Chapter 1 – Introduction: How Do We Study Earth’s Systems?
1.1 Why Study the History of Earth?
 Geology is the science that studies the history of Earth and its life
o Understanding how Earth changes tells us how natural processes affect humans
and how humans affect natural processes
o Many natural processes act very slowly
o Earth’s environments change over the time span of many human generations
 Humans have begun to affect Earth’s environment at rates faster than rates of natural
processes
o Burning of fossil fuels releases greenhouse gases such as carbon dioxide into the
atmosphere
o Greenhouse gases trap heat and keep Earth’s temperature warm
o Carbon dioxide levels in the atmosphere have increased 30% since the start of
the Industrial Revolution generations
 Anthropogenic (human generated) activities such as fossil fuel combustion impacting
Earth has led to the study of Earth as a series of systems
o A system is a series of components that interact to produce a larger, more
complex whole
o Rocks and fossils are studied by geologists because they preserve the
interactions of the Earth systems
1.2 What Are the Major Earth Systems and What Are Their Characteristics?
 Earth’s environments are regulated by four major systems and their components
o The solid Earth system consists of the nonliving solid Earth from its center to its
surface, including continents and seafloor
o The atmosphere comprises the gaseous envelope surrounding Earth
o The hydrosphere consists of oceans, rivers and streams, lakes and ice in glaciers
and ice caps (the latter is sometimes termed the cryosphere)
o The biosphere consists of all living organisms and their dead remains
 Some compartments (smaller parts of a system) may serve as reservoirs in which certain
types of matter may be stored for some length of time
 Most natural systems are open systems, meaning that they exchange matter and energy
with the surrounding environment
o This is termed a flux; an example is the operation of Earth’s convection cells,
both in Earth’s interior and in the atmosphere
 Earth’s systems interact through feedback
o Positive feedback promotes an effect whereas negative feedback counters an
effect
o Feedbacks may involve the biogeochemical cycles of elements such as carbon
 The relative importance of processes within the Earth systems varies with the duration
of time
1.3 Geologic Time and Process
 Many processes relevant to change in Earth’s systems are imperceptible on human time
scales
 Early geologists recognized the enormity of geologic time
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
Analysis of layered rock sequences led to the Principle of Superposition and other
relative age techniques
o James Hutton interpreted the action of processes much slower than those
observed on human time scales
 The Principle of Faunal Succession is based on fossils as evidence for ancient life
o It states that different groups of fossils follow each other in a characteristic
sequence
 More recently (during the 20th century), absolute ages were determined from the rates
of radioactive decay of certain minerals
o The modern geologic time scale incorporates both changes in fossil assemblages
and absolute ages
 The Principle of Uniformitarianism states that processes we observe today have always
operated; it underlies all scientific inquiry
o Traced to James Hutton but also expressed in writings of earlier scientists
o Hutton recognized that natural processes are cyclic and that Earth has an
internal source of heat
o Charles Lyell developed uniformitariansm to counter castrophism, the view that
Earth resulted through processes not observable today
o The uniformitarian approach is termed actualism, and considers processes in
modern environments as analogs of those in ancient environments
o Uniformitarianism is often stated as “the present is the key to the past” but the
past is not the key to the present; conditions then may have been quite different
from present-day conditions
o The current understanding of uniformitarianism is that although processes
remain the same, the rates can vary (and the duration of time involved can be
important); also, that highly unusual conditions and phenomena such as meteor
impacts and mass extinctions occur
1.4 Directionality and the Evolution of Earth Systems
 Lyell envisioned Earth as being in equilibrium, meaning a system exhibiting no net
change through time
 Evidence exists, however, that Earth has also evolved, meaning that its seemingly
equilibrium states have actually shifted through time in particular directions; this is
termed secular change
 Earth’s history has consisted of a succession of vastly different worlds leading up to
ours
1.5 Geology as an Historical Science
 The view of nature and its components as machines dates to Rene Descartes (16th
century)
o This led to reductionism, the view that nature can be understood by taking it
apart, such as breaking the Earth system into components
 Science is also based on the assumption that each effect has a particular cause
o This view is called determinism
o The notion that the simplest explanation of a phenomenon is most likely to be
correct is called Ockham’s Razor
o Earth’s phenomena are not strictly deterministic because the same effect may
have multiple or overlapping causes; this is termed multiple causation
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o The processes that occurred during the ancient past have varied with historical
circumstances, or contingency
1.6 The Scientific Method and the Study of Earth’s Evolving Systems
 According to most scientists, proof is based on formulating and testing hypotheses to
see whether or not predictions hold
o This method is iterative and self-correcting
o Karl Popper, a philosopher who developed the modern scientific method, stated
that the best hypotheses are the ones that can be easily falsified
o Scientists use procedures of reasoning called induction (in which the conclusion
does not necessarily follow from the premises) and deduction (in which the
conclusion follows from the premises) to formulate and test hypotheses
 This approach to science is best exemplified in experimental sciences such as physics
and chemistry
o Geologists typically test hypotheses by looking for rocks, sediments or fossils
and make observations on them on the variables of interest
o They then use postdiction (rather than prediction) to reason backward from the
geologic data to infer the processes involved
 Scientists follow the method of multiple working hypotheses in which multiple factors
acting on different scales may interact to product a final effect
 As a hypothesis is tested and confirmed over time it may be elevated to the status of a
theory
 Relationships between phenomena considered to be fundamental truths are called laws
o Laws are abstractions; they describe relationships that are repeatable irrespective
of contingencies
o In geology, general truths are referred to a principles rather than laws
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