Using 15 or more terms, adjectives. etc. describing what friendship includes.

amiable

amicable

beautiful

deep

eternal

heartfelt

intimate

lasting

lifelong

loving

mutual

reciprocal

selfless

sincere

steadfast

strong

true

unbounded

uncomplicated

unequalled

wonderful

affable

affectionate

attentive

available

believable

brave

caring

cheerful

considerate

cordial

discerning

easygoing

empathetic

faithful

forgiving

funny

generous

gentle

giving

good listener

honest

humorous

kind

loving

loyal

nice

optimistic

punctual

reliable

responsible

sensitive

sincere

sociable

sweet

sympathetic

tactful

thoughtful

trustworthy

truthful

warm

warm-hearted

winning

imagine me knowing the answer

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)