1![EART163 Homework #5 Due Mon 9th May 2016 Show all your working for full credit Question 1. Here we’re going to look at the transition between simple and complex craters. EART163 Homework #5 Due Mon 9th May 2016 Show all your working for full credit Question 1. Here we’re going to look at the transition between simple and complex craters.](https://www.pdfsearch.io/img/80ebcc0508f68682ac2e723d16472316.jpg) | Add to Reading ListSource URL: www.es.ucsc.eduLanguage: English - Date: 2016-05-03 17:22:15
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2![Crater Count Constraints on Radiolysis of Complex Organic Matter at 2020 Candidate Sites Use crater counts to fit erosion rates at 2020 candidate sites Crater Count Constraints on Radiolysis of Complex Organic Matter at 2020 Candidate Sites Use crater counts to fit erosion rates at 2020 candidate sites](https://www.pdfsearch.io/img/0ccc16db0ad1fb029f96ba01a2f9d455.jpg) | Add to Reading ListSource URL: marsnext.jpl.nasa.govLanguage: English |
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3![REPORTS exceeding 40° when referred to the ellipsoid. Gravitational slopes are slightly less steep but also reach up to ~ 40° on a lower-resolution shape model (~700 m). A considerable number of slopes on Vesta are mos REPORTS exceeding 40° when referred to the ellipsoid. Gravitational slopes are slightly less steep but also reach up to ~ 40° on a lower-resolution shape model (~700 m). A considerable number of slopes on Vesta are mos](https://www.pdfsearch.io/img/a4da2a4ebaaa0f05c2633ff690b641f6.jpg) | Add to Reading ListSource URL: www-ssc.igpp.ucla.eduLanguage: English - Date: 2012-06-22 13:09:07
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4![46th Lunar and Planetary Science Conferencepdf EARHART: A LARGE, PREVIOUSLY UNKNOWN LUNAR NEARSIDE CRATER REVEALED BY GRAIL GRADIOMETRY. R. Sood1, L. Chappaz1, C. Milbury2, D. M. Blair2, H. J. Melosh1,2, an 46th Lunar and Planetary Science Conferencepdf EARHART: A LARGE, PREVIOUSLY UNKNOWN LUNAR NEARSIDE CRATER REVEALED BY GRAIL GRADIOMETRY. R. Sood1, L. Chappaz1, C. Milbury2, D. M. Blair2, H. J. Melosh1,2, an](https://www.pdfsearch.io/img/d7c9420dfdeaa161dc4defe0e6b48449.jpg) | Add to Reading ListSource URL: www.hou.usra.eduLanguage: English - Date: 2015-01-06 09:36:34
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5![Large Meteorite Impacts and Planetary Evolution Vsess451.pdf Wednesday, August 7, 2013 COMPLEX IMPACT CRATERS: THEIR FORMATION AND STRUCTURE Large Meteorite Impacts and Planetary Evolution Vsess451.pdf Wednesday, August 7, 2013 COMPLEX IMPACT CRATERS: THEIR FORMATION AND STRUCTURE](https://www.pdfsearch.io/img/7d027a80c3efc38907eeeee5b0cb8768.jpg) | Add to Reading ListSource URL: www.hou.usra.eduLanguage: English - Date: 2013-07-03 12:01:13
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6![On location, circumnavigating the rim of the Laguna Cuicocha Volcanic Complex crater. An assessment of the volcanic hazards associated with volcanic lake Laguna Cuicocha in Ecuador PhD research undertaken by Jacqueline On location, circumnavigating the rim of the Laguna Cuicocha Volcanic Complex crater. An assessment of the volcanic hazards associated with volcanic lake Laguna Cuicocha in Ecuador PhD research undertaken by Jacqueline](https://www.pdfsearch.io/img/f69a200c0453ad90d7bc6ef66355bb5e.jpg) | Add to Reading ListSource URL: www.minersoc.orgLanguage: English - Date: 2014-04-22 10:40:34
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7![Possible Opaline Silica in the Central Uplift of Elorza Crater Elorza Crater is an approximately 40-kilometer diameter complex crater located at 304.8°E, 8.76°N, about 300 kilometers north of Coprates Possible Opaline Silica in the Central Uplift of Elorza Crater Elorza Crater is an approximately 40-kilometer diameter complex crater located at 304.8°E, 8.76°N, about 300 kilometers north of Coprates](https://www.pdfsearch.io/img/0a94fabbc813a625d61fc0bb53cf1691.jpg) | Add to Reading ListSource URL: static.uahirise.org- Date: 2014-12-15 18:34:32
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8![Getting a Feel for Lunar Craters www.nasa.gov or lunarscience.nasa.gov/ keyword: tactile craters (for more resources and audio files) Getting a Feel for Lunar Craters www.nasa.gov or lunarscience.nasa.gov/ keyword: tactile craters (for more resources and audio files)](https://www.pdfsearch.io/img/6ca95a373f14b06f904d6ab62f955528.jpg) | Add to Reading ListSource URL: sservi.nasa.govLanguage: English - Date: 2013-09-18 16:45:25
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9![Microsoft Word - PCC-Abstract2014-Pluto.docx Microsoft Word - PCC-Abstract2014-Pluto.docx](https://www.pdfsearch.io/img/16c6f38cca8107632f26fb2ae7b93cb7.jpg) | Add to Reading ListSource URL: www.planetarycraterconsortium.nau.eduLanguage: English - Date: 2014-07-31 10:41:49
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10![3-5: Volcano Deformation and Caldera Collapse Introduction How do calderas form in the top of volcanoes?Some form by the violent expulsion of material. But most crater structures on volcanoes form by collapse. When magma 3-5: Volcano Deformation and Caldera Collapse Introduction How do calderas form in the top of volcanoes?Some form by the violent expulsion of material. But most crater structures on volcanoes form by collapse. When magma](https://www.pdfsearch.io/img/3c6c92ecb185752940df4fa5752e20e4.jpg) | Add to Reading ListSource URL: jclahr.comLanguage: English - Date: 2006-04-24 10:33:39
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