M6D1: Rejection of Continental Drift TheoryHow did society view Alfred Wegener’s continental drift theory? Explain the differences between these points-of-view.Your initial post should be at least 250 words and must substantively integrate the assigned readings from the module with proper APA (Links to an external site.) style formatting// You may use additional sources and materials as long as they are relevant to the discussion and cited properly.M6D2: Internal vs. External ProcessesDistinguish between internal and external processes that shape the Earth’s surface. For example, how are intrusive igneous rock formations different from extrusive ones and what role have those differences played in how the surface of the Earth developed and the civilization developed on top of that?Your initial post should be at least 250 words and must substantively integrate the assigned readings from the module with proper APA (Links to an external site.) style formatting// You may use additional sources and materials as long as they are relevant to the discussion and cited properly.M6D3: Porosity vs. PermeabilityDiscuss the difference between porosity and permeability of earth materials and how they affect their development and use of underground water supplies.Your initial post should be at least 250 words and must substantively integrate the assigned readings from the module with proper APA (Links to an external site.) style formatting// You may use additional sources and materials as long as they are relevant to the discussion and cited properly.
M6D1: Rejection of Continental Drift Theory How did society view Alfred Wegener’s continental drift theory? Explain the differences between these points-of-view. Your initial post should be at least 2
Module 6: Module Notes: Earth’s Lithosphere We begin this module by studying the characteristics, development and distribution of soils around the world. It begins by describing soil-forming factors, soil components, soil properties, soil chemistry and soil profiles. The section on pedogenic regimes relates the formation and characteristics of soil to differences in the environment, especially differences in climate. The part of the module concludes with a description of soil classification and the distribution pattern of major soil types around the world. As you begin your study of soils, focus on how the various processes of soil formation influence the characteristics of soil. The pattern of soil distribution is complex, but by noting the close relationship between climate and many soil types, this pattern is more comprehensible. The next section of the module provides a general introduction to this topic by discussing the overall structure of the Earth, the basic types of rocks, the key concepts of geological time and Uniformitarianism and the various scales of landform analysis. Several sections of the latter part of this module deserve special attention. The general introduction to the structure of the Earth is important because terms and concepts first presented here will be utilized when we discuss plate tectonics in. Similarly, references to various types of rocks are also found in subsequent chapters. One of the most important concepts to consider here is “Geological Time. ” Unless we can expand our perspective of time to include periods of millions of years, the processes described in the remainder of the modules will have little meaning. This Module includes a wide range of important concepts in geomorphology. It covers the theory of plate tectonics and the broadest-scale movements of the surface of the Earth. The second major section focuses on volcanism, including both the consequences of volcanic activity, as well as the movement of magma beneath the surface. The final section looks at diastrophism, the deformation of the Earth’s crust through folding and faulting. After studying the section on plate tectonics, you should be familiar with the kinds of major topographic features and tectonic activity associated with the three different types of plate boundaries, as well as the modifications to the basic plate tectonic model, such as terranes and mantle plumes. Also, pay attention to the historical development of this theory and the lines of evidence that have helped verify it. The sections on volcanism and diastrophism focus mainly on the development of landforms. However, note the general relationship of these different kinds of processes to plate tectonics and plate boundaries. Demonstration Playlist: Chapter 14: Volcano Types Chapter 14: Understanding Tuttle and Bowen’s Data Chapter 14: Motion at Transform Boundaries Chapter 14: Terrane Formation Chapter 14: Tectonic Settings and Volcanic Activity Chapter 14: Seismic Wave Motion Chapter 14: Earthquake Waves Chapter 14: Motion at Plate Boundaries Chapter 14: Plate Motions Through Time Chapter 14: Debris Avalanche and Eruption of Mount St. Helens, Washington Chapter 14: Hot Spot Volcano Tracks Chapter 14: Folding Chapter 14: Fault Motion Chapter 14: Forming a Divergent Boundary Chapter 14: Formation of Crater Lake Chapter 14: Convergent Margins: India-Asia Collision Chapter 14: How Calderas Form Chapter 15: Physical Weathering Chapter 15: Mass Movements
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