QUESTION IMPORTANCE. It is important to find ice if the idea of humans on Mars would ever become a possibility.
|
|
- Dwain Briggs
- 6 years ago
- Views:
Transcription
1 MSIP TEAM KAPPA
2 SCIENCE QUESTION How can crater diameter and rampart diameter ratios of rampart craters be used to find different amounts of ice present in the Northern and Southern parts of Mars?
3 HYPOTHESES Main: Rampart Crater ratios will be larger in the Northern part of Mars. Alternate: Rampart Crater ratios will not change in the Northern and Southern areas of Mars.
4 QUESTION IMPORTANCE It is important to find ice if the idea of humans on Mars would ever become a possibility.
5 DEFINITIONS Rampart crater- A specific type of Martian impact crater which are accompanied by distinctive fluidized ejecta features, have evidence of ice or liquid water beneath the surface. Chryse - A smooth circular plain in the northern equatorial region, located at 320, 28. Solis Lacus Albedo- A dark feature know as "The Eye of Mars located at 270, -27 Alba Mons- A volcano in the Northern region located at 250, 40 Utopia - A large impact basin on Mars located at 118, 49 Malea Patera- Located Southwest of Hellas at 312, 63 Pityusa Rupes- Located Southwest of Hellas at 64, 29 Acidalia - A plain located between the Tharsis volcanic province and Arabia Terra to the north of Valles Marineris, centered at 46, 42 CTX image- A picture from the context camera found on the space craft named The Mars Reconnaissance Orbiter (MRO). Themis image- A picture from the Themis camera found on the space craft named The Odyssey.
6 Black arrow: Crater Red arrow: Rampart CONTROL IMAGES Chryse Themis Camera V Solis Lacus Albedo Context camera (CTX) B05_011544_1508_XI_29S87W
7 CONTROL IMAGES Pityusa Rupes B02_010406_XI_61S332W Acidalia V
8 Black arrow: Crater Red arrow: Rampart CONTROL IMAGE Utopia V
9 MARS/EARTH COMPARISON Mars Earth Haughton Crater V
10 Black arrow: Crater Red arrow: Rampart CONTROL IMAGES B19_016925_2431_XN_63N127W Alba Mons G03_019438_1223_XN_57S318W Malea Patera
11 RESEARCH Ages of rampart craters in equatorial regions on Mars: Implications for the past and present distribution of ground ice: D. Reiss, S. Gasselt, E. Hauber, G. Michael, R. Jaumann, G. Neukum(2006) Scientist are testing the theory that rampart craters may have formed a significant time ago, which would mean that the minimum diameter of the crater would only reflect the ice depth at that certain time. The tests showed that a rampart crater will form within or shortly after water activity can cause a lowering of ground ice tables which is indicated by the increase of the crater diameter.
12 CTX Image ID# Latitude Longitude Crater Diameter (KM) Rampart Diameter (KM) Ratio Region P12_005545_1515_XI_28S093W E :7.31 Solis Lacus Albedo P18_008050_1500_XI_28S093W E :16.5 Solis Lacus Albedo B01_009843_1525_XI_27S087W E :10.72 Solis Lacus Albedo B01_009922_1530 XI_27S085W E :8.8 Solis Lacus Albedo P11_005426_1530_XN_27S084W E :8.8 Solis Lacus Albedo P11_005426_1530_XN_27S084W E :11.1 Solis Lacus Albedo P19_008498_1529_XI_27S E :11.1 Solis Lacus Albedo B16_015984_1508_XN_29S081W E :10.5 Solis Lacus Albedo P13_006138_1555_XN_24S084W E :10.33 Solis Lacus Albedo B05_011557_1512_XI_28S082W E :8.95 Solis Lacus Albedo B22_018058_XN_24S087W E :6.17 Solis Lacus Albedo P18_008050_1500_XN_30S089W E :17.8 Solis Lacus Albedo P17_007483_1484_XI_31S086W E :8.6 Solis Lacus Albedo B18_016832_1514_XN_28S094W E :6.34 Solis Lacus Albedo
