The book requires only rudimentary physics knowledge but ability to program computers creatively and to keep the mind open to simple and not so simple models, based in individuals, for the living world around us.
* Interdisciplinary coverage
* Research oriented
* Contains and explains programs
* Based on recent discoveries
* Little special knowledge required besides programming
* Suitable for undergraduate and graduate research projects

Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 138.Subduction zones helped nucleate and grow the continents, they fertilize and lubricate the earth's interior, they are the site of most subaerial volcanism and many major earthquakes, and they yield a large fraction of the earth's precious metals. They are obvious targets for study--almost anything you learn is likely to impact important problems--yet arriving at a general understanding is notoriously difficult: Each subduction zone is distinct, differing in some important aspect from other subduction zones; fundamental aspects of their mechanics and igneous processes differ from those in other, relatively well-understood parts of the earth; and there are few direct samples of some of their most important metamorphic and metasomatic processes. As a result, even first-order features of subduction zones have generated conflict and apparent paradox. A central question about convergent margins, for instance--how vigorous magmatism can occur where plates sink and the mantle cools--has a host of mutually inconsistent answers: Early suggestions that magmatism resulted from melting subducted crust have been emphatically disproved and recently just as emphatically revived; the idea that melting is fluxed by fluid released from subducted crust is widely held but cannot explain the temperatures and volatile contents of many arc magmas; generations of kinematic and dynamic models have told us the mantle sinks at convergent margins, yet strong evidence suggests that melting there is often driven by upwelling. In contrast, our understanding ofwhy volcanoes appear at ocean ridges and "hotspots"--although still presenting their own chestnuts--are fundamentally solved problems.

Continental Scientific Drilling Project of the Cretaceous Songliao Basin (SK-1) in China is the first reference to provide the results of the first part of scientific drilling project at the Songliao Basin in the Daqing oil field, the largest known oil field in China. The project has two major objectives: one is to correlate the oceanic and continental records and determine the principal drivers of climate change in order to assist in future climate change predictions and its influence on the earth's environment. The second is to further test the theory of terrestrial genesis of hydrocarbons, and to explore the formation of intra-continental sedimentary basins, as many are major hydrocarbon provinces. In addition, this project provides the scientific basis for exploration of the Daqing Oilfields, which have a yearly production of forty million tons of oil. The world is entering a new exciting era to explore in which scientific drilling will provide a quantum leap in our understanding of its deep earth and history. Continental Scientific Drilling Project of the Cretaceous Songliao Basin (SK-1) in China will play an important role in promoting scientific drilling and earth system science research.

For all introductory physical geology courses. Bringing Earth to life Earth: An Introduction to Physical Geology, 13th Edition, is a leading text in the field, characterized by no-nonsense, student-friendly writing, excellent illustrations, and a modular learning path driven by learning objectives. The new editionis the first to integrate 3D technology that brings geology to life. This edition features significant content updates, a new Geology in the News feature to promote student engagement, and a new Data Analysis feature to help develop students' critical thinking skills. Also available as a Pearson eText or packaged with Mastering Geology Pearson eText is a simple-to-use, mobile-optimized, personalized reading experience available within Mastering Geology. It lets students highlight, take notes, and review key vocabulary all in one place - even when offline. Seamlessly integrated videos and other rich media engage students and give them access to the help they need, when they need it. Educators can easily share their own notes with students so they see the connection between their eText and what they learn in class. Mastering (TM) is the teaching and learning platform that empowers you to reach every student. By combining trusted author content with digital tools developed to engage students and emulate the office-hour experience, Mastering personalizes learning and improves results for each student. Built for, and directly tied to the text, Mastering Geology enables students to get hands on with tools and activities to practice, learn, and apply geology outside of the classroom. Note: You are purchasing a standalone product; Mastering Geology does not come packaged with this content. Students, ask your instructor for the correct package ISBN and Course ID. Instructors, contact your Pearson representative for more information. If your instructor has assigned Pearson eText as your main course material, search for: * 0135586097 / 9780135586099 Pearson eText Earth: An Introduction to Physical Geology -- Access Card, 13/e OR * 0135729629 / 9780135729625 Pearson eText Earth: An Introduction to Physical Geology, 13/e -- Instant Access If you would like to purchase both the physical text and Mastering Geology search for: 0135191122 / 9780135191125 Earth: An Introduction to Physical Geology Plus Mastering Geology with Pearson eText -- Access Card Package Package consists of: 0135188318 / 9780135188316 Earth: An Introduction to Physical Geology 0135188660 / 9780135188668 Mastering Geology with Pearson eText -- ValuePack Access Card -- for Earth: An Introduction to Physical Geology

