Igneous Rocks, Earth Science Lesson PowerPoint

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This PowerPoint is one small part of the Geology Topics unit from www.sciencepowerpoint.com. This unit consists of a five part 6000+ slide PowerPoint roadmap, 14 page bundled homework package, modified homework, detailed answer keys, 12 pages of unit notes for students who may require assistance, follow along worksheets, and many review games. The homework and lesson notes chronologically follow the PowerPoint slideshow. The answer keys and unit notes are great for support professionals. The activities and discussion questions in the slideshow are meaningful. The PowerPoint includes built-in instructions, visuals, and review questions. Also included are critical class notes (color coded red), project ideas, video links, and review games. This unit also includes four PowerPoint review games (110+ slides each with Answers), 38+ video links, lab handouts, activity sheets, rubrics, materials list, templates, guides, 6 PowerPoint review Game, and much more. Also included is a 190 slide first day of school PowerPoint presentation.
Areas of Focus within The Geology Topics Unit: -Plate Tectonics, Evidence for Plate Tectonics, Pangea, Energy Waves, Layers of the Earth, Heat Transfer, Types of Crust, Plate Boundaries, Hot Spots, Volcanoes, Positives and Negatives of Volcanoes, Types of Volcanoes, Parts of a Volcano, Magma, Types of Lava, Viscosity, Earthquakes, Faults, Folds, Seismograph, Richter Scale, Seismograph, Tsunami's, Rocks, Minerals, Crystals, Uses of Minerals, Types of Crystals, Physical Properties of Minerals, Rock Cycle, Common Igneous Rocks, Common Sedimentary Rocks, Common Metamorphic Rocks.
This unit aligns with the Next Generation Science Standards and with Common Core Standards for ELA and Literacy for Science and Technical Subjects. See preview for more information
If you have any questions please feel free to contact me. Thanks again and best wishes. Sincerely, Ryan Murphy M.Ed www.sciencepowerpoint@gmail.com

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Igneous Rocks, Earth Science Lesson PowerPoint

  1. 1. • Which rock is Basalt and which rock is Gabbro? Copyright © 2010 Ryan P. Murphy
  2. 2. • RED SLIDE: These are notes that are very important and should be recorded in your science journal. Copyright © 2010 Ryan P. Murphy
  3. 3. -Nice neat notes that are legible and use indentations when appropriate. -Example of indent. -Skip a line between topics -Don’t skip pages -Make visuals clear and well drawn.
  4. 4. • RED SLIDE: These are notes that are very important and should be recorded in your science journal. • BLACK SLIDE: Pay attention, follow directions, complete projects as described and answer required questions neatly. Copyright © 2010 Ryan P. Murphy
  5. 5. http://sciencepowerpoint.com/Website Link:
  6. 6.  Igneous Rocks: Molten Earth cooled. - - -  - Copyright © 2010 Ryan P. Murphy
  7. 7.  Igneous Rocks: Molten Earth cooled. INtrusive – Cooled below crust (slow) - - - Copyright © 2010 Ryan P. Murphy
  8. 8.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) - - - Copyright © 2010 Ryan P. Murphy
  9. 9.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) - - - Copyright © 2010 Ryan P. Murphy
  10. 10.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals - - Copyright © 2010 Ryan P. Murphy
  11. 11.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals - - Copyright © 2010 Ryan P. Murphy
  12. 12.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals - - Copyright © 2010 Ryan P. Murphy
  13. 13.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals - - Copyright © 2010 Ryan P. Murphy
  14. 14. • Igneous Rocks: Molten Earth cooled. • Intrusive – Cooled below crust (slow) –Larger crystals • - –- Copyright © 2010 Ryan P. Murphy
  15. 15. • Igneous Rocks: Molten Earth cooled. • Intrusive – Cooled below crust (slow) –Larger crystals • - –- Copyright © 2010 Ryan P. Murphy
  16. 16. • Igneous Rocks: Molten Earth cooled. • Intrusive – Cooled below crust (slow) –Larger crystals • - –- Copyright © 2010 Ryan P. Murphy
  17. 17.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals Extrusive – Cooled on Earth’s surface (faster). Copyright © 2010 Ryan P. Murphy
  18. 18.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals Extrusive – Cooled on Earth’s surface (faster). Copyright © 2010 Ryan P. Murphy Can be minutes to seconds.
