Browse All Chapters of This Textbook
Chapter 1 - Earth As A SystemChapter 2 - Rock-forming Minerals And RocksChapter 3 - The Diversity Of LifeChapter 4 - Environments And LifeChapter 5 - Sedimentary EnvironmentsChapter 6 - Correlation And Dating Of The Rock RecordChapter 7 - Evolution And The Fossil RecordChapter 8 - The Theory Of Plate TectonicsChapter 9 - Continental Tectonics And Mountain ChainsChapter 10 - Major Geochemical Cycles
Chapter 11 - The Hadean And Archean Eons Of Precambrian TimeChapter 12 - The Proterozoic Eon Of Precambrian TimeChapter 13 - The Early Paleozoic WorldChapter 14 - The Middle Paleozoic WorldChapter 15 - The Late Paleozoic WorldChapter 16 - The Early Mesozoic EraChapter 17 - The Cretaceous WorldChapter 18 - The Paleogene WorldChapter 19 - The Late Cenozoic World Before The HoloceneChapter 20 - The Retreat Of Glaciers And The Holocene
Earth System History remains the only text for the historical geology module written from a truly integrated earth systems perspective, combining the physical and biological history of Earth.
Sample Solutions for this Textbook
We offer sample solutions for Earth System History homework problems. See examples below:
Actualism is the term used by geologists. It is a main principle of science, and it applies on all...An atom consists of protons, neutrons, and electrons. Protons have a positive (+) charge and...Fossils are the remains of ancient organisms that are preserved for thousands or millions of years....Pictorial representation: Fig.1 represents a food web. Fig.2 represents food chain. Fig.1: Food web...Evaporites and sand dunes reflect the arid environment. These are explained as follows: (i) Sand...Stratigraphic correlation is a method used by geologists to gather the information about the widely...The process of natural selection is the key to the evolution of a certain type of species into the...The evidence which supports the idea that continents have moved over Earth’s surface are as follows:...The geologic features that enable the geologists to recognize ancient continental rifting are as...
Negative feedback: When the output of a system or mechanism tend to decrease the input of the...The Precambrian shield is the nuclear area (that is exposed at Earth’s surface) of Precambrian...The Wopmay system can be defined as the deformation of the body of rocks or mountain that has been...The life forms that colonized early Paleozoic seafloors lived close to the surface of the sediment....The marine taxa during Ordovician Period rediversified and became the members of the Silurian and...The alternative transgression and regression of shallow seas are described as cyclothems. Most...The Paleozoic Era completed after the great mass extinction at the end of the Permian Period about...Coccolithophores were a single-celled organism that had tiny shield-like plates. These plates armour...Paleogene life was very similar to modern life. There was no special alteration in the Paleogenic...Many Neogene mammal groups became modernized because of the spread of grassy woodlands. Several...About 22,000 years ago, the continental glacier started to melt. The water from the continental...
More Editions of This Book
Corresponding editions of this textbook are also available below:
Earth System History 4e & Launchpad Solo For Earth System History (six Months Access)
Earth System History
Loose-leaf Version for Earth System History
Earth System History
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