Chapter 1 - Introduction (Week 1) Flashcards

1
Q

What is geology, and what aspects do geologists study?

A

Geology is the scientific study of Earth, encompassing the study of its interior and exterior surface, rocks, other materials, and the processes that formed them. Geologists investigate changes over Earth’s vast timespan and consider changes that might occur in the near future.

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1
Q

What characterizes geology as a science, and why is it considered one of the most interdisciplinary sciences?

A

Geology is a science characterized by deductive reasoning and scientific methodology. It is considered one of the most interdisciplinary sciences because geologists must understand and apply other sciences, including physics, chemistry, biology, mathematics, astronomy, and more in their investigations.

Geology is about understanding the evolution of Earth through time. It is about discovering resources such as metals and energy, and minimizing the environmental implications of our use of resources

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2
Q

What distinguishes the role of time in geology compared to other sciences, and how does deep time influence geological processes?

A

In geology, time plays a unique role, specifically, deep time — spanning billions of years. Geologists study events that occurred thousands, millions, and even billions of years in the past. Many geological processes occur at incredibly slow rates, ranging from millimeters to centimeters per year. However, due to the vast amount of time available, these slow changes can lead to significant transformations, such as the formation of expansive oceans or the wearing away of entire mountain ranges.

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3
Q

Geology on a Grand Scale in the Canadian Rocky Mountains

A

Many geological features are shown here. The rocks that these mountains are made of formed in ocean water over 500 million years ago. A few hundred million years later, the rocks were pushed east for tens to hundreds of kilometres, and thousands of meters upward in a great collision between Earth’s tectonic plates.

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4
Q

Why is studying Earth important, and what are some key reasons for studying Earth?

A

Studying Earth is crucial because it is our only home for the foreseeable future, and understanding how it works is essential to ensure it remains a great place to live. Some key reasons for studying Earth include:

-Understanding the evolution of our environment and life through the study of rocks and fossils.
-Minimizing risks from natural hazards such as earthquakes, volcanoes, slope failures, and storms.
-Exploring the reasons behind past climate changes and comprehending both natural and human-caused climate change.
-Utilizing Earth’s resources sustainably, including soil, water, metals, industrial minerals, and energy.
-Recognizing and addressing the impact of human activities on the environment.
-Gaining insights into other planets in our solar system and those around distant stars through knowledge of Earth.

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5
Q

What do geologists do, and what are some of the diverse tasks and fields where geologists work?

A

Geologists engage in various tasks and work in diverse fields, including:

-Resource industry: In mineral exploration, mining, and the exploration and extraction of energy sources.
-Hazard assessment and mitigation: Assessing risks from slope failures, earthquakes, and volcanic eruptions.
-Subsurface study: Investigating the nature of the subsurface for construction projects like highways, tunnels, and bridges.
-Water supply planning: Using subsurface information for planning, development, and management of water supply.
-Contaminant containment: Deciding how best to contain contaminants from waste.
-Research: Conducting research to enable practical applications of geology, from field mapping to laboratory analysis of rocks.
-Specializations: Some geologists specialize in inventing ways to use complex instruments for measurements.
-Paleontology: Studying fossils to understand ancient animals and environments.
-Astrogeology: Helping NASA understand data from objects in space.
-Geological work can be conducted both indoors, in offices and labs, and outdoors. Many geological opportunities involve fieldwork in fascinating and remote locations.

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6
Q

How do scientists study Earth, and what are the key features of serious inquiry in scientific research?

A

Scientists study Earth using the scientific method, which involves key features of serious inquiry:

Creation of a hypothesis: Forming a tentative idea to explain a set of observations.
Testing the hypothesis: Using the hypothesis to make predictions and conducting experiments to verify if those predictions are correct.

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7
Q

Can you provide an example of the scientific method in action, and what considerations should be taken when formulating and testing a hypothesis?

A

Consider a field trip to a stream where rocks are rounded. A hypothesis is formed that the rocks were rounded as they collided during stream transport. Predictions are made: rocks downstream should be rounder and smaller, while upstream rocks should be more angular and larger. Testing involves marking rocks and checking if they change as predicted. The hypothesis must be open to alternative explanations, and if proven wrong, a new hypothesis must be developed. A good hypothesis is testable, unlike impractical ones, such as an extraterrestrial organization creating rocks invisibly.

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8
Q

What are theories and laws in the context of the scientific method, and how do they differ?

A

In the scientific method, a theory evolves from a hypothesis and stands the test of time and numerous tests. It is not a wild and unproven guess, but a well-supported explanation.

On the other hand, a law is a description of a phenomenon, not an explanation. It is a formula or pattern observed through repeated tests but does not provide the “why” behind the phenomenon.

In geology, there are fundamental ideas that shape our understanding of Earth’s workings, akin to the soundtrack of a movie, influencing our perception.

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9
Q

Three Big Ideas

A

Geological Time, Uniformitarianism, and Plate Tectonics

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10
Q

Geological Time (Deep Time):

A

Earth is approximately 4.57 billion years old.

Geological events unfold over immense periods.