  19. 19.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals Extrusive – Cooled on Earth’s surface (faster). Copyright © 2010 Ryan P. Murphy
  20. 20.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals Extrusive – Cooled on Earth’s surface (faster). Fine grain crystals or no crystals. Copyright © 2010 Ryan P. Murphy
  21. 21.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals Extrusive – Cooled on Earth’s surface (faster). Fine grain crystals or no crystals. Copyright © 2010 Ryan P. Murphy
  22. 22.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals Extrusive – Cooled on Earth’s surface (faster). Fine grain crystals or no crystals. Copyright © 2010 Ryan P. Murphy
  23. 23.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals Extrusive – Cooled on Earth’s surface (faster). Fine grain crystals or no crystals. Copyright © 2010 Ryan P. Murphy
  24. 24.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals Extrusive – Cooled on Earth’s surface (faster). Fine grain crystals or no crystals. Copyright © 2010 Ryan P. Murphy
  25. 25.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals Extrusive – Cooled on Earth’s surface (faster). Fine grain crystals or no crystals Copyright © 2010 Ryan P. Murphy
  26. 26.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals Extrusive – Cooled on Earth’s surface (faster). Fine grain crystals or no crystals Copyright © 2010 Ryan P. Murphy
  27. 27.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals Extrusive – Cooled on Earth’s surface (faster). Fine grain crystals or no crystals Copyright © 2010 Ryan P. Murphy
  28. 28.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals Extrusive – Cooled on Earth’s surface (faster). Fine grain crystals or no crystals Copyright © 2010 Ryan P. Murphy
  29. 29.  Igneous Rocks: Molten Earth cooled. Intrusive – Cooled below crust (slow) Larger crystals Extrusive – Cooled on Earth’s surface (faster). Fine grain crystals or no crystals Copyright © 2010 Ryan P. Murphy
  30. 30. • Which of the rocks below cooled quickly (Extrusive) and which cooled slowly (Intrusive)? A B
  31. 31. • Which of the rocks below cooled quickly (Extrusive) and which cooled slowly (Intrusive)?
  32. 32. • Which of the rocks below cooled quickly (Extrusive) and which cooled slowly (Intrusive)?
  33. 33. • Which of the rocks below cooled quickly (Extrusive) and which cooled slowly (Intrusive)?
  34. 34. • Which of the rocks below cooled quickly (Extrusive) and which cooled slowly (Intrusive)?
  35. 35. • Which of the rocks below cooled quickly (Extrusive) and which cooled slowly (Intrusive)?
  36. 36. • Which of the rocks below cooled quickly (Extrusive) and which cooled slowly (Intrusive)?
  37. 37. • Which of the rocks below cooled quickly (Extrusive) and which cooled slowly (Intrusive)?
  38. 38. • Which of the rocks below cooled quickly (Extrusive) and which cooled slowly (Intrusive)?
  39. 39. • Which of the rocks below cooled quickly (Extrusive) and which cooled slowly (Intrusive)?
  40. 40. • Which of the rocks below cooled quickly (Extrusive) and which cooled slowly (Intrusive)? Which one has large crystals?
  41. 41. • Which of the rocks below cooled quickly (Extrusive) and which cooled slowly (Intrusive)? Which one has large crystals?
  42. 42. • Which of the rocks below cooled quickly (Extrusive) and which cooled slowly (Intrusive)? Which one has large crystals?
  43. 43. • Which of the rocks below cooled quickly (Extrusive) and which cooled slowly (Intrusive)? Which one has large crystals?
  44. 44. • Can rocks float?
  45. 45. • Can rocks float? • Activity! Floating a piece of pumice.
  46. 46. • Picture of floating Pumice Island. Copyright © 2010 Ryan P. Murphy
  47. 47. • Igneous rocks – Mafic is used for silicate minerals, magmas, and rocks which are relatively high in the heavier elements.
  48. 48. • Igneous rocks – Mafic is used for silicate minerals, magmas, and rocks which are relatively high in the heavier elements. (Magnesium and Iron)
  49. 49. • Igneous rocks – Mafic is used for silicate minerals, magmas, and rocks which are relatively high in the heavier elements. (Magnesium and Iron)
  50. 50. • Igneous rocks – Mafic is used for silicate minerals, magmas, and rocks which are relatively high in the heavier elements. (Magnesium and Iron) – Felsic is used for silicate minerals, magmas, and rocks which have a lower percentage of the heavier elements. Have more of the lighter elements.
  51. 51. • Igneous rocks – Mafic is used for silicate minerals, magmas, and rocks which are relatively high in the heavier elements. (Magnesium and Iron) – Felsic is used for silicate minerals, magmas, and rocks which have a lower percentage of the heavier elements. Have more of the lighter elements. (Silicon and oxygen, aluminum, and potassium)
  52. 52. • Igneous rocks – Mafic is used for silicate minerals, magmas, and rocks which are relatively high in the heavier elements. (Magnesium and Iron) – Felsic is used for silicate minerals, magmas, and rocks which have a lower percentage of the heavier elements. Have more of the lighter elements. (Silicon and oxygen, aluminum, and potassium)
  53. 53. • Igneous rocks – Mafic is used for silicate minerals, magmas, and rocks which are relatively high in the heavier elements. (Magnesium and Iron) – Felsic is used for silicate minerals, magmas, and rocks which have a lower percentage of the heavier elements. Have more of the lighter elements. (Silicon and oxygen, aluminum, and potassium)
  54. 54. • Igneous rocks – Mafic is used for silicate minerals, magmas, and rocks which are relatively high in the heavier elements. (Magnesium and Iron) – Felsic is used for silicate minerals, magmas, and rocks which have a lower percentage of the heavier elements. Have more of the lighter elements. (Silicon and oxygen, aluminum, and potassium)
  55. 55. • Igneous rocks – Mafic is used for silicate minerals, magmas, and rocks which are relatively high in the heavier elements. (Magnesium and Iron) – Felsic is used for silicate minerals, magmas, and rocks which have a lower percentage of the heavier elements. Have more of the lighter elements. (Silicon and oxygen, aluminum, and potassium)
  56. 56. • Igneous rocks – Mafic is used for silicate minerals, magmas, and rocks which are relatively high in the heavier elements. (Magnesium and Iron) – Felsic is used for silicate minerals, magmas, and rocks which have a lower percentage of the heavier elements. Have more of the lighter elements. (Silicon and oxygen, aluminum, and potassium) Feldspar
  57. 57.  Igneous rocks
  58. 58.  Igneous rocks  Mafic – Darker in color (Heavy Elements)
  59. 59.  Igneous rocks  Mafic – Darker in color (Heavy Elements)  Iron, Magnesium
  60. 60.  Igneous rocks  Mafic – Darker in color (Heavy Elements)  Iron, Magnesium
  61. 61.  Igneous rocks  Mafic – Darker in color (Heavy Elements)  Iron, Magnesium  Felsic – Lighter in color (Lighter Elements)
  62. 62.  Igneous rocks  Mafic – Darker in color (Heavy Elements)  Iron, Magnesium  Felsic – Lighter in color (Lighter Elements)  Oxygen, Silicon, Aluminum,
  63. 63. • Which is considered mafic, and which is felsic?
