The "psycho" theme, for all its startling originality, owes a debt to the great russian composer, igor stravinsky, whose 1913 ballet, the rite of spring, radically transformed the world of classical music. what made stravinsky's music so different?

Correct Igor Stravisnky's great diversity of music styles.

Explanation:

The Russian composer Igor Stravinsky has been recognized as the most important figure in the musical panorama of the 20th century. His influence on the development of the new currents of the twentieth century resembles that of the painter Pablo Picasso in the plastic arts. Much of his life has been narrated by the author himself in the book "Stravinsky: an autobiography", published in New York in 1939. Stravisnky's great diversity of music styles, from baroque music to dodecaphonism, makes each of his works different but always maintaining a great personality.

answer; i believe the first answer to be (independent; /// and the second answer is (french); good luck

the earth’s crust is broken into separate pieces called tectonic plates (fig. 7.14). recall that the crust is the solid, rocky, outer shell of the planet. it is composed of two distinctly different types of material: the less-dense continental crust and the more-dense oceanic crust. both types of crust rest atop solid, upper mantle material. the upper mantle, in turn, floats on a denser layer of lower mantle that is much like thick molten tar.

each tectonic plate is free-floating and can move independently. earthquakes and volcanoes are the direct result of the movement of tectonic plates at fault lines. the term fault is used to describe the boundary between tectonic plates. most of the earthquakes and volcanoes around the pacific ocean basin—a pattern known as the “ring of fire”—are due to the movement of tectonic plates in this region. other observable results of short-term plate movement include the gradual widening of the great rift lakes in eastern africa and the rising of the himalayan mountain range. the motion of plates can be described in four general patterns:

collision: when two continental plates are shoved together

subduction: when one plate plunges beneath another (fig. 7.15)

spreading: when two plates are pushed apart (fig. 7.15)

transform faulting: when two plates slide past each other (fig. 7.15)