How Mountains Are Made

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Overview

Even though Mount Everest measures 29,028 feet high, it may be growing about two inches a year. A mountain might be thousands of feet high, but it can still grow taller or shorter each year. Mountains are created when the huge plates that make up the earth's outer shell very slowly pull and push against one another. Read and find out about all the different kinds of mountains.

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More About This Book

Overview

Even though Mount Everest measures 29,028 feet high, it may be growing about two inches a year. A mountain might be thousands of feet high, but it can still grow taller or shorter each year. Mountains are created when the huge plates that make up the earth's outer shell very slowly pull and push against one another. Read and find out about all the different kinds of mountains.

Editorial Reviews

Children's Literature
This book explains a big subject to little people. A group of kids hikes up a mountain and discover an ocean fossil. In learning why a fossil was on the mountain, they also learn about the four different types of mountains: folded, dome, fault-block, and volcanic. The kids discover that mountains are hardly static: some are shrinking, through the long-term effects of rain, wind and ice, while others are growing. Mt. Everest may be rising as much as 2 inches a year. This is a nice presentation of the complex geologic workings of our planet and gives kids manageable ways to think about the vast piles of rock that we call mountains. "Let's-Read-&-Find-Out Science" series-Stage 2.
School Library Journal
Gr 2-3In this clear, concise presentation, four children introduce the subject of mountain formation by taking a hike in their local community. The youngsters appear throughout the book, commenting in dialogue bubbles about specific facts, giving demonstrations of ways mountains change, or making humorous asides. They provide continuity and keep the tone light while information is related to explain why fossils of sea animals are found atop mountains, the various layers in the earth, why volcanoes form, and the effects of erosion. The text and illustrations work together well in this sequential, well-organized book. Much credit goes to Hale's engaging watercolor illustrations done in cheery colors; they are simply drawn but add effective examples and diagrams. Used with Franklyn Branley's Volcanoes (HarperCollins, 1985), this fine addition to the science series would be of value to students interested in the geology and the changes of planet Earth.Diane Nunn, Richard E. Byrd Elementary School, Glen Rock, NJ

Product Details

  • ISBN-13: 9780064451284
  • Publisher: HarperCollins Publishers
  • Publication date: 3/28/1995
  • Edition number: 1
  • Pages: 32
  • Sales rank: 321,736
  • Age range: 5 - 8 Years
  • Lexile: 620L (what's this?)
  • Series: Let's-Read-and-Find-Out Science 2 Series
  • Product dimensions: 9.81 (w) x 8.00 (h) x 0.07 (d)

Meet the Author

Kathleen Zoehfeld

Kathleen Weidner Zoehfeld is the award-winning author of more than sixty books, including Dinosaur Tracks, "a great choice for even the most discriminating dinophiles" (School Library Journal); Did Dinosaurs Have Feathers?, a Children's Book of the Month Club selection described as "fascinating" by Kirkus Reviews; and Dinosaurs Big and Small, a 2003 Oppenheim Toy Portfolio Best Book Award winner. When she's not reading, researching, writing, or editing, Kathleen loves to spend her free time exploring, doing fieldwork, and preparing fossils in the laboratory for her local natural history museums. She lives in Berkeley, California.

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  • Anonymous

    Posted May 3, 2008

    Inaccurate and misleading

    The model of the Earth's interior illustrated and described in this book is wrong and leads to numerous other conceptual errors throughout the book. The book claims that there is a molten magma layer beneath the upper 95 mile thick lithosphere of the Earth. This is false. The layer of the Earth beneath the lithosphere is the asthenosphere, which is a solid that flows on very long time scales - it is not a liquid magma. In addition to other misleading and inaccurate statements throughout the text, the illustrations are sure to create misconceptions among children. For example, one illustration shows a volcano at Earth's surface that is directly fed by the misinterpreted magma layer deep beneath the Earth's lithosphere, and leads one to believe that when the entire 95-mile thick lithosphere cracks, liquid magma suddenly shoots up from below. A quick comparison between the model of the Earth presented in this book and that presented in modern geology textbooks, or Wikipedia for that matter, will hopefully convice existing owners of this book that it is deeply flawed.

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