  64. 64. • Which is considered mafic, and which is felsic?
  65. 65. • Which is considered mafic, and which is felsic?
  66. 66. • Which is considered mafic, and which is felsic?
  67. 67. • Which is considered mafic, and which is felsic?
  68. 68. • Which is considered mafic, and which is felsic?
  69. 69. • Which is considered mafic, and which is felsic?
  70. 70. • Which is considered mafic, and which is felsic?
  71. 71. • Which is considered mafic, and which is felsic?
  72. 72. • Which is considered mafic, and which is felsic?
  73. 73. • Which is considered mafic, and which is felsic?
  74. 74. • Note: Although Obsidian looks “Dark”
  75. 75. • Note: Although Obsidian looks “Dark” It’s actually clear and Felsic in Chemistry.
  76. 76. • Note: Although Obsidian looks “Dark” It’s actually clear and Felsic in Chemistry. Obsidian consists mainly of SiO2 (silicon dioxide), usually 70% or more
  77. 77. • Note: Although Obsidian looks “Dark” It’s actually clear and Felsic in Chemistry. Can sometimes also be an intermediate between felsic and mafic.
  78. 78. • Note: Although Obsidian looks “Dark” It’s actually clear and Felsic in Chemistry. Can sometimes also be an intermediate between felsic and mafic.
  79. 79. • Which rocks are incorrectly labeled below? PumiceBasalt RhyoliteObsidian Granite Copyright © 2010 Ryan P. Murphy Pumice
  80. 80. • Which rocks are incorrectly labeled below? PumiceBasalt RhyoliteObsidian Granite Copyright © 2010 Ryan P. Murphy Pumice
  81. 81. • Which rocks are incorrectly labeled below? PumiceBasalt RhyoliteObsidian Granite Copyright © 2010 Ryan P. Murphy Pumice
  82. 82. • Which rock is incorrectly labeled below? PumiceBasalt RhyoliteObsidian Granite Copyright © 2010 Ryan P. Murphy Pumice Basalt
  83. 83. • Which rock is incorrectly labeled below? PumiceBasalt RhyoliteObsidian Granite Copyright © 2010 Ryan P. Murphy Pumice Basalt
  84. 84. • Which rock is incorrectly labeled below? PumiceBasalt RhyoliteObsidian Granite Copyright © 2010 Ryan P. Murphy Pumice Basalt
  85. 85. • Which rock is incorrectly labeled below? PumiceBasalt RhyoliteObsidian Granite Copyright © 2010 Ryan P. Murphy Pumice Basalt
  86. 86.  Classification of Igneous Rocks  -  -  - Copyright © 2010 Ryan P. Murphy
  87. 87.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy
  88. 88.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy
  89. 89.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy
  90. 90.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy
  91. 91.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy
  92. 92.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy
  93. 93.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy
  94. 94.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy
  95. 95.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy
  96. 96.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy
  97. 97.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy
  98. 98.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy Basalt is fine-grained so that the individual minerals are not visible. Basalt includes pyroxene, plagioclase feldspar and olivine. These minerals are visible in the coarse-grained basalt called gabbro.
  99. 99.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy Basalt is fine-grained so that the individual minerals are not visible. Basalt includes pyroxene, plagioclase feldspar and olivine. These minerals are visible in the coarse-grained basalt called gabbro.
  100. 100.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy Basalt is fine-grained so that the individual minerals are not visible. Basalt includes pyroxene, plagioclase feldspar and olivine. These minerals are visible in the coarse-grained basalt called gabbro.
  101. 101.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy Basalt is fine-grained so that the individual minerals are not visible. Basalt includes pyroxene, plagioclase feldspar and olivine. These minerals are visible in the coarse-grained basalt called gabbro.
  102. 102.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy Basalt is fine-grained so that the individual minerals are not visible. Basalt includes pyroxene, plagioclase feldspar and olivine. These minerals are visible in the coarse-grained basalt called gabbro.
  103. 103.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy Basalt is fine-grained so that the individual minerals are not visible. Basalt includes pyroxene, plagioclase feldspar and olivine. These minerals are visible in the coarse-grained basalt called gabbro.
