Can someone me quick
compare relations between parliament and king james ii to parliament’s relationship to king james i.

At first, James I established quite acceptable relations with the first parliament of 1604–1610. But the Crown’s ever-increasing need for money and James I’s persistent desire to subordinate parliament to his power constituted a serious threat to this cooperation. Members of the House of Commons were particularly acutely displeased. They boycotted the plans of James I to unite England and Scotland, as well as the Great Contract. The parliamentarians defended their rights: for example, in 1604, the king objected to the election of Francis Goodwin, a very dubious person, to parliament. Members of the House of Commons forced James to accept this appointment, thereby creating an important precedent for resolving controversial issues in parliamentary elections. The second parliament was even less successful. It did not last long and did not actually adopt a single law, for which it received the name "Spoiled". After its dissolution in 1614, the king until 1621 preferred to rule without parliament.

James II was an active and powerful man, but too straightforward. He did not like parliament and clearly showed a penchant for Catholicism. After suppressing the revolt of his half-brother James Crofts in 1685, he further increased the army, mainly due to Catholic officers from Scotland and Ireland. Soon, Catholics again gained the right to hold public office and head departments in universities. In 1687 and 1688 declarations of tolerance were issued, which, however, exacerbated the situation. The bishops who opposed them were imprisoned in the Tower. Parliament, which tried in response to the king’s abuses to strip it of subsidies, was dissolved.

Explanation:

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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)