13 CTX Image ID # Latitude Longitude Crater Diameter (KM) Rampart Diameter (KM) Ratio Region B05_011544_1508_XI_29S 087W E :9 Solis Lacus Albedo P18_007958_1514_XN_28 S098W P21_009355_1493_XI_30S 084W P20_008722_1542_XN_25 S081W B09_013113_1580_XI_22S 083W P10_004925_1592_XI_20S 087W P11_005347_1596_XN_20 S088W P22_009487_1527_XI_27S 088W B03_010819_1561_XN_23 S094W E :8.5 Solis Lacus Albedo E :8.4 Solis Lacus Albedo E :9.6 Solis Lacus Albedo E :5.01 Solis Lacus Albedo :4.8 Solis Lacus Albedo E :12.53 Solis Lacus Albedo E :5.22 Solis Lacus Albedo E :6.5 Solis Lacus Albedo
14 CTX Image ID# Latitude Longitude Crater Diameter (KM) Rampart Diameter (KM) Ratio Region B17_016379_1208_XN_59S322W E :56.5 Pityusa Rupes B16_015944_1222_XN_57S327W E :13.49 Pityusa Rupes B16_015944_1222_XN_57S032W E :19.68 Pityusa Rupes B02_010406_XI_61S332W E :35.3 Pityusa Rupes P04_002508_1108_XI_69S330W :14.55 Pityusa Rupes G13_23223_1089_XI_71S329W E :6.05 Pityusa Rupes G13_23223_XI_1089_71S329W :6.77 Pityusa Rupes G13_23223_1089_71S329W E :1.495 Pityusa Rupes G13_23223_1089_71S329W E :5.43 Pityusa Rupes G13_23223_1089_71S329W E :5.25 Pityusa Rupes B04_011369_1110_XN_69S341W E :16.89 Pityusa Rupes
15 CTX Image ID # Latitude Longitude Crater Diameter (KM) Rampart Diameter (KM) Ratio Region P16_007399_1182_X N_61S307W E :34.3 Malea Patera B17_016379_1208_X N_59S322W P15_007004_1222_X N_57S323W P15_007004_1222_X N_57S323W G03_019438_1223_X N_57S318W G03_019491_1207_X N_59S325W P05_001782_1194_XI _60S314W P16_007399_1182_X N_61S307W E :58.2 Malea Patera E :41.8 Malea Patera E :9.71 Malea Patera E :44.4 Malea Patera E :22 Malea Patera E :13.85 Malea Patera :37.5 Malea Patera
16 Image ID# Latitude Longitude Crater Diameter (KM) Rampart Diameter (KM) Ratio Region V E :66 Chryse V E :65.7 Chryse V E :33.1 Chryse V E :15.1 Chryse V E :4.23 Chryse V E :9 Chryse V E :34 Chryse V E : 4.07 Chryse V E :16.97 Chryse V E :16.87 Chryse
17 V :6.46 Chryse V E :13.2 Chryse V E :15.1 Chryse V E : 24.4 Chryse V E : 26.6 Chryse V E : 29.5 Chryse V E : 11.3 Chryse V E : 15.8 Chryse V E :14.1 Chryse V E : 67.5 Chryse V : 13.2 Chryse
18 Region Latitude Longitude (E) VIS ID# Crater Diameter (KM) Rampart Diameter (KM) Ratio Utopia Utopia Utopia Utopia Utopia Utopia Utopia V : V : V : V : V : V : V : 26.8
19 Region Latitude Longitude VIS ID# Crater Rampart Ratio (E) Diameter (KM) Diameter (KM) Utopia Utopia Utopia Utopia Utopia Utopia Utopia V : V : V : V : V : V : V : 7.57
20 Region Latitude Longitude (E) VIS ID # Crater Diameter (KM) Rampart Diameter ( KM) Ratio Acidalia Acidalia Acidalia Acidalia Acidalia Acidalia Acidalia V : V : V : V : V : V : V : 5.9
21 Region Latitude Longitude (E) VIS ID# Crater Diameter (km) Rampart Diameter (km) Ratio Acidalia Acidalia Acidalia Acidalia Acidalia Acidalia Acidalia V : V : V : V : V : V : V :24.9
22 Crater Diameter (km) Rampart Diameter (km) Ra,o CTX image # La,tude Longitude Region B20_017399_2 459_XN_65N10 9W :13.7 Alba Mons P18_008116_2 474_XN_67N10 8W :5.9 Alba Mons B19_016925_2 431_XN_63N12 7W : 10.5 Alba Mons P18_008117_2 431_XN_63N13 3W :12.6 Alba Mons B16_015910_2 355_XN_55N13 5W :7.2 Alba Mons B21_017901_2 376_XN_57N13 4W :11.1 Alba Mons B20_017479_2 343_XI_54N13 1W :16.3 Alba Mons P16_00739_23 09_XN_50N125 W :16.2 Alba Mons