  104. 104.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy Basalt is fine-grained so that the individual minerals are not visible. Basalt includes pyroxene, plagioclase feldspar and olivine. These minerals are visible in the coarse-grained basalt called gabbro.
  105. 105.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy Basalt is fine-grained so that the individual minerals are not visible. Basalt includes pyroxene, plagioclase feldspar and olivine. These minerals are visible in the coarse-grained basalt called gabbro.
  106. 106.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy Basalt is fine-grained so that the individual minerals are not visible. Basalt includes pyroxene, plagioclase feldspar and olivine. These minerals are visible in the coarse-grained basalt called gabbro.
  107. 107.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy Basalt is fine-grained so that the individual minerals are not visible. Basalt includes pyroxene, plagioclase feldspar and olivine. These minerals are visible in the coarse-grained basalt called gabbro.
  108. 108.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy Basalt is fine-grained so that the individual minerals are not visible. Basalt includes pyroxene, plagioclase feldspar and olivine. These minerals are visible in the coarse-grained basalt called gabbro.
  109. 109.  Basaltic: Dark, heavy (dense) Copyright © 2010 Ryan P. Murphy Basalt is fine-grained so that the individual minerals are not visible. Basalt includes pyroxene, plagioclase feldspar and olivine. These minerals are visible in the coarse-grained basalt called gabbro.
  110. 110. “It looked bigger in the brochure Honey”
  111. 111.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy
  112. 112.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy
  113. 113.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy
  114. 114.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy
  115. 115.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals.
  116. 116.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals.
  117. 117.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals.
  118. 118.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals.
  119. 119.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals.
  120. 120.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals.
  121. 121.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals.
  122. 122.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals.
  123. 123.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals.
  124. 124.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals.
  125. 125.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals.
  126. 126.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals.
  127. 127.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals.
  128. 128.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals.
  129. 129.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals.
  130. 130.  Granitic: Light colored, less heavy, filled with oxygen. Copyright © 2010 Ryan P. Murphy Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals.
  131. 131.  Andesitic: Intermediate. Copyright © 2010 Ryan P. Murphy
  132. 132.  Andesitic: Intermediate. Copyright © 2010 Ryan P. Murphy
  133. 133.  Andesitic: Intermediate. Copyright © 2010 Ryan P. Murphy
  134. 134.  Andesitic: Intermediate. Copyright © 2010 Ryan P. Murphy
  135. 135.  Andesitic: Intermediate. Copyright © 2010 Ryan P. Murphy
  136. 136.  Andesitic: Intermediate. Copyright © 2010 Ryan P. Murphy
  137. 137.  Andesitic: Intermediate. Copyright © 2010 Ryan P. Murphy
  138. 138.  Andesitic: Intermediate. Copyright © 2010 Ryan P. Murphy
  139. 139. • Quiz 1-10, Is it Basaltic, Granitic or Name the Rock Band. Copyright © 2010 Ryan P. Murphy
  140. 140. • Quiz 1-10, Is it Basaltic, Granitic or Name the Rock Band. Copyright © 2010 Ryan P. Murphy
  141. 141. • Quiz 1-10, Is it Basaltic, Granitic or Name the Rock Band. Copyright © 2010 Ryan P. Murphy
  142. 142. • Quiz 1-10, Is it Basaltic, Granitic or Name the Rock Band. Copyright © 2010 Ryan P. Murphy Rock and Roll Quiz Music at… http://www.youtube.com/watch?v=5XfRjVo5wOE
  143. 143. • Answers 1-10. Is it Basaltic, Granitic, or name that rock band. Copyright © 2010 Ryan P. Murphy
  144. 144.  Common Igneous Rocks  -  -  -  -  - Copyright © 2010 Ryan P. Murphy
  145. 145.  Granite is an Igneous Rock.  Quartz and feldspar minerals. Copyright © 2010 Ryan P. Murphy
  146. 146.  Granite is an Igneous Rock.  Quartz and feldspar minerals, Copyright © 2010 Ryan P. Murphy
  147. 147.  Granite is an Igneous Rock.  Quartz and feldspar minerals, Copyright © 2010 Ryan P. Murphy
  148. 148.  Granite is an Igneous Rock.  Quartz and feldspar minerals, Copyright © 2010 Ryan P. Murphy
  149. 149.  Granite is an Igneous Rock.  Quartz and feldspar minerals, Copyright © 2010 Ryan P. Murphy
  150. 150.  Granite is an Igneous Rock.  Quartz and feldspar minerals, Copyright © 2010 Ryan P. Murphy
  151. 151.  Granite is an Igneous Rock.  Quartz and feldspar minerals, Copyright © 2010 Ryan P. Murphy
  152. 152.  Granite is an Igneous Rock.  Quartz and feldspar minerals, Copyright © 2010 Ryan P. Murphy
  153. 153.  Granite is an Igneous Rock.  Quartz and feldspar minerals, and mica. Copyright © 2010 Ryan P. Murphy
  154. 154.  Granite is an Igneous Rock.  Quartz and feldspar minerals, and mica. Copyright © 2010 Ryan P. Murphy
  155. 155.  Granite is an Igneous Rock.  Quartz and feldspar minerals, and mica. Copyright © 2010 Ryan P. Murphy
  156. 156.  Pumice Copyright © 2010 Ryan P. Murphy ?????????
