Why did he forbidden his Governors to pass Laws of immediate and pressing importance?

This refers to the policy of requiring the colonial governors or chief executives within each colony to suspend certain kinds of laws passed by the Colonial assemblies until the King should give his assent to them. Sometimes these laws would be neglected by the King for years. Jefferson wrote in his "Summary View of the Rights of British America" (1774): "With equal inattention to the necessities of his people here has his majesty permitted our laws to lie neglected in England for years, neither confirming them by his assent, nor annulling them by his negative

as populations grew, the consent had to be from the governed,or the government

Explanation:

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)