23 B19_016991_23 36_XN_53N127 W :7.9 Alba Mons B _23 28_XI_52N129 W :6.5 Alba Mons P15_006970_23 98_XN_59N133 W :14.5 Alba Mons B19_016854_24 27_XN_62N125 W :3.9 Alba Mons B19_016854_24 27_XN_62N125 W :1.7 Alba Mons B17_016292_23 14_XN_51N123 W :9.9 Alba Mons B20_017307_23 69_XI_56N115 W :11.1 Alba Mons B20_017307_23 69_XI_56N115 W :5.1 Alba Mons B16_015883_23 41_54N117W :8.3 Alba Mons
24 B20_01749_24 10_XN_61N101 W :22.6 Alba Mons P19_008511_2 443_XI_64N09 2W` :1.4 Alba Mons P21_009091_2 420_XN_62N09 0W :9.1 Alba Mons P21_009091_2 420_XN_62N09 0W :7.8 Alba Mons B16_015922_2 386_XN_ 58N103W :19 Alba Mons B18_016832_2 356_XN_55N10 6W :11.6 Alba Mons B19_016977_2 393_XN_59N10 6W :11.7 Alba Mons B19_016977_2 393_XN_59N10 6W :4.9 Alba mons
25 CTX Image ID # Longitude Latitude Crater Diameter (km) Rampart Diameter (km) Ratio Region B16_016006_2298_XI_49N235W E N :20 Utopia B17_016178_2254_XN_45N249W E 44.37N :14 Utopia P15_006882_2241_XN_44N248W E E :3.7 Utopia B03_010666_2263_XN_46N_246W E N :15.7 Utopia B17_016191_2286_XN_48N245W E N :24.5 Utopia B19_017206_2290_XN_49N236W E N :20 Utopia B19_017008_2350_XI_55N237W E N :19.1 Utopia B19_017008_2350_XI_55N237W E N :20.1 Utopia B19_017008_2350_XI_55N237W E N :15.1 Utopia P15_006842_2310_XN_51N236W E N :10.9 Utopia
26 G01_018749_2369_ XN_56N243W B20_017338_2283_ XN_48N241W P15_007027_2319_ XN_51N247W P16_007238_2331_ XN_53N249W B16_015901_2285_ XN_48N248W B18_016758_XN _47N244W B18_016837_2289_ XN_48N241W B20_017338_2283_ XN_48N241W B19_016969_2363_ XI_56N247W B20_017246_2366_ XI_56N249W E N :14.2 Utopia E N :62 Utopia E N :60 Utopia E N :17.5 Utopia E N :19.9 Utopia E N :38 Utopia E N :33.7 Utopia E 48.94N :63 Utopia E N :16 Utopia E N :17.6 Utopia
27 PLOTS ON MOLA MAP Utopia Alba Mons Acadilia Chryse Solis Lacus Albedo Pityusa Rupes Malea Patera
28 1. Download Jmars on your computer 2. Go to Google and type in Jmars and click enter 3. When the results come up, click on the first link PROCEDURES 4. Scroll down the page and find the box that says JMARS Public Downloads and click on JMARS crossplatform WebStart installer 5. When link is clicked, a pop up window will come up, click on RUN to download Jmars. 6. Let Jmars download, this usually takes about 5 minutes to download. 7. When the download is complete, another pop up window will come up asking for a username and password, ignore that and click OK 8. Once you ve clicked OK Jmars is done downloading and a Layer Manager and a view of Mars will come up in 2 separate windows. 9. To find the region Solis Lacus Albedo go to New Layer on the Layer Manager window, scroll down and click on Nomenclature 10. At the top of the Layer Manager, click on the Nomenclature Tab. 11. Go to the Selected Landmark Types list and click the first landmark type Albedo. 12. Go to Navigation and on the Landmark list, scroll down and click on Solis Lacus. 13. Once the region if found click on Goto on the bottom of the window. 14. Now, Solis Lacus Albedo will be in your view, go to the Main tab and go to New Layer, Stamps, and click on Projected CTX Stamps 15. A window will pop up and click on Set Lon/Lat to bounds of MainView then click on OK
