What did the case of Marbury v. Madison establish for the courts, and what does that mean?
A) Equal power for the legislative and executive branches of government was established, which means both had to follow the laws outlined in the Constitution.

B) "Due process" was established, which means the government must respect all of the legal rights owed to a person under the Constitution, even if that person is accused of a crime.

C) "Freedom of Expression" was established, which means citizens can seek, receive, and impart information orally, or in writing, without censorship.

D) The court's power of judicial review was established, which means the court has the power to review and determine if laws or acts of government are unconstitutional.

the answer I got was D o.o

D) The court's power of judicial review was established, which means the court has the power to review and determine if laws or acts of government are unconstitutional.

Explanation:

Marbury v. Madison was a court ruling that led to the established principle of judicial reveiw

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)