  157. 157.  Pumice Copyright © 2010 Ryan P. Murphy
  158. 158.  Pumice Copyright © 2010 Ryan P. Murphy
  159. 159.  Pumice Copyright © 2010 Ryan P. Murphy
  160. 160.  Pumice Copyright © 2010 Ryan P. Murphy
  161. 161.  Pumice Copyright © 2010 Ryan P. Murphy
  162. 162.  Pumice Copyright © 2010 Ryan P. Murphy
  163. 163.  Pumice Copyright © 2010 Ryan P. Murphy
  164. 164.  Pumice Copyright © 2010 Ryan P. Murphy
  165. 165.  Pumice Copyright © 2010 Ryan P. Murphy
  166. 166.  Pumice Copyright © 2010 Ryan P. Murphy
  167. 167.  Obsidian  Glassy Copyright © 2010 Ryan P. Murphy
  168. 168.  Obsidian  Glassy Copyright © 2010 Ryan P. Murphy
  169. 169.  Obsidian  Glassy Copyright © 2010 Ryan P. Murphy
  170. 170.  Obsidian  Glassy Copyright © 2010 Ryan P. Murphy
  171. 171.  Obsidian  Glassy Copyright © 2010 Ryan P. Murphy
  172. 172.  Obsidian  Glassy Copyright © 2010 Ryan P. Murphy
  173. 173.  Obsidian  Glassy Copyright © 2010 Ryan P. Murphy
  174. 174.  Obsidian  Glassy Copyright © 2010 Ryan P. Murphy
  175. 175.  Obsidian  Glassy Copyright © 2010 Ryan P. Murphy
  176. 176.  Obsidian  Glassy Copyright © 2010 Ryan P. Murphy
  177. 177.  Obsidian  Glassy Copyright © 2010 Ryan P. Murphy
  178. 178.  Obsidian  Glassy Copyright © 2010 Ryan P. Murphy
  179. 179.  Obsidian  Glassy Copyright © 2010 Ryan P. Murphy
  180. 180.  Obsidian  Glassy Copyright © 2010 Ryan P. Murphy
  181. 181.  Obsidian  Glassy Copyright © 2010 Ryan P. Murphy
  182. 182.  Obsidian  Glassy Copyright © 2010 Ryan P. Murphy
  183. 183. • Obsidian was an important rock to ancient peoples as it could be used as a cutting tool.
  184. 184. • Video: Flintknapping (The process of making stone tools). – Hornstone (Not Obsidian) used in video although the process is similar. – http://www.youtube.com/watch?v=- cHM8rfmQII&feature=fvsr
  185. 185.  Rhyolite
  186. 186.  Rhyolite
  187. 187.  Rhyolite
  188. 188.  Rhyolite
  189. 189.  Rhyolite
  190. 190.  Rhyolite
  191. 191.  Rhyolite
  192. 192.  Rhyolite
  193. 193.  Rhyolite
  194. 194. • Which is Rhyolite and which is Granite?
  195. 195. • Which is Rhyolite and which is Granite?
  196. 196. • Which is Rhyolite and which is Granite?
  197. 197. • Which is Rhyolite and which is Granite?
  198. 198. • Which is Rhyolite and which is Granite?
  199. 199. • Which is Rhyolite and which is Granite?
  200. 200. • Which is Rhyolite and which is Granite?
  201. 201. • Which is Rhyolite and which is Granite?
  202. 202. • Which rock is Obsidian and which is Pumice? Copyright © 2010 Ryan P. Murphy
  203. 203. • Which rock is Obsidian and which is Pumice? Copyright © 2010 Ryan P. Murphy
  204. 204. • Which rock is Obsidian and which is Pumice? Copyright © 2010 Ryan P. Murphy
  205. 205. • Which rock is Obsidian and which is Pumice? Copyright © 2010 Ryan P. Murphy
  206. 206. • Which rock is Obsidian and which is Pumice? Copyright © 2010 Ryan P. Murphy
  207. 207. • Which rock is Obsidian and which is Pumice? Copyright © 2010 Ryan P. Murphy
  208. 208. • Which rock is Obsidian and which is Pumice? Copyright © 2010 Ryan P. Murphy
  209. 209. • Which rock is Obsidian and which is Pumice? Copyright © 2010 Ryan P. Murphy
  210. 210. • Which pumice sample is made of heavy elements such as Iron?
  211. 211. • Which pumice sample is made of heavy elements such as Iron?
  212. 212. • Which pumice sample is made of heavy elements such as Iron?