29 PROCEDURES CONTINUED 16. When clicked OK, the CTX stamps will come up and will look like long, blue rectangles. 17. In the images, find one that has a rampart crater in it. 18. Once an image is found, click on it, the blue box will be yellow now, and right click, scroll down to Render Selected Projected _CTX Stamps and click on Render Selected as PROJECTED_CTX 19. The image will now look realistic and to zoom in on the image, right click and click on Zoom & recenter and choose how far to zoom in. 20. On Layer Manager go to New Layer Mas by Instrument Mola MOLA 128ppd Elevation and click on Plot Numeric Data. 21. This layer allows you to measure the crater diameter and rampart diameter, to do this go to 1 rim and click, go across the middle to the other rim and DOUBLE CLICK. At the bottom of the screen, it will tell you how long the diameter is in KM, write the crater diameter in the data table. 22. To measure the rampart diameter, go from the edge of the ejecta, click and go across the middle to the other end of the ejecta and DOUBLE CLICK. Write the rampart diameter in the data table. 23. To find the ratio of the crater and rampart diameters, reduce if possible, and put the rampart diameter first, then the colon, and then the crater diameter. 24. Now put the image ID#, latitude, longitude, and region into the data table. 25. Repeat steps until images are found. 26. Go back to Nomenclature tab and change region to Chryse. 27. On CTX layer, delete that, and go to New Layer Stamps and click on Themis 28. A pop up window will come up like the CTX Stamps, and click on Set Lat/Lon to bounds of MainView and click OK 29. Repeat steps with new region and stamp.
30 PROCEDURES CONTINUED 30. Once all images are found in Chryse, go back to Nomenclature tab, and find Utopia. 31. Delete the Themis Stamp for Chryse and create a new Themis stamp for Utopia. 32. Repeat steps Delete the Themis stamp and make a new stamp for Utopia using the CTX stamps. 34. Repeat steps Now, go back to the Nomenclature tab and find the region Pityusa Rupes. 36. Delete the CTX stamp for Utopia, and set up a CTX stamp for Pityusa Rupes. 37. Repeat steps Once done in Pityusa, go to Nomenclature and find Malea Patera 39. Delete CTX stamp for Pityusa, and create a new CTX stamp for Malea. 40. Repeat steps When done with Malea Patera, go back to Nomenclature and find Acidalia. 42. Delete the CTX stamp in Malea, and set up a Themis stamp for the new region 43. Repeat steps Once finished in Acidalia, go to Nomenclature and find Alba Mons. 45. Delete the Themis stamp in Acidalia and create a CTX stamp in Alba Mons/
31 GEOGRAPHIC REGIONS Utopia Alba Mons Chryse Acidalia Solis Lacus Albedo Pityusa Rupes Malea Patera
32 LAYERS AND WEBSITES Nomenclature- Used to locate regions. CTX Stamps- Used to find rampart craters in Solis Lacus, Alba, Utopia, Pityusa, and Malea. THEMIS Stamps- Used to find rampart craters in Chryse and in Acidalia. MOLA 128ppd Elevation- This later was used to measure the crater and rampart diameters. Crater Counting Layer- Used to show where all images were found. MOLA Shaded Relief/Colorized Elevation-This layer was used to show the elevation differences between the 7 regions. Lat/Long Grid- This layer was used to find precise locations when images were found. Mola Shaded Relief (NE)- This layer showed the view Mars. HEND Epithermal (counts/second)- This layer allowed us to see where water was located on Mars. Mars on Earth.org- This website was used to compare rampart craters on Mars and on Earth. Jmars.com- This website was used to find the control image and used to find the geographic image. Mendeley.com- Used to find scientific research for presentation.
