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BGSU GEOL 1040 - Early Ideas on Earth's Interior
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Geol 1040 1st Edition Lecture 5Outline of Last Lecture VI. How geology influences where and how we livea. Volcanoesb. Landslidesc. Riversd. Earth QuakesVII. Distribution of Natural Resourcesa. Copperb. IronVIII. Parts of the Eartha. Crustb. Mantlec. CoreOutline of Current Lecture IX. Early Ideas on Earth’s Interiora. Heavily influenced by the Mediterraneanb. Dark ages 400-1000c. Athanasius Kircherd. 1724 Nebular Hypothesise. Ridgety of EarthCurrent LectureX. Early Ideas on Earth’s Interiora. Heavily influenced by the Mediterraneani. Many major volcanoes in this regionii. One idea thought that Earth was hollow and wind rubbed against walls that crated friction and ignited sulfur.iii. Idea came from observation of volcanic eruptions. A powerful sulfur smelland big up heave of Earth’s materials made them think wind played a role. b. Dark ages 400-1000i. Dante’s Infernoii. Not something the church should study These notes represent a detailed interpretation of the professor’s lecture. GradeBuddy is best used as a supplement to your own notes, not as a substitute.c. Athanasius Kircheri. 1600’sii. There has to be a central fireiii. Constructed first diagram of inner earth d. 1724 Nebular Hypothesisi. Molten interiore. Ridgety of Earthi. Earths movement is based on Earth’s tide and gravitational attraction from Moon and sunii. Earth’s Interior is very hot but very solidAthanasius Kircher’s diagram of Inner Earth. Showing that there was a molten interior as a heat


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BGSU GEOL 1040 - Early Ideas on Earth's Interior

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