources are interpretations or analyses of primary sources created by someone not directly involved in the event.