33 LAYER LIMITATIONS Nomenclature- This layer was good to use to find the regions, but when zoomed in to far, Mars is blurry and no images cannot be found. CTX Stamps- These stamps were great to use, but the images were long and there were a lot of repeat images found. THEMIS Stamps- This layer had a lot of images found within regions and poor image quality in the southern part of Mars. MOLA 128ppd Elevation- Good to measure the features, but if zoomed to far in the image, measuring was not accurate. Crater Counting Layer- Helpful, but can t do much with it but show were all images were found. MOLA Shaded Relief/Colorized Elevation- Doesn t show raised or sunken features and shadows, only elevation. Lat/Long Grid- Hard to get an exact lat/long points. Mola Shaded Relief (NE)- Doesn t give the realistic image of Mars and when zoomed in to far, the view of Mars is blurry and hard to find exact images. HEND Epithermal (counts/second)- This layer was very blurry and it s hard to see anything.
34 IMAGES We used 50 Themis images and 87 CTX images. Giving us a total of 137 images used. The data and images obtained is substantial enough to support our hypothesis and scientific question.
35 We are going to measure: MEASUREMENTS Crater diameter using the layer MOLA elevation 128ppd in JMARS by clicking one side of the crater rim with a yellow line and continuing it across the crater diameter to the other side s rim and double click to turn the yellow line red. The measurement is then displayed at the bottom of the screen in kilometers. Rampart diameter also using the MOLA elevation 128ppd in JMARS, clicking one side of the rampart s rim with a yellow line continuing it across the rampart diameter all the way to the other side of the rampart s rim and double click turning the yellow line red. The measurement is shown at the bottom of the screen in kilometers.
36 MEASUREMENTS Red line: measurement of the rampart diameter Yellow line: measurements of the crater diameter.
37
38
39
40
41
42
43 Solis Lacus Albedo: Correlation: Slope: 3.32 Chryse : Correlation: Slope : 1.37 Pityusa Rupes: Correlation: Slope: 2.09 Malea Patera: Correlation: Slope: 3.14 GRAPHICAL DATA Acidalia : Correlation: Slope: 1.38 Utopia : Correlation: Slope: 1.37 Alba Mons: Correlation: Slope: 3.26 Utopia : Correlation: Slope: 2.31
44 PLOTS ON MOLA MAP Utopia Alba Mons Acadilia Chryse Solis Lacus Albedo Pityusa Rupes Malea Patera
45 GRS/HEND EPITHERMAL Utopia Alba Mons Acidalia Chryse Solis Lacus Albedo Pityusa Rupes Malea Patera
46 Solis Lacus Albedo: 3.32 Alba Mons: 3.26 Malea Patera: 3.14 Utopia : 2.31 Pityusa Rupes: 2.09 Acidalia : 1.38 Chryse : 1.37 Utopia : 1.37 RESULTS
47 CONCLUSION Restated question: How can crater diameter and rampart diameter ratios of rampart craters be used to find different amounts of ice present in the Northern and Southern parts of Mars? Restated Hypothesis: Rampart Crater ratios will be larger in the Northern part of Mars. Restated importance: It is important to find ice if the idea of humans on Mars would ever become a possibility.
