The government gives public funds to low-performing
schools for new computers. they decide to give more
money to the lowest performers, some of which happen to
promote multidenominational religions.
according to the establishment clause, how would a court
rule on this case?
as a direct violation of the clause because government
institutions cannot support religious institutions for any
reason
as a violation of the clause because the government
gave more money to religious schools than public
schools
as in compliance with the clause because the
government's action was for a secular purpose did not
advance a particular religion, and was unentangled
as in compliance with the clause because the
government gave money to fewer religious schools than
public schools

According to the establishment clause, the court would rule out the government action as in compliance with the clause because the  government's action was for a secular purpose did not  advance a particular religion, and was unentangled

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)