Rather than using a case efficiency model of justice, courts make problem-solving their primary goal and orient their proceedings toward social justice.

Specialized

Explanation:

Specialized courts is the law court that closely works along the base of jurisdiction so all the cases related with jurisdiction are forwarded towards this court. These courts have well knowledgeable and specialist judge for making decision on jurisdiction matter.

They are supposed to be efficient as these courts tend to decrease the amount of criminal activities in future as they focus on social justice by addressing reason and circumstances under which the person commits the crime or behaves as a criminal.E.g:- mental health courts, domestic violence court.

me no say

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)