48 REFERENCES Jmars Images: Christensen, Philip R., E. Engle, S. Anwar, S. Dickenshied, D. Noss, N. Gorelick, and M. Weiss-Malik. "JMARS - A Planetary GIS." Jmars.asu.edu. Mars Space Flight Facility, Arizona State University, Dec Web. 26 Mar <Mars Space Flight Facility, Arizona State University>. PowerPoint Images: Lee, Pascal. Digital image. Marsonearth.org. SETI Institute, Mars Institute, Canadian Space Agency, NASA, Web. 28 Mar < Scientific research: Reiss D., S. Gasselt, E. Hauber, G. Michael, R. Jaumann, and G. Neukum. "Ages of Rampart Craters in Equatorial Regions on Mars: Implications for the past and Present Distribution of Ground Ice." Medeley (2006): Web. 29 Mar <
49 REFERENCES CONTINUED Themis: Christensen, P.R., N.S. Gorelick, G.L. Mehall, and K.C. Murray, THEMIS Public Data Releases, Planetary Data System node, Arizona State University, < CTX: NASA/JPL/University of Arizona
Why is this ques0on important and interes0ng? Our ques-on is interes-ng because we want to see if wind veloci-es can vary around Alba Patera.
What is your science ques0on? Can wind streak ra-os be used to determine wind velocity differences in the eleva-on band of 2500-5000m around Alba Patera? Why is this ques0on important and interes0ng? Our
More informationQuestion. Which volcano on the Tharsis region of Mars is the youngest?
Question Which volcano on the Tharsis region of Mars is the youngest? Importance We believe that this question is important and interesting because we don t have any evidence of recent tectonic activity
More informationØ How does the length of the volcanic eruption effect the length of the collapsed lava tube?
Ø How does the length of the volcanic eruption effect the length of the collapsed lava tube? Ø Main: The bigger the volcanic eruption the bigger the collapsed lava tube. Ø Alt1: The bigger the volcanic
More informationMARS STUDENT IMAGING PROJECT FINAL REPORT ASU MARS EDUCATION PROGRAM Waubonsie Valley High School Period School Year
I. Introduction What is your science question? What effect do the polar ice caps have on craters in the rock strata? Why is this question important and interesting? This question is important for the following
More informationWhy. history. features. 1. Fractures. not as wide. the lowered. Graben refers to. complex. This. Mars index_0.html :07
I. Introduction What is your science question? What is the differencee in the depth, width and length of fractures associated with volcanic activity compared to fractures thatt are associated with tectonism
More informationEffect of Albedo Change on Martian Temperature
Effect of Albedo Change on Martian Temperature Upper Darby High School, Period 5 Introduction: Similar to Earth, Mars is experiencing a period of global warming. However, the causes for global warming
More informationMars for Earthlings. Purpose: Observe and rank potential Earth analogs for Mars planetary study.
LESSON 1: Introduction In Class Activity 1 Mars Analogs Purpose: Observe and rank potential Earth analogs for Mars planetary study. Earth Analogs 1. What do you think scientists mean by an earth analog
More information8 th Grade Earth Science Brookhaven Academy
8 th Grade Earth Science Brookhaven Academy Science Question What factors effect lava flows on Mars? Why is this question interesting and important? By studying lava flows on Mars the geology of Mars can
More informationIntroduction. Background
Introduction In introducing our research on mars we have asked the question: Is there a correlation between the width of an impact crater and the depth of that crater? This will lead to answering the question:
More informationMapping the Surface of Mars Prelab. 1. Explain in your own words what you think a "geologic history" for a planet or moon is?
Prelab 1. Explain in your own words what you think a "geologic history" for a planet or moon is? 2. Describe some of the major features seen on the Martian surface by various spacecraft missions over the
More informationAs you can see in the picture to the left, the dust devils on Mars are significantly larger than dust devils on Earth.
A Study of Wind Streak and Dust Devil Track Direction in Syrtis Major to Establish Consistent Wind Direction and Determine if This Changes by Season. Mars Student Imaging Project March 2011 Rim Country
More informationAre There Plate Tectonics on Mars? 5 th Grade Class of 2013 John Read Middle School Redding, CT 06896
Are There Plate Tectonics on Mars? 5 th Grade Class of 2013 John Read Middle School Redding, CT 06896 Introduction: Are there plate tectonics on Mars? Could plate tectonics explain the formation of Valles
More informationIntroduction. Background
Introduction Our question was What is the affect of the elevation of an area on the state of the crater found there?. This question is important because it shows us how the weather at each elevation affects
More informationGrading Summary: Question 1: 80 points. Question 2: 20 points. Total: 100 points
HOMEWORK #5 Mars & Mercury Due Friday, May 26 th IN CLASS Answers to the questions must be given in complete sentences (except where indicated), using correct grammar and spelling. Please be as brief and
More informationSt. John Bosco Mars Project Essay The question chosen for this project was, what is the relationship between crater
St. John Bosco Mars Project Essay 2012 The question chosen for this project was, what is the relationship between crater diameter and wind streak length. Two hypotheses were formulated to answer this question.
