When President Andrew Jackson vetoed the extension of the Second National Bank’s charter, the national bank was divided up and taken over by state banks. had to borrow money to continue operating. ceased to operate once its charter expired. had its charter renewed by popular vote.

C. ceased to operate once its charter expired.

Explanation:

President Andrew Jackson was born on the 5th of March, 1767 in the old British America and died on the 8th of June, 1845 in Tennessee, USA.

During his tenure as the seventh president of the United States of America (1829-1837), President Andrew Jackson was mockingly being referred to by his critics as "King Andrew I" due to his style of leadership and rash display of power (authoritarianism) without recourse to the US Congress.

He opined that the second bank of the united states was typically a corrupt financial institution that was beneficial to the rich and wealthy people living in America at the detriment of the ordinary citizens who were poor and as a result, President Jackson vetoed the extension of the bank's charter.

When President Andrew Jackson vetoed the extension of the Second National Bank’s charter, the national bank ceased to operate once its charter expired because they were considered by President Jackson to only make the rich more wealthy and the potent to be more powerful.

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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)