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GalinKa [24]
3 years ago
15

Which contributions of ancient Greece still influence the modern world? Choose all answers that are correct. philosophy literatu

re religion government
Geography
2 answers:
shusha [124]3 years ago
7 0

Answer:

The good answers are philosophy, literature and  government.

Explanation:

Greek philosophy is the foundation of Western philosophy; Greek comedies and tragedies are Western classics, and democracy as a form of government was born in ancient Greece.

AnnZ [28]3 years ago
5 0

Answer:

  • philosophy
  • literature
  • religion

Explanation:

  • In the ancient Greece, religion ideas that were linked to the Christianity were promoted, as the Aristotle envision of the perfect god, were considered virtues in heaven and in terms of the philosophy they gave birth to the scientific thoughts and observations that made through the various development of the theories like those of Thales and the Alexandrian, have contributed to the field of the science, maths, and philosophy.
  • <u>Greece has remarkable literature that is marked as more than 2800 years old as the beginning of the classical era the epic poem of the homer and the Herodotus is credited with the development of the modern society of history.</u>
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The popular theory of drifting continents and oceans is called "plate tectonics."1 (Tectonics is the field of geology which studies the processes which deform the earth’s crust.) The general tenets of the popular theory may be stated as follows. The outer lithospheric shell of the earth consists of a mosaic of rigid plates, each in motion relative to adjacent plates. Deformation occurs at the margins of plates by three basic types of motion: horizontal extension, horizontal slipping, and horizontal compression. Sea-floor spreading occurs where two plates are diverging horizontally (e.g., the Mid-Atlantic Ridge and East Pacific Rise) with new material from the earth's mantle being added between them to form a new oceanic crust. Transform faulting occurs where one plate is slipping horizontally past another (e.g., the San Andreas fault of California and the Anatolian fault of northern Turkey). Subduction occurs where two plates are converging with one plate underthrusting the other producing what is supposed to be compressional deformation (e.g., the Peru-Chile Trench and associated Andes Mountains of South America). In conformity with evolutionary-uniformitarian assumption, popular plate tectonic theory supposes that plates move very slowly — about 2 to 18 centimeters per year. At this rate it would take 100 million years to form an ocean basin or mountain range.

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The idea that the continents can be fitted together like a jigsaw puzzle to form a single super continent is an old one. Especially interesting is how the eastern "bulge" of South America can fit into the southwestern "concavity" of Africa. Recent investigators have used computers to fit the continents. The "Bullard fit"2 gives one of the best reconstructions of how Africa, South America, Europe, and North America may have once touched. There are, however, areas of overlap of continents and one large area which must be omitted from consideration (Central America). There are a number of ways to fit Africa, India, Australia, and Antarctica (only one can be correct!). Reconstructions have been shown to be geometrically feasible which are preposterous to continental drift (e.g., rotation of eastern Australia fits nicely into eastern North America).3

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