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Transcript
Name _______________________ date ___________ CHAPTER 6 NOTES: EVOLUTION – EVIDENCE OF CHANGE III. Evolution and Plate A. Continental Drift 1. Evolution - Evidence of Change are evidence that changes to the Earth’s _______________ plates are still occurring 2. As lithospheric plates _______________, they create environmental change for the organisms that live on and near them 3. Environmental changes caused by moving plates can lead to the development of and extinction of _______________ B. Geographic Isolation 1. _______________ isolation occurs when populations of species are divided or separated by a physical barrier a. Geographic isolation can occur when lithospheric plate collide and form _______________ b. _______________ and large bodies of _______________ can also cause geographic isolation of species c. Once separated by geographic isolation, species may follow different _______________ paths if they are in different environments over time 2. Darwin’s observations in _______________ and Ecuador led to the idea of evolution by natural selection C. Convergent Evolution 1. When species evolve _______________ under similar conditions and develop structural and functional similarities, the process is known as _______________ a. Convergent evolution results in very distantly related species that appear _______________ b. Geographic isolation leads to closely related species that appear _______________ CHAPTER 7 NOTES: THE AGE OF THE EARTH I. Relative Ages of Rocks A. The Beginning of Modern Geology 1. geologist learn about Earth’s history by studying _______________Scientist _______________ _______________ realized two process were at work on Earth – one that forms rock and one that tears it down a. Hutton developed the principle of _______________, which states that the processes at work _______________ are the same processes that have been at work in the Earth’s past b. Uniformitarianism can be restated as “the _______________ is the key to the past” c. Hutton realized that changes on Earth occur so _______________ that direct observation of them is not possible B. The Rock Cycle 1. The _______________ _______________ is a series of processes that make and change rocs through heating, melting, cooling, uplift, weathering, burial, and increasing pressure 2. Geologist categorize rock into three group based on how the rock _______________ a. The three rock types are _______________, _______________, and _______________ 3. Igneous rock forms when _______________ solidifies a. Different types of igneous rocks are identified by the size of the _______________ from rapid cooling b. _______________ crystals form from slow cooling, whereas small _______________ form from rapid cooling 4. _______________ rock is any rock subjected to extreme pressure or heat a. _______________ can cause minerals to become more tightly packed b. Heat can cause minerals to _______________ and form a new rock mineral 5. Sedimentary rocks form from sediments a. Sediments are tiny particles of eroded _______________ C. Sediment Formation and Layering 1. Sedimentary rocs form in a four-step process: _______________, _______________, _______________, and _______________Weathering is the physical or chemical breakdown of rock into smaller pieces 2. Weathering is the _______________ or _______________ breakdown of rocks into smaller pieces 3. _______________ occurs when sediments are moved downhill by running water, wind, moving ice, and gravity a. Individual sediment grains are called _______________ b. During transportation, clast become _______________ as they wear down and break apart c. As the speed of the sediment carrier _______________, larger-sized clast drop out 4. _______________ occurs when sediment carried by water, wind, and glaciers stop moving a. The sediment from _______________, horizontal layers 5. _______________ occurs when sediments become compacted and cementation changes the sediments into rock D. Superposition and the Fossil Record 1. Layers of rock are called _______________ 2. Danish physician _______________ _______________ presented four principles to help geologist study strata and interpret the rock’s history a. The four principles are _______________, original horizontality, original lateral continuity, and crosscutting relationship 3. The principle of _______________ states that in a stack of undisturbed sedimentary rock layers, the layers on the bottom were deposited before the layers on the top a. The rock layers on the bottom are the _______________ than the layers farther up b. _______________ age tells how old something is compared to something else II. 4. The principle of original horizontality states that the rock layers are original deposited in _______________, or nearly _______________, layers 5. The principle of original lateral continuity states that sedimentary rocks form layers that cover _______________ areas 6. The principle of crosscutting relationships states that a rock layer or feature that cuts across another rock layer is _______________ than the ones being cut (dykes) Absolute Ages of Rocks A. Atoms and Isotopes 1. Atoms are made of _______________, _______________, and _______________ 2. Isotopes of an atom have the same number of _______________, but different number of _______________ a. Isotopes of an element can be _______________ or _______________ B. Dating and Tree Rings 1. _______________is the science of comparing the annual tree ring growth to date events and changes in past environments a. A _______________ is a layer of wood cells produced in one year b. Some of the factors affecting the width of tree rings are _______________, temperature, sunlight, and _______________ c. _______________ is a technique that gives each tree ring an exact-year to date of formation C. Half-Life 1. Ernest Rutherford and Frederick Soddy discovered that parent isotopes decay into daughter isotopes at a _______________ rate 2. A _______________is the amount of time for half of a specific amount of parent isotopes to decay into daughter isotopes a. Geologist can determine the _______________ age of rock by calculating the absolute age of the _______________ that compose it b. The absolute age of a mineral is determined by measuring its _______________to _______________ isotope ratio D. Determining Earth’s Age 1. The decay of radioactive isotopes is used by geologist as a “_______________” 2. _______________ dating is a procedure used to calculate the ages of rocks and minerals a. _______________ rocks are most commonly used for radiometric dating b. Determining the age of _______________ rocks is difficult c. Geologist rarely use radiometric dating for _______________ rocks E. The Absolute Age of Earth 1. The oldest rocks on Earth are part or areas called _______________ shields 2. Earth is at least as old as the zircon discovered in Australia in 2001, which was estimated to be _______________ years old 3. Meteorites collected in _______________ have been calculated to be between 4.48 and 4.56 billion years old 4. Rocks from the _______________ have been calculated to be approximately 4.6 billion years old