Students will be able to:
use information from internet access, textbooks, and classroom discussions to
-describe how fossils are formed.
-compare and contrast relative and absolute age.
-describe geologic time scale.
Students took the last pre-test on benchmarks SC.F.1.3.1, SC.F.2.3.2, SC.F.2.3.3, SC.G.1.3.4, and SC.G.2.3.4.
Students then finished any notes on fossils. You can find the notes at the bottom of this blog.
Students learned site recognition of words from the strands Processes of Living Things and How Living Things Interact With Their Environment by playing a word search game. The link can be found under today's date on Dr. Gayden's Science Zone (drgcdms.podomatic.com) or you can cut and paste the following link directly.
http://www.wordduck.com/wordsearch.php?user_id=1700
There was no additional home learning. Students are to continue to work on their rock collection.
>>>>>>>>>>FOSSIL NOTES<<<<<<<<<<<
Fossils
Fossils are the remains, or traces, of organisms that lived long ago.
Fossil Formation in Rocks – organism buried by sediment soon after it dies, soft parts of organism decay, leaving the hard parts like shells and bones.
Molds form when an organism is buried by sediments, and the sediments change into rock. Once the organisms decays, an opening (mold) is left in the rock.
Casts form when the cavity created by the mold fills with sand or mud and hardens.
Imprints form when living things or their marks (footprint) are made in soft mud, which hardens to form the imprint.
Entire organisms can be found as fossils. Entire mammoths have been trapped in ice. Animals on their way to drink, slipped into tar pits
Small insects can be trapped in tree amber.
Scientists study fossils to determine how many living things have become extinct, how living things change over the earth, and how the earth’s climate and surface have changed over millions of years.
Relative Age of Rocks
When rock layers form, the older layers form first, and are located at the bottom. The younger layers form on top of these. This is the law of superposition.
Relative age-age of an object compared to the age of another object.
Index fossils are also used to determine the age of rocks. An index fossil is an organism that lived only during a short part of the earth’s history, was found in many places on earth and must be unique.
Absolute Age of Rocks
Absolute age-specific age or a rock or fossil.
Radioactive elements may be found in rocks and organisms. These elements give off particles and energy. As they give off energy, new, nonradioactive elements form. The rate of this radioactive decay is steady and regular and can be measured.
Half-life is the length of time it takes for one-half of the amount of a radioactive element to change into another element.
Some radioactive isotopes, like Carbon-14, can only be used to find the absolute age of the remains of once living things.
Geologic Time Scale
The earth is more than 4.6 billion years old. The earth’s past is divided into sections. The geologic time scale outlines the major events in the earth’s history and the kinds of organisms that lived on the earth in the past. It is divided into eras, period, and epochs.