More informationMSIP Proposal 2013 Nebraska City Lourdes Central Catholic. Mrs. Falcone s 6 th Grade Science
MSIP Proposal 2013 Nebraska City Lourdes Central Catholic Mrs. Falcone s 6 th Grade Science INTRODUCTION Our science question: Is more ice in older or new craters in the mid-latitudes? It is important
More informationName: Lab Instructor: Lab Section: GEO104: Planetary Geology LAB 10: MARS GEOLOGIC MAPPING
Name: Lab Instructor: Lab Section: GEO104: Planetary Geology LAB 10: MARS GEOLOGIC MAPPING OBJECTIVES: I. Apply our understanding of relative age dating and geologic processes to the Moon II. Develop an
More informationEleva&on vs. Wind Streaks
Eleva&on vs. Wind Streaks Scien&fic Ques&on Are wind streaks more common in higher or lower eleva&ons on the Southern Hemisphere of Mars? Why This Is Important o Answering this ques&on may help give us
More informationCliffsNotes.com. Stream Erosion. 18 Oct 2012 < ,articleId 9511.html>.
I. Introduction What is your science question? Is there a relationship between local base plateau elevation and depth, width, and length of channels within them? Why is this question important and interesting?
More informationThe Main Points. The View from the Surface. Geology of Mars. Lecture #20: Reading:
Surface of Mars Lecture #20: Geology and Geologic Processes View from the Surface History/Evolution of the surface Reading: Chapter 9.4 The Main Points Mars has had a geologically active past that has
More informationBrookhaven Academy. 8 th Grade Earth Science Final Report
Brookhaven Academy 8 th Grade Earth Science Final Report Introduction and Hypothesis: Science Question: What effect does elevation have on Martian lava flows? Our class was interested in conducting Earth
More informationMSIP Proposal Milks Period 4
part of Hebrus Vallis, V11030007, probably lava-formed (http://themis.asu.edu/zoom-20041203a) Tinjar Vallis, V11030007, maybe water-formed? ( http://themis.asu.edu/ zoom-20040519a) MSIP Proposal Milks
More informationMSIP PROPOSAL TEAM OMICRON
MSIP PROPOSAL TEAM OMICRON QUESTION: How much more destructive is the lava flow from Olympus Mons compared to a smaller volcano like Biblis Patera? Centennial High School Peoria, AZ Question: How much
More informationESCI 121 Physical Geology
Observing Streams & Rivers in Google Earth Dr. Jennifer L. Piatek Dept. of Physics and Earth Sciences Central Connecticut State University 506 Copernicus Hall 1615 Stanley Street New Britain, CT 06050
More informationLesson Plan 2 - Middle and High School Land Use and Land Cover Introduction. Understanding Land Use and Land Cover using Google Earth
Understanding Land Use and Land Cover using Google Earth Image an image is a representation of reality. It can be a sketch, a painting, a photograph, or some other graphic representation such as satellite
More informationMars for Earthlings. Purpose: Recognize the purpose and need for understanding the scale and context of various remote sensing imaging techniques.
