Did you know that millions of years ago the Earth only had one super continent? If you look at a globe today, you’d notice how continents fit into each other like puzzle pieces. But how did the super continent break apart and become seven different continents? Let’s look at the mechanics of the continental drift in this book for fifth graders. Grab a copy today.
Did you know that millions of years ago the Earth only had one super continent? If you look at a globe today, you'd notice how continents fit into each other like puzzle pieces. But how did the super continent break apart and become seven different continents? Let's look at the mechanics of the continental drift in this book for fifth graders. Grab a copy today.
Explores the Supercontinent Cycle from the earliest recorded time to the geological discoveries of today including the drifting of the continents and the evolution of dinosaurs.
Learn how the continents have changed throughout time and how continental drift has influenced the world we live in today! Explore how the continents have drifted, from the Devonian Era to the Jurassic Period, to form the world as we know it! This beautiful book will take readers through different periods and explore the ecosystems and conditions of each time and how the changes led to where we are now. Learn about sea life, insects, animals, plants, rocks, and more! This book will be sure to capture the attention of young readers and educate them in the process!
A source of profound influence and controversy, this landmark 1915 work explains various phenomena of historical geology, geomorphy, paleontology, paleoclimatology, and similar areas in terms of continental drift. 64 illustrations. 1966 edition.
Travel with me, if you will, on this incredible journey spanning millions of years from when Pangea begin its development towards becoming a single, supercontinent to its break up to form what we know as todays' seven continents, each rich in treasure. Detect, if you can, the unique secrets left behind in Pangea's wake that will lead us to hidden treasures and hidden dangers. Do not delay your journey, for others are trying to discover the still hidden treasures and hidden dangers. Will you be next to find unimaginable wealth? Will you be able to detect the hidden dangers?
To this day, there is a great amount of controversy about where, when and how the so-called supercontinents--Pangea, Godwana, Rodinia, and Columbia--were made and broken. Continents and Supercontinents frames that controversy by giving all the necessary background on how continental crust is formed, modified, and destroyed, and what forces move plates. It also discusses how these processes affect the composition of seawater, climate, and the evolution of life. Rogers and Santosh begin with a survey of plate tectonics, and go on to describe the composition, production, and destruction of continental and oceanic crust, and show that cratons or assemblies of cratons became the first true continents, approximately one billion years after the earliest continental crust evolved. The middle part of the book concentrates on supercontinents, beginning with a discussion of types of orogenic belts, distinguishing those that formed by closure of an ocean basin within the belt and those that formed by intracontinental deformation caused by stresses generated elsewhere. This information permits discrimination between models of supercontinent formation by accretion of numerous small terranes and by reorganization of large old continental blocks. This background leads to a description of the assembly and fragmentation of supercontinents throughout earth history. The record is most difficult to interpret for the oldest supercontinent, Columbia, and also controversial for Rodinia, the next youngest supercontinent. The configurations and pattern of breakup of Gondwana and Pangea are well known, but some aspects of their assembly are unclear. The book also briefly describes the histories of continents after the breakup of Pangea, and discusses how changes in the composition of seawater, climate, and life may have been affected by the sizes and locations of continents and supercontinents.
The Pulitzer Prize-winning view of the continent, across the fortieth parallel and down through 4.6 billion years Twenty years ago, when John McPhee began his journeys back and forth across the United States, he planned to describe a cross section of North America at about the fortieth parallel and, in the process, come to an understanding not only of the science but of the style of the geologists he traveled with. The structure of the book never changed, but its breadth caused him to complete it in stages, under the overall title Annals of the Former World. Like the terrain it covers, Annals of the Former World tells a multilayered tale, and the reader may choose one of many paths through it. As clearly and succinctly written as it is profoundly informed, this is our finest popular survey of geology and a masterpiece of modern nonfiction. Annals of the Former World is the winner of the 1999 Pulitzer Prize for Nonfiction.
Fifty years ago, no one could explain mountains. Arguments about their origin were spirited, to say the least. Progressive scientists were ridiculed for their ideas. Most geologists thought the Earth was shrinking. Contracting like a hot ball of iron, shrinking and exposing ridges that became mountains. Others were quite sure the planet was expanding. Growth widened sea basins and raised mountains. There was yet another idea, the theory that the world's crust was broken into big plates that jostled around, drifting until they collided and jarred mountains into existence. That idea was invariably dismissed as pseudo-science. Or "utter damned rot" as one prominent scientist said. But the doubtful theory of plate tectonics prevailed. Mountains, earthquakes, ancient ice ages, even veins of gold and fields of oil are now seen as the offspring of moving tectonic plates. Just half a century ago, most geologists sternly rejected the idea of drifting continents. But a few intrepid champions of plate tectonics dared to differ. The Mountain Mystery tells their story.
Some 250 million years ago, at the beginning of the Mesozoic era, the world's continents were grouped into a single supercontinent known as Pangaea. This publication contains information on the key stages in the break-up of this supercontinent into the geological face of the Earth as we know it today. It includes 11 maps, based on recent scientific work, with explanatory notes, a glossary of terms and a CD-ROM of the map images in bmp, tiff, pict and powerpoint formats.