  213. 213. • Which rock is Rhyolite, and which is Pumice? Copyright © 2010 Ryan P. Murphy
  214. 214. • Which rock is Rhyolite, and which is Pumice? Copyright © 2010 Ryan P. Murphy
  215. 215. • Which rock is Rhyolite, and which is Pumice? Copyright © 2010 Ryan P. Murphy
  216. 216. • Which rock is Rhyolite, and which is Pumice? Copyright © 2010 Ryan P. Murphy
  217. 217. • Which rock is Rhyolite, and which is Pumice? Copyright © 2010 Ryan P. Murphy
  218. 218.  Basalt.????????? Copyright © 2010 Ryan P. Murphy
  219. 219.  Basalt. Copyright © 2010 Ryan P. Murphy
  220. 220.  Basalt. Copyright © 2010 Ryan P. Murphy Basalt is a mixture of feldspar and pyroxene, a rock made mainly of silica and oxygen. Little… Quartz (Less than 20%)
  221. 221.  Basalt. Copyright © 2010 Ryan P. Murphy Basalt is a mixture of feldspar and pyroxene, a rock made mainly of silica and oxygen. Little… Quartz (Less than 20%)
  222. 222.  Basalt. Copyright © 2010 Ryan P. Murphy Basalt is a mixture of feldspar and pyroxene, a rock made mainly of silica and oxygen. Little… Quartz (Less than 20%)
  223. 223.  Basalt. Copyright © 2010 Ryan P. Murphy Basalt is a mixture of feldspar and pyroxene, a rock made mainly of silica and oxygen. Little… Quartz (Less than 20%)
  224. 224.  Basalt. Copyright © 2010 Ryan P. Murphy Basalt is a mixture of feldspar and pyroxene, a rock made mainly of silica and oxygen. Little… Quartz (Less than 20%)
  225. 225.  Basalt. Copyright © 2010 Ryan P. Murphy Basalt is a mixture of feldspar and pyroxene, a rock made mainly of silica and oxygen. Little… Quartz (Less than 20%)
  226. 226.  Basalt. Copyright © 2010 Ryan P. Murphy Basalt is a mixture of feldspar and pyroxene, a rock made mainly of silica and oxygen. Little… Quartz (Less than 20%)
  227. 227.  Basalt. Copyright © 2010 Ryan P. Murphy Basalt is a mixture of feldspar and pyroxene, a rock made mainly of silica and oxygen. Little… Quartz (Less than 20%)
  228. 228.  Basalt. Copyright © 2010 Ryan P. Murphy Basalt is a mixture of feldspar and pyroxene, a rock made mainly of silica and oxygen. Little… Quartz (Less than 20%)
  229. 229.  Gabbro  - Copyright © 2010 Ryan P. Murphy
  230. 230.  Gabbro  Same composition as basalt but cooled slower (Intrusive) Copyright © 2010 Ryan P. Murphy
  231. 231.  Gabbro  Same composition as basalt but cooled slower (Intrusive) Copyright © 2010 Ryan P. Murphy
  232. 232.  Gabbro  Same composition as basalt but cooled slower (Intrusive) Copyright © 2010 Ryan P. Murphy
  233. 233.  Gabbro  Same composition as basalt but cooled slower (Intrusive) Copyright © 2010 Ryan P. Murphy
  234. 234.  Gabbro  Same composition as basalt but cooled slower (Intrusive) Copyright © 2010 Ryan P. Murphy
  235. 235.  Gabbro  Same composition as basalt but cooled slower (Intrusive) Copyright © 2010 Ryan P. Murphy
  236. 236.  Gabbro  Same composition as basalt but cooled slower (Intrusive) Copyright © 2010 Ryan P. Murphy
  237. 237.  Gabbro  Same composition as basalt but cooled slower (Intrusive) Copyright © 2010 Ryan P. Murphy
  238. 238.  Gabbro  Same composition as basalt but cooled slower (Intrusive) Copyright © 2010 Ryan P. Murphy
  239. 239.  Gabbro  Same composition as basalt but cooled slower (Intrusive) Copyright © 2010 Ryan P. Murphy
  240. 240.  Gabbro  Same composition as basalt but cooled slower (Intrusive) Copyright © 2010 Ryan P. Murphy
  241. 241.  Gabbro  Same composition as basalt but cooled slower (Intrusive) Copyright © 2010 Ryan P. Murphy
  242. 242.  Gabbro  Same composition as basalt but cooled slower (Intrusive) Copyright © 2010 Ryan P. Murphy
  243. 243.  Gabbro  Same composition as basalt but cooled slower (Intrusive) Copyright © 2010 Ryan P. Murphy
  244. 244. • Gabbro – A large group of dark,
  245. 245. • Gabbro – A large group of dark, coarse-grained,
  246. 246. • Gabbro – A large group of dark, coarse-grained, intrusive mafic igneous rocks chemically equivalent to basalt.
  247. 247. • Gabbro – A large group of dark, coarse- grained, intrusive mafic igneous rocks chemically equivalent to basalt.
  248. 248. • Gabbro – A large group of dark, coarse-grained, intrusive mafic igneous rocks chemically equivalent to basalt. Formed when molten magma is trapped beneath the earth's surface and cools into a crystalline mass.
  249. 249. • Gabbro – A large group of dark, coarse-grained, intrusive mafic igneous rocks chemically equivalent to basalt. Formed when molten magma is trapped beneath the earth's surface and cools into a crystalline mass. (Slowly)
  250. 250. • Gabbro
  251. 251. • Develop your film.
  252. 252. • Which rock is Basalt and which rock is Gabbro? Copyright © 2010 Ryan P. Murphy
  253. 253. • Which rock is Basalt and which rock is Gabbro? Copyright © 2010 Ryan P. Murphy
  254. 254. • Which rock is Basalt and which rock is Gabbro? Copyright © 2010 Ryan P. Murphy
  255. 255. • Which rock is Basalt and which rock is Gabbro? Copyright © 2010 Ryan P. Murphy
  256. 256. • Which rock is Basalt and which rock is Gabbro? Copyright © 2010 Ryan P. Murphy
  257. 257. • Which rock is Basalt and which rock is Gabbro? Copyright © 2010 Ryan P. Murphy
  258. 258. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  259. 259. • Answer!
