¿QUE PIENSAS DE LA CONTAMINACION VISUAL?
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Explanation:

instruct you on how to draw his/her picture. For example, if they drew a bird, they are going to tell you, step by step, how to draw that bird. They cannot, however, tell you what you are drawing. They can say "draw a small line in the middle of your paper, then connect another line going down from that one." They cannot say "draw a head and a beak and wings." At the end of the allotted time, compare drawings. See if your version of their picture looks the same as theirs. Step 5: Switch roles. Now it is your turn to explain how to draw your picture to your partner as he/she attempts to recreate it. Again, give clear step by step directions. You are not allowed to tell him/her what he/she is drawing. After 5-10 minutes, compare drawings yet again. Step 6: Discuss and reflect. Discuss with your partner the outcome of this activity. What did you learn? In 5-7 sentences, write a reflection about this activity. Were you better at giving instructions or receiving them? If you could do this again, how might you improve your instructions? How might you improve your listening skills? How can this apply to any group activity

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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)