Using the ideas from your Narrative Organization Chart. write the introduction to your narrative. Be sure to select your story’s narrator and maintain that point of view. Review the story and writing prompt on which your chart was based.

Write an introduction of 100 words in more. Remember to:

introduce the character

establish the setting

hook your reader with an interesting quote, a vivid description, or an interesting or outlandish fact

The correct answer to this open question is the following.

Unfortunately, you did not attach your Narrative Organization Chart. That is why we are going to use our Narrative Organization Chart to help you answer this question.

This is my introduction of 100 words.

Not all tje stories are easy to tell. This is one of those.

"Chip," they call me. Since I was a boy I remember to be called Chip.  I do not why because my real name Jim.

But that comes in another part of this story.

I have lived in Villagetown all my life and I have witnessed with my own eyes the story I am about to tell. No from third persons, no from books. I was there, I see it, and I was part of it.

Now, 35 years later, Villagetown is not the same.

So long ago, before these incidents, I am about to tell, Villagetown used to be a quiet country town. We could say my town could have been the perfect place for a love story. A town surrounded by pine trees in the middle of the forest, very close to "Cold River," named cold because the water comes from the mountains and is very cold.

That was Village town until that Tuesday morning, the first day of Fall, when, for the first in years, the water of Cold River had that strange odor ...and color.

more than 1 person for sure

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)