The fliers below were distributed by two candidates running for the Florida Senate.

ELECT TOM JONES AS STATE SENATOR

* State resident for 12 years

* Graduate of the University of North Florida in Jacksonville

*1 year as volunteer worker for the Red Cross

*3 years as volunteer for the Florida Humane Society

ELECT MARY LAMB AS STATE SENATOR!

* State resident for 10 years

* Graduate of the University of Central Florida in Orlando

* 6 years on City Council

* 2 years as State Representative

Based on the information on the fliers, why might Mary Lamb be considered as more qualified than Tom Jones to be elected as State Senator?

A) She has better views on the major issues.

B) She has better educational qualifications.

C) She has more experience in public office.

D) She has spent more money in the election campaign.

Ringo is the one who has been in a bit more of you to come to my mom said that he has been there before me so happy I have been there before me so happy I have been there before me so happy I have been there before

prime rate/ credit history apex

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)