Which characteristic did Chandragupta Maurya and Aśoka have in common? They both converted to Buddhism. They both formed alliances with the Greeks. Which characteristic did Chandragupta Maurya and Aśoka have in common? They both converted to Buddhism. They both formed alliances with the Greeks. They both embraced nonviolence later in life. They both carved edicts into rocks and pillars. They both embraced nonviolence later in life. They both carved edicts into rocks and pillars.

They both embraced nonviolence later in life

Explanation:

Chandragupta Maurya who reigned between 321 to 297 BCE was known as the founder of the Maurya Empire. He was popular in conquering the territories around him. However, based on the historical account, it was revealed that in his attempt to embrace nonviolence later in life, he left his empire and later turn to Jian Monk.

Similarly, Asoka who reigned between 268 to 232 BCE was known as the last empire of the Maurya empire. During his reign he was known to have conquered many places, however, following the battle of Kalinga, he also embraces nonviolence by joining Buddhism.

a factory opens that mass-produces light bulbs.

explanation:

not sure if that's an answer to your questions but this is an example! : )

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)