This is the story of the Peak landscape from its tropical beginnings to its rugged gritty present. Limestone reefs grow in the shallows of tropical seas, taking captive fossilised sea creatures. As the seas shift and coastlines change, sandstones build on the banks of a great river delta. Forests of giant ferns take hold of the land, leaving behind a legacy of coal and bitumen. From the water worn limestone of the White Peak to the wind sculpted sandstones of the Dark Peak, the landscape here is always atmospheric. There are mysterious dry valleys with no sign of running water, caves adorned with sumptuous stalactite chandeliers and the remains of an industrial era built on mineral riches. Paul leads you on a series of fifteen walks which afford spectacular views of the best of the Peak District scenery and reveal evidence of the landscape's intriguing history. In the first half of the book Paul tells the story of the Dark and White Peaks. How limestone reefs grew upon the basement bedrock and the shifting seas deposited layers of sandstone and shale. Tectonic forces buckled and tilted these beds of sedimentary rock to create the rocky edges and tors which characterise the Peak District. The second half of the book details fifteen walks, from easy to challenging, which reveal the geological drama.

This book chronicles how successive generations of natural philosophers, geologists and geomorphologists have come to invent the view of the Earth over the past 250 years.
Chronicles how successive generations of natural philosophers, geologists and geomorphologists have come to invent different views of the Earth over the last 250 years.
Uses as its central viewpoint changing ideas about the significance of the action of rain and rivers on the Earth's surface.
Shows how our contemporary "truths" have come to be accepted and exposes the frailty of even the most impeccably scientific visions of the Earth.

Interpretation of Micromorphological Features of Soils and Regoliths, Second Edition, provides researchers and students with a tool for interpreting features observed in soil thin sections and through submicroscopic studies. After an introduction and general overview, micromorphological aspects of regoliths (e.g., saprolites, transported materials) are highlighted, followed by a systematic and coherent discussion of the micromorphological expression of various pedogenic processes. The book is written by an international team of experts in the field, using a uniform set of concepts and terminology, making it a valuable interdisciplinary reference work. The following topics are treated: freeze-thaw features, redoximorphic features, calcareous and gypsiferous formations, textural features, spodic and oxic horizons, volcanic materials, organic matter, surface horizons, laterites, surface crusts, salt minerals, biogenic and pedogenic siliceous materials, other authigenic silicates, phosphates, sulphidic and sulphuric materials, and features related to faunal activity. The last chapters address anthropogenic features,archaeological materials and palaeosoils.

A multidisciplinary perspective on the dynamic processes occurring in Earth's mantle The convective motion of material in Earth's mantle, powered by heat from the deep interior of our planet, drives plate tectonics at the surface, generating earthquakes and volcanic activity. It shapes our familiar surface landscapes, and also stabilizes the oceans and atmosphere on geologic timescales. Mantle Convection and Surface Expressions brings together perspectives from observational geophysics, numerical modelling, geochemistry, and mineral physics to build a holistic picture of the deep Earth. It explores the dynamic processes occurring in the mantle as well as the associated heat and material cycles. Volume highlights include: Perspectives from different scientific disciplines with an emphasis on exploring synergies Current state of the mantle, its physical properties, compositional structure, and dynamic evolution Transport of heat and material through the mantle as constrained by geophysical observations, geochemical data and geodynamic model predictions Surface expressions of mantle dynamics and its control on planetary evolution and habitability The American Geophysical Union promotes discovery in Earth and space science for the benefit of humanity. Its publications disseminate scientific knowledge and provide resources for researchers, students, and professionals. Find out more about this book from this Q&A with the Author.

Indian Shield: Precambrian Evolution and Phanerozoic Reconstitution highlights unique evolutionary trends covering a period of over 3,500 million years, from the oldest crust to the most recent geological activity of the Indian Subcontinent. The book discusses regional terrain geology in terms of the evolutionary history of the crust, describing how the Precambrian Shield evolved from a stable continental region to a tectonically unstable zone marked by frequent high-intensity earthquakes in a Plate-interior setting. It is a complete and readable account of the history of growth and evolution of the Indian Subcontinent, including Bangladesh, Bhutan, India, Nepal and Pakistan. The book is intended for graduate students, researchers, and teachers in the geosciences, especially geophysics, geomorphology and geology. The book also serves as an important resource for tectonics and petrology researchers, as well as those involved in exploration of mineral resources.