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Define these terms

Define these terms. Define: The law of original horizontality Index fossil Stratigraphy Petrifaction Altered remains Unconformity Angular unconformity Superposition Name the five stages in sedimentary rock formation Explain why fossils are found primarily in sedimentary?

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Define these terms

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  1. Define these terms Define: The law of original horizontality Index fossil Stratigraphy Petrifaction Altered remains Unconformity Angular unconformity Superposition Name the five stages in sedimentary rock formation Explain why fossils are found primarily in sedimentary? What is the cambrian explosion? What is the fundamental idea behind fossil succession?

  2. AMUatomic mass unit Protons and neutrons are treated as being equal in mass. This mass is 1 amu. In fact there is a slight difference. be considered to have the same mass. The mass of an electron is 5/10,000ths of an amu. The charge of a proton is +; the charge of an electron is negative. These charges are equal, but opposite. Atoms have three main components. Each of these has mass. Two of them have charge.

  3. AMU and isotopes Because the mass of an electron is so small compared to the mass of the proton and neutron (5/10,000ths), it is not used to determine atomic mass. The atomic mass of an atom is calculated by adding the mass of the protons and the mass of the neutrons found in the nucleus. The proton and neutron are located in the nucleus. The nucleus is approximately 1 x 10-14 m in diameter. An entire atom can be from 1 – 5 x 10-10 m. The volume outside of the nucleus is called the electron cloud. It is much, much larger than the nucleus.

  4. AMU, isotopes and radioactivity An isotope is one of the possible variants (versions) of any given element that nature has allowed/created. The variation that makes an atom an isotope is the number of neutrons in the nucleus. The number of protons in an atom’s nucleus uniquely determines which element that atom is. The number of neutrons is another matter.

  5. AMU, isotopes and radioactivity Radioactivity refers to the ‘spontaneous’ decay of an atom’s nucleus. The decay happens when part of a nucleus breaks away, or is ‘ejected from the nucleus. It is a form of alchemy, or maybe like a nervous breakdown: when it happens the atom is permanently changed.

  6. There are three primary types of radioactive decay: Alpha, Beta and Gamma. Alpha is the loss of a ‘helium’ nucleus from the parent atom; Beta involves an electron being ejected and Gamma is the emission of powerful waves, like x-rays. AMU, isotopes and radioactivity The symbols (same order as above) for the three types of radioactive decay are: α β ϒ

  7. Radioactive Decay • The atoms of certain elements have unstable nuclei that tend to break apart into more stable atoms. • This breaking apart or decay is called radioactivity. • The original atom is known as the parentatom and the new atoms created by decay are known as the daughteratoms. • There are three types of radioactive decay. Each one differs in what is emitted during decay. Alpha decay involves the loss of a Helium atom from the nucleus. This means that the parent atom changes because The number of protons has been reduced. Daughter Atoms Parent Atom

  8. Parent Material Decay particles Decay particles Radioactive Decay A, Initial condition = 100% Parent 50% Parent Parent Material 50% daughter Daughter material A1 B1 After 1 half life Half life: Amount of time in which half of the isotope will be changed into daughter material. 50%, or ½ of the original amount is still a radioactive isotope 50%, or ½ of the original amount is now a different molecule

  9. Decay particles Condition after 1 half life: 50% Parent, 50% daughter Parent Material Daughter material In another half life A1 has been reduced by 50% again. The newly created daughter material is just like the the other daughter material. B1 A1 New daughter matl 25% Parent After 2 half lives Daughter material Parent Material Daughter material 25%, or 1/4 of the original amount. 75%, or ¾, is daughter material A2 B2

  10. Half-Life • The time that it takes for ½ of the parent material to decay into the daughter material is known as the _____________________. • The half-life is a known amount of time for each element – each element has a different half-life length. • For example, uranium-238 decays into lead-206 at a half-life of 4.5 billion years.

  11. Radiocarbon Dating • When an organism dies, the carbon-14 contained in the body starts to decay. • The ratio of carbon-14 (parent material) to carbon-12 (daughter material) is determined. • The age of the organism is known by known the carbon-14:carbon-12 ratio and the length of the half-life.

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