GEOL 100. Planet Earth (3) I, II
Earth’s global systems. Plate tectonics, earthquakes, and volcanoes; evolution of our planet and life through geologic time; economic resources including fossil fuels and precious minerals; agents of erosion that shape the land.
Quartz: SiO2
Quartz: SiO2
The constantly evolving earth has been shaped by a variety of mechanisms and processes. An understanding of these, through the study of geology, gives us an appreciation of our dynamic planet and a more knowledgeable perspective of our fragile environment. The purpose of this course is to study global processes of planet earth and specific mechanisms that form its surface, such as the growth of minerals, the formation of rocks, mountain building, earthquakes, volcanoes, erosion, and coastal processes. Geologists utilize physics, chemistry, biology, mathematics, and computer science to develop a holistic understanding of our planet.
Goals and Objectives
This course has several overarching and content goals. Overarching goals are outline below and meet several of the Goals and Objectives for GE Courses in the Sciences as outlined in the 2003 SDSU Curriculum Guide
I. Overarching Goals/Outcomes
After completion of this course students will be able to:
1. Articulate the multidisciplinary integrated nature of the Earth Sciences and the importance of its role in their and others everyday lives (Goal 1 – Objectives 2 and 3)
2. Articulate how technological advances along with the collection of a myriad of observational and analytical data over the last 200 years have lead naturally to the interpretation that the Earth originated about 4.6 billion years ago, and that its development has been punctuated by several major planet-wide events that brought about profound change in Earth’s habitants (Goal 2 – Objective 1)
3. Articulate how laboratory experimentation has lead to an enhanced understanding of dynamic earth processes such as faults and earthquakes, and, as a result, how the Earth Sciences have impacted their and others quality of life (Goal 2 – Objective 2; Goal 3 – Objective 3).
4. Articulate how the scientific method is used to infer the causes of global-scale changes that have affected planet Earth over time (Goal 2 – Objectives 2, 3).
5. Articulate examples of everyday observations that indicate that the Earth is dynamic and ever changing, and how these observations impact their daily life (Goal 4 – Objectives 1, 3, 4).
The above overarching goals are intertwined with the following specific content goals.
II. Content Goals/Outcomes
To meet content goals students will be able to:
1. Articulate the role that lithospheric plates and their movements play in shaping the Earth’s landmasses and ocean basins, and the internal compositional and mechanical attributes of planet Earth
2. Identify from their physical and chemical characteristics the common minerals in the non-silicate and silicate mineral groups
3. Distinguish the three major rock groups based on their physical characteristics and modes of formation
4. Articulate the distribution of the 12 major soil orders within the various states, and convey the major climatic or parental controls on this distribution
5. Convey the vastness of geologic time, key biological and physical events that have affected Earth through time, the terminology used to distinguish time from the rocks and sediments deposited during a specific time interval, and the role of the fundamental age equation in establishing the temporal framework for the geologic time scale
6. Identify the different types of faults and demonstrate an understanding of their origin, distribution, and relationship to earthquakes.
7. Identify the different types of folds from their geometrical and stratigraphic character, and the various map symbols used to locate and characterize them on geologic maps.
8. Identify the various landforms displayed on topographic maps, articulate locations in township and range format, and convey the differences between magnetic and geographic north.
9. Articulate the role of the Earth, Moon, and Sun in producing tides, the role of wind in producing waves, and the physical characteristics of deep and shallow water waves.
10. Convey that the Earth’s climate has been different in the past as exemplified by the Great Ice Age, and that the Earth’s climate is influenced by a variety of mechanisms including the precession and obliquity of the Earth’s axis of rotation and the eccentricity of its orbit around the sun along with large volcanic eruptions and bolide impacts
ATTENTION: The online content of these courses may be neither current nor final. Be sure to check with the instructor for the latest information regarding lecture schedules, exams, etc.