Tiny changes, like chemical reactions over a year, accumulate to have significant impacts over millions of years.

For geologists studying slow processes, even 1 million years might be considered trivial.

“Ancient” takes on a new meaning in the context of deep geological time.

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11
Q

How is geological time expressed in numbers, and what are the common abbreviations used for different time scales?

A

Expressing Geological Time:
Special notation is used to avoid writing numerous zeroes.

Common Abbreviations:
-Ga: Giga annum or billions of years (e.g., Earth is 4.57 Ga old).
-Ma: Mega annum or millions of years (e.g., Earth is 4,570 Ma old).
-ka: Kilo annum or thousands of years (e.g., the last glacial cycle ended 11,700 years ago, or 11.7 ka).

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12
Q

How is geological time expressed using the Geological Time Scale, and why is it based on events rather than specific years?

A

Geological Time Scale:
-A way of breaking down geological time based on significant events in Earth’s history.
-Divided into eons, eras, periods, and epochs.
-Intervals are named rather than using specific years.

Reasoning:
-Naming intervals makes sense as we may not always know the absolute age of rocks or fossils in years.
-Relative age is determined by comparing the rock or fossil’s age to others, placing it in context based on the geological record.

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13
Q

How can geological time be conceptualized using the analogy of a calendar year, and what is the significance of uniformitarianism?

A

Geological Time Analogous to a Calendar Year:
-Origin of the solar system and Earth at 4.57 Ga represents January 1.
-Present year represents the last tiny fraction of a second on New Year’s Eve.
-Each day of the year represents 12.5 million years, each hour about 500,000 years, each minute 8,694 years, and each second 145 years.
-Significant events in Earth’s history expressed on this time scale.

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14
Q

Uniformitarianism in Geology

A

Uniformitarianism:
-Geological processes today are the same as those in the past.
-“The present is the key to the past,” a concept presented by James Hutton and paraphrased by Charles Lyell.
-Observations of current geological processes help interpret and understand the rock record.
-Initially groundbreaking and controversial, challenging perceptions of the Earth’s age and religious beliefs.

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15
Q

Uniformitarianism in Geology cont.

A

Definition:
Uniformitarianism posits that the geological processes occurring on Earth today are similar to those that operated in the past.

Significance:
-Interpreting the Rock Record: Observations of present-day geological phenomena are applied to interpret and understand the geological history preserved in rocks.
-Controversy: In its early days, uniformitarianism challenged prevailing beliefs. Many, accustomed to thinking in thousands of years, found it revolutionary, as it required considering vast geological timescales.
-Religious Implications: The concept raised questions about traditional religious beliefs regarding the Earth’s age.

Historical Context:
-James Hutton: Scottish geologist James Hutton introduced the concept of uniformitarianism in 1785.
-Charles Lyell: In his book Principles of Geology, Scottish geologist Charles Lyell expressed this idea as “the present is the key to the past,” a phrase commonly used today.

Clarifications:
-Oversimplification: While “the present is the key to the past” is a helpful concept, not all present-day geological processes occurred throughout Earth’s history.
-Chemical Reactions: Some contemporary chemical reactions are dependent on factors, such as atmospheric oxygen, which varied in the geological past.

Considerations:
-Changing Conditions: Conditions on Earth varied throughout its history, acknowledging differences in factors like atmospheric composition and continental development.
-Interpreting the Rock Record: Despite variations, present environments resembling past conditions offer insights into Earth’s geological history.

16
Q

Plate Tectonics

A

The theory that Earth’s surface is divided into large moving fragments known as plates, which play a crucial role in shaping the planet’s geological features.

17
Q

Understanding Earth’s Dynamics

A

Plate tectonics revolutionized our understanding of geological processes, allowing us to explain the formation of features such as mountain ranges and the occurrence of earthquakes.

18
Q

Plate Motion

A

Earth’s 15 largest tectonic plates are depicted in Figure 1.8, showing their directions of motion with arrows. Longer arrows indicate faster plate motion.

19
Q

Historical Perspective:

A

Before Plate Tectonics: Observations were made, but mechanisms were speculative, akin to guessing the inner workings of a clock by watching its hands.

After Plate Tectonics: Comparable to opening the clock and understanding the gears, as plate tectonics provides a mechanistic explanation.

20
Q

Mechanism: Plate Mobility

A

Explanation: Earth’s outer layer consists of rigid plates that constantly interact by moving around the planet. This mobility is facilitated by the plates floating on a weak rock layer, allowing deformation similar to the sliding of layers in a sandwich.

21
Q

Plate Boundaries:

A

Divergent Boundaries: Plates move away from each other.

Convergent Boundaries: Plates collide.

Transform Boundaries: Plates slide past each other.

22
Q

Geological Consequences:

A

Mountain Belts and Volcanoes: Influenced by plate convergence.

Earthquakes: Occur at plate boundaries due to their interactions.

Oceans and Continents: Shapes and sizes are determined by various plate movements.

23
Q

Future Predictions

A

Role of Plate Tectonics: Not only explains past geological events but also enables predictions about future occurrences based on the ongoing interactions of tectonic plates.