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Earth as a system The Earth system is powered by energy from the sun that drives the external processes in the Atmosphere Hydrosphere Biosphere Geosphere.

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Presentation on theme: "Earth as a system The Earth system is powered by energy from the sun that drives the external processes in the Atmosphere Hydrosphere Biosphere Geosphere."— Presentation transcript:

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2 Earth as a system The Earth system is powered by energy from the sun that drives the external processes in the Atmosphere Hydrosphere Biosphere Geosphere (lithosphere) Earth system is also powered by internal processes driven by heat flow within earth. What are some sources of heat?

3 Figure 1.4 Was this rock formation the result of internal or external processes? What had to occur for this arch to form?

4 Can you think of one or more internal processes that are of interest to geologists?
Can these processes be explained?

5

6 Two views of Pakistan Charakusa Valley, Karakorum Range

7 Muzzaffarabad

8 Natural Hazards One important reason to study geology and be able to predict processes is to prevent threats to humans A natural hazard is just that – natural process. It only becomes a hazard when humans put themselves in harm’s way.

9 The Science of Geology Geology - the science that pursues an understanding of planet Earth GEO=earth OLOGY = study of Physical geology - examines the materials composing Earth and seeks to understand the many processes that operate beneath and upon its surface Historical geology - seeks an understanding of the origin of Earth and its development through time

10 The Science of Geology Some historical notes about geology
The nature of Earth has been a focus of study for centuries Catastrophism Uniformitarianism and the birth of modern geology James Hutton: Theory of the Earth Late 1700s – birth of modern Geology

11 The nature of scientific inquiry
Science assumes the natural world is consistent and predictable Goal of science is to discover patterns in nature and use the knowledge to make predictions Scientists collect data through observation and measurements

12 The nature of scientific inquiry
How or why things happen is explained using a Hypothesis – a tentative (or untested) explanation Theory – a well-tested and widely accepted view that the scientific community agrees best explains certain observable facts

13 Box 1. 2 Do glaciers move. (pg
Box 1.2 Do glaciers move? (pg. 11) Rhone Glacier, Switzerland, credit: L. Agassiz

14 The nature of scientific inquiry
Scientific method involves Gathering facts through observations Formulation of hypotheses and theories There is no fixed path that scientists follow that leads to scientific knowledge

15 Solar Nebular Hypothesis
Is this hypothesis created by direct or indirect observation? How do you think this model was made?

16 Early evolution of Earth
Origin of planet Earth Nebular hypothesis Assumes a flat, disk shape with the protosun (pre-Sun) at the center Inner planets begin to form from metallic and rocky substances Larger outer planets began forming from fragments of ices (H2O, CO2, and others)

17 Early evolution of Earth
Origin of planet Earth Most researchers believe that Earth and the other planets formed at essentially the same time Nebular hypothesis Rotating cloud called the solar nebula Composed of hydrogen and helium Nebula began to contract about 5 billion years ago

18 Figure 1.9A How did the moon form? Do scientists agree?

19 Speaking of models…how did this diagram become a model of earth?

20 Early evolution of Earth
Formation of Earth’s layered structure Metals sank to the center Molten rock rose to produce a primitive crust Chemical segregation established the three basic divisions of Earth’s interior Primitive atmosphere evolved from gases in Earth’s interior

21 Earth’s internal structure
Layers defined by composition Crust Mantle Core Layers defined by physical properties Lithosphere Asthenosphere Mesosphere Inner and Outer Core

22 Earth’s Layered structure
Figure 1.16

23 Figure 2.29

24 Figure 1.5

25 Concept of Geologic Time
The second frame of reference for geologic time is absolute dating Absolute dating results in specific dates for rock units or events expressed in years before the present Radiometric dating is the most common method of obtaining absolute ages Such dates are calculated from the natural rates of decay of various natural radioactive elements present in trace amounts in some rocks


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