  260. 260. F I N D G A B B R O
  261. 261. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  262. 262. • Answer! Copyright © 2010 Ryan P. Murphy
  263. 263. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  264. 264. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  265. 265. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  266. 266. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  267. 267. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  268. 268. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  269. 269. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  270. 270. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  271. 271. • Which rocks below are Gabbro? Copyright © 2010 Ryan P. Murphy
  272. 272. • Which rocks below are Gabbro? Copyright © 2010 Ryan P. Murphy
  273. 273. • Which rocks below are Gabbro? Copyright © 2010 Ryan P. Murphy
  274. 274. • Which rocks below are Gabbro? Copyright © 2010 Ryan P. Murphy
  275. 275. • Which rocks below are Gabbro? Copyright © 2010 Ryan P. Murphy
  276. 276. • Which rocks below are Gabbro? Copyright © 2010 Ryan P. Murphy
  277. 277. • Which rocks below are Gabbro? Copyright © 2010 Ryan P. Murphy
  278. 278. • Which rocks below are Gabbro? Copyright © 2010 Ryan P. Murphy
  279. 279. • Which rocks below are Gabbro? Copyright © 2010 Ryan P. Murphy
  280. 280. • Which rocks below are Gabbro? Copyright © 2010 Ryan P. Murphy
  281. 281. • Which rocks below are Gabbro? Copyright © 2010 Ryan P. Murphy
  282. 282. • Which rocks below are Gabbro? Copyright © 2010 Ryan P. Murphy
  283. 283. • Which rocks below are Gabbro? Copyright © 2010 Ryan P. Murphy
  284. 284. • Which rocks below are Gabbro? Copyright © 2010 Ryan P. Murphy
  285. 285. • Which rocks below are Gabbro? Copyright © 2010 Ryan P. Murphy
  286. 286. • Which rocks below are Gabbro? Copyright © 2010 Ryan P. Murphy
  287. 287. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  288. 288. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  289. 289. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  290. 290. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  291. 291. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  292. 292. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  293. 293. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  294. 294. • Which rock below is Gabbro? Copyright © 2010 Ryan P. Murphy
  295. 295. Igneous Rocks. Learn more at… http://geology.com/rocks/igneous-rocks.shtml
  296. 296. • Which rock is incorrectly labeled below? Basalt Obsidian Rhyolite Gabbro Granite Copyright © 2010 Ryan P. Murphy
  297. 297. • Answer! Basalt Obsidian Rhyolite Gabbro Granite Copyright © 2010 Ryan P. Murphy
  298. 298. • Answer! Should be Pumice not Gabbro. Basalt Obsidian Rhyolite Granite Copyright © 2010 Ryan P. Murphy
  299. 299. • Which rock is correctly labeled below? Pumice Basalt Rhyolite Obsidian Gabbro Copyright © 2010 Ryan P. Murphy
  300. 300. • Answer! Rhyolite. Pumice Basalt Rhyolite Obsidian Gabbro Copyright © 2010 Ryan P. Murphy
  301. 301. • Answer! Rhyolite. Basalt Obsidian Rhyolite Pumice Granite Copyright © 2010 Ryan P. Murphy
  302. 302. • Which rock is incorrectly labeled below? PumiceBasalt RhyoliteObsidian Granite Copyright © 2010 Ryan P. Murphy Pumice
  303. 303. • Which rock is incorrectly labeled below? PumiceBasalt RhyoliteObsidian Granite Copyright © 2010 Ryan P. Murphy Pumice
  304. 304. • Which rock is incorrectly labeled below? PumiceBasalt RhyoliteObsidian Granite Copyright © 2010 Ryan P. Murphy Pumice
  305. 305. • Which two rocks are switched? Obsidian Basalt Rhyolite Pumice Granite Copyright © 2010 Ryan P. Murphy
  306. 306. • Answer! Basalt (Bottom) and Obsidian (top) Obsidian Basalt Rhyolite Pumice Granite Copyright © 2010 Ryan P. Murphy
  307. 307. • Answer! Basalt (Bottom) and Obsidian (top) Basalt Obsidian Rhyolite Pumice Granite Copyright © 2010 Ryan P. Murphy
  308. 308. • Try and guess the hidden picture beneath the boxes. – Raise your hand when you think you know. You only get one guess. Copyright © 2010 Ryan P. Murphy
  309. 309. • Try and guess the hidden picture beneath the boxes. – Raise your hand when you think you know. You only get one guess. Copyright © 2010 Ryan P. Murphy
  310. 310. “Here comes a magic trick with pumice.”
  311. 311. “Mafnificent.”
  312. 312. • Try and guess the hidden picture beneath the boxes. – Raise your hand when you think you know. You only get one guess. Copyright © 2010 Ryan P. Murphy
  313. 313. “Here comes a gneiss magic trick. I’m going to disappear.”
