Life, Earth, and Physical Science

Introduction

The theme of this course will focus on helping you use scientific inquiry to discover patterns, trends, structures, and relationships that may be inferred from simple principles. These principles are related to the properties or interactions within and between systems.

The systems can be described and understood by analysis of the interaction of components. Energy, forces, and motion combine to change Earth's physical features. The changes in the physical Earth and the species that lived on Earth are found in the rock record. For species to continue, reproduction must be successful.

 


 

Three branches of science will be discussed in this course:  Life Science, Earth and Space Science, and Physical Science.

Branch of Science

Topic

Focus

Life Science

Species & Reproduction

This topic focuses on the continuation of the species.

Earth & Space Science

Physical Earth

This topic focuses on the physical features of Earth and how they formed. This includes the interior of Earth, the rock record, plate tectonics, and landforms.

Physical Science

Forces & Motion

This topic focuses on forces and motion within, on, and around the Earth and the universe.

 

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Below is a list of the content statements and elaborations that you will be studying in this course. 

 

Life Science

         Content Statement # 1

Diversity of species, a result of variation of traits, occurs through the process of evolution and extinction over many generations. The fossil records provide evidence that changes have occurred in number and types of species.

 

         Content Elaboration

Fossils provide important evidence of how life and environmental conditions have changed.

Changes in environmental conditions can affect how beneficial a trait will be for the survival and reproductive success of an organism or an entire species.

Throughout Earth’s history, extinction of a species has occurred when the environment changes and the individual organisms of that species do not have the traits necessary to survive and reproduce in the changed environment. Most species (approximately 99 percent) that have lived on Earth are now extinct.

 

 

         Content Statement #2

Every organism alive today comes from a long line of ancestors who reproduced successfully every generation.

 

         Content Elaboration

Reproduction is the transfer of genetic information from one generation to the next. It can occur with mixing of genes from two individuals (sexual reproduction). It can occur with the transfer of genes from one individual to the next generation (asexual reproduction). The ability to reproduce defines living things.

 

Animals and plants can reproduce or create new life.

         Content Statement #3

The characteristics of an organism are a result of inherited traits received from parent(s). 

         Content Elaboration

Expression of all traits is determined by genes and environmental factors to varying degrees. Many genes influence more than one trait, and many traits are influenced by more than one gene.

During reproduction, genetic information (DNA) is transmitted between parent and offspring. In asexual reproduction, the lone parent contributes DNA to the offspring. In sexual reproduction, both parents contribute DNA to the offspring.


 

Earth Science

         Content Statement #1

The composition and properties of Earth’s interior are identified by the behavior of seismic waves.

 

         Content Elaboration

The refraction and reflection of seismic waves as they move through one type of material to another is used to differentiate the layers of Earth’s interior. Earth has a core, a mantle, and a crust. Impacts during planetary formation generated heat.

These impacts converted gravitational potential energy to heat. Earth’s core is also able to generate its own thermal energy because of decaying atoms. This continuously releases thermal energy. Thermal energy generated from Earth’s core drives convection currents in the asthenosphere.

 

 

         Content Statement #2

Earth’s lithosphere consists of major and minor tectonic plates that move relative to each other.

 

         Content Elaboration

Historical data and observations such as fossil distribution, paleomagnetism, continental drift and seafloor spreading contributed to the theory of plate tectonics. The rigid tectonic plates move with the molten rock and magma beneath them in the upper mantle.

Convection currents in the asthenosphere cause movements of the lithospheric plates. The energy that forms convection currents comes from deep within the Earth.

There are three main types of plate boundaries: divergent, convergent and transform. Each type of boundary results in specific motion and causes events (such as earthquakes or volcanic activity) or features (such as mountains or trenches) that are indicative of the type of boundary.

 

The diagram above shows several kinds of interactions at plate boundaries, including convergent boundaries where oceanic crust meets oceanic crust, at left, and where oceanic crust meets continental crust, at right. Divergent and transform boundaries associated with seafloor spreading are shown in the center.

 

         Content Statement #3

A combination of constructive and destructive geologic processes formed Earth’s surface.

 

         Content Elaboration

Earth’s surface is formed from a variety of different geologic processes, including but not limited to plate tectonics.

Water, wind, glaciers, and gravity all can change the land through the processes of erosion.

 

         Content Statement #4

Evidence of the dynamic changes of Earth’s surface through time is found in the geologic record.

 

         Content Elaboration

Earth is approximately 4.6 billion years old. Earth history is based on observations of the geologic record and the understanding that processes observed at present day are similar to those that occurred in the past (uniformitarianism). There are different methods to determine relative and absolute age of some rock layers in the geologic record. Within a sequence of undisturbed sedimentary rocks, the oldest rocks are at the bottom (superposition). The geologic record can help identify past environmental and climate conditions .

 

 


 

Physical Science

       Content Statement #1

Objects can experience a force due to an external field such as magnetic, electrostatic, or gravitational fields.

 

         Content Elaboration

Magnetic, electrical, and gravitational forces can act at a distance.

 

tug-of-war: force in action

Each side in a tug-of-war game uses force to try to pull down the other side.

Ryan Child/U.S. Navy

 

         Content Statement #2

Forces can act to change the motion of objects.

 

         Content Elaboration

The motion of an object is always measured with respect to a reference point.

Forces can be added. The net force on an object is the sum of all the forces acting on the object.

If there is a nonzero net force acting on an object, its speed and direction will change.

Kinetic friction and drag are forces that act in a direction opposite the relative motion of objects.

 

motion

The swings on this amusement park ride are in motion.

© Photohunter/Shutterstock.com

 

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