  314. 314. • Activity! Rocks PowerPoint Review Game Copyright © 2010 Ryan P. Murphy
  315. 315. http://sciencepowerpoint.com/Website Link:
  316. 316. • This part of the PowerPoint roadmap is just one small part of my Geology Topics Unit. This unit includes… • A six part 6,000 Slide PowerPoint Presentation / unit roadmap full of activities, review questions, games, video links, flashcards, materials list, and much more. • A 18 bundled homework package, modified version, 19 pages of unit notes, 6 PowerPoint Review Games of 100+ slides each, videos, rubrics, and much more that all chronologically follow the unit slideshow. • This is a fantastic unit for any Earth Science Class. • http://sciencepowerpoint.com/Geology_Unit.html
  317. 317. Areas of Focus within The Geology Topics Unit: -Areas of Focus within The Geology Topics Unit: Plate Tectonics, Evidence for Plate Tectonics, Pangea, Energy Waves, Layers of the Earth, Heat Transfer, Types of Crust, Plate Boundaries, Hot Spots, Volcanoes, Positives and Negatives of Volcanoes, Types of Volcanoes, Parts of a Volcano, Magma, Types of Lava, Viscosity, Earthquakes, Faults, Folds, Seismograph, Richter Scale, Seismograph, Tsunami’s, Rocks, Minerals, Crystals, Uses of Minerals, Types of Crystals, Physical Properties of Minerals, Rock Cycle, Common Igneous Rocks, Common Sedimentary Rocks, Common Metamorphic Rocks., Age of the Earth, Uniformitarianism, Principle of Superposition, Earth History, Time Units, Timeline of Events, Basic Evolution, Mass Extinction Events, Dinosaurs, Early Mammals, and more. Full Unit can be found at… http://sciencepowerpoint.com/Geology_Unit.html
  318. 318. • This was a very brief tour. Please visit the links below to learn more about each of the units in this curriculum package. – These units take me about four years to complete with my students in grades 5-10. Earth Science Units Extended Tour Link and Curriculum Guide Geology Topics Unit http://sciencepowerpoint.com/Geology_Unit.html Astronomy Topics Unit http://sciencepowerpoint.com/Astronomy_Unit.html Weather and Climate Unit http://sciencepowerpoint.com/Weather_Climate_Unit.html Soil Science, Weathering, More http://sciencepowerpoint.com/Soil_and_Glaciers_Unit.html Water Unit http://sciencepowerpoint.com/Water_Molecule_Unit.html Rivers Unit http://sciencepowerpoint.com/River_and_Water_Quality_Unit.html = Easier = More Difficult = Most Difficult 5th – 7th grade 6th – 8th grade 8th – 10th grade
  319. 319. Physical Science Units Extended Tour Link and Curriculum Guide Science Skills Unit http://sciencepowerpoint.com/Science_Introduction_Lab_Safety_Metric_Methods. html Motion and Machines Unit http://sciencepowerpoint.com/Newtons_Laws_Motion_Machines_Unit.html Matter, Energy, Envs. Unit http://sciencepowerpoint.com/Energy_Topics_Unit.html Atoms and Periodic Table Unit http://sciencepowerpoint.com/Atoms_Periodic_Table_of_Elements_Unit.html Life Science Units Extended Tour Link and Curriculum Guide Human Body / Health Topics http://sciencepowerpoint.com/Human_Body_Systems_and_Health_Topics_Unit.html DNA and Genetics Unit http://sciencepowerpoint.com/DNA_Genetics_Unit.html Cell Biology Unit http://sciencepowerpoint.com/Cellular_Biology_Unit.html Infectious Diseases Unit http://sciencepowerpoint.com/Infectious_Diseases_Unit.html Taxonomy and Classification Unit http://sciencepowerpoint.com/Taxonomy_Classification_Unit.html Evolution / Natural Selection Unit http://sciencepowerpoint.com/Evolution_Natural_Selection_Unit.html Botany Topics Unit http://sciencepowerpoint.com/Plant_Botany_Unit.html Ecology Feeding Levels Unit http://sciencepowerpoint.com/Ecology_Feeding_Levels_Unit.htm Ecology Interactions Unit http://sciencepowerpoint.com/Ecology_Interactions_Unit.html Ecology Abiotic Factors Unit http://sciencepowerpoint.com/Ecology_Abiotic_Factors_Unit.html
  320. 320. • More Units Available at… Earth Science: The Soil Science and Glaciers Unit, The Geology Topics Unit, The Astronomy Topics Unit, The Weather and Climate Unit, and The Rivers and Water Quality Unit, The Water Molecule Unit. Physical Science: The Laws of Motion and Machines Unit, The Atoms and Periodic Table Unit, The Energy and the Environment Unit, and Science Skills Unit. Life Science: The Diseases and Cells Unit, The DNA and Genetics Unit, The Life Topics Unit, The Plant Unit, The Taxonomy and Classification Unit, Ecology: Feeding Levels Unit, Ecology: Interactions Unit, Ecology: Abiotic Factors, The Evolution and Natural Selection Unit and The Human Body Systems and Health Topics Unit Copyright © 2010 Ryan P. Murphy
  321. 321. • The entire four year curriculum can be found at... http://sciencepowerpoint.com/ Please feel free to contact me with any questions you may have. Thank you for your interest in this curriculum. Sincerely, Ryan Murphy M.Ed www.sciencepowerpoint@gmail.com
  322. 322. http://sciencepowerpoint.com/Website Link:

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