LESSON 4: Remote Sensing Mars In-Class Activity 1 Scale and Context Purpose: Recognize the purpose and need for understanding the scale and context of various remote sensing imaging techniques. Study the
More informationIntroduction. width, and location of grabens and tension cracks. The question is important because the answer will show us the
Introduction The question which we based the experience off of was, what was the relationship between the depth, width, and location of grabens and tension cracks. The question is important because the
More informationQues%on: Are there spots on Mars where there are volcanoes and room for a rover to go and land? Importance: It is important to find places to land in
Ques%on: Are there spots on Mars where there are volcanoes and room for a rover to go and land? Importance: It is important to find places to land in order to find life on Mars. 1 st Hypothesis Ø Yes we
More informationAnalysis of Mars Color Camera (MCC) of Mars Orbiter Mission (MOM)
Analysis of Mars Color Camera (MCC) of Mars Orbiter Mission (MOM) Introduction: STRUCTURE About Mars Color Camera Part:1 Browsing of Mars Color Camera (MCC) data in Long Term Data Archive (LTA) Downloading
More informationMARS PUBLIC MAPPING PROJECT (MP)2
KWL Prior Knowledge/Engagement Activity In your small group, brainstorm ideas about what you think you know about geologic features that may be found on Mars. Also include what questions you have about
More informationBradley Central High School 4 th Hour Physics. Introduction:
Bradley Central High School 4 th Hour Physics Introduction: Our scientific question is, is there a connection between the location and size of a crater. Our underlying questions are, is there a correlation
More information1.2: Observing the Surfaces of Mars and Earth
GEOLOGY ON MARS Unit 1 - Chapter 1-2 Comparing Rocky Planets 1.2: Observing the Surfaces of Mars and Earth Log on to Amplify Geology on Mars Chapter 1.2 In a moment, you will watch a video made by other
More informationMars Possible Supervolcanoes
Mars Possible Supervolcanoes By: 5 th Grade GATE Walter Bracken STEAM Academy Supervised by Ms. Sekovski June 2013 Introduction The science question that was researched is, Are volcanic features, such
More informationTHE NEW GEOLOGY OF MARS: TOP TEN RESULTS OF POST-VIKING GLOBAL MAPPING AND CRATER-DATING
THE NEW GEOLOGY OF MARS: TOP TEN RESULTS OF POST-VIKING GLOBAL MAPPING AND CRATER-DATING K.L. Tanaka 1, J.A. Skinner, Jr. 1, C.M. Fortezzo 1, T.M. Hare 1, R.P. Irwin 2, T. Platz 3, G. Michael 3, J.M. Dohm
More informationI. Introduction: II. Background:
I. Introduction: Is there a difference between the size of the crater and the ejecta blanket? This question could lead to many different discoveries. When you think about the thousands of craters on mars,
More informationMAPPING THE SURFACE OF MARS
MAPPING THE SURFACE OF MARS What will you learn in this lab? How can we determine the geologic history of a planet or satellite without travelling to the planetary body? In this lab you will create a simple
More informationEOS 102: Dynamic Oceans Exercise 1: Navigating Planet Earth
EOS 102: Dynamic Oceans Exercise 1: Navigating Planet Earth YOU MUST READ THROUGH THIS CAREFULLY! This exercise is designed to familiarize yourself with Google Earth and some of its basic functions while
More informationRonald Wilhelm & Jennifer Wilhelm, University of Kentucky Ages on Mars. Martian Surface Age Exploration
Ronald Wilhelm & Jennifer Wilhelm, University of Kentucky 2008 Ages on Mars Martian Surface Age Exploration You have now learned some very important things about various planets and moons in our Solar
More informationHighs and Lows Floods and Flows
Highs and Lows Floods and Flows Planetary Mapping Facilitator Guide Becky Nelson Education Specialist The Lunar and Planetary Institute Highs and Lows, Floods and Flows Planetary Mapping Overview In this
More informationHighs and Lows, Floods and Flows PLANETARY MAPPING
Highs and Lows, Floods and Flows PLANETARY MAPPING OVERVIEW Teams of students become familiar with the topography of Mars, its geologic features, and patterns of features using a color-coded topographic
More informationKingswood 5 th Grade MSIP Final Project. Is it Possible to Predict Dust Storms Based on Sand Patterns?
Kingswood 5 th Grade MSIP Final Project Is it Possible to Predict Dust Storms Based on Sand Patterns? Science Question Is it Possible to Predict Dust Storms Based on Sand Patterns? We were interested in
More informationCHANNELS ON MARS. KWL Prior Knowledge/Engagement Activity
CHANNELS ON MARS KWL Prior Knowledge/Engagement Activity In your small group, brainstorm ideas about what you think you know about channels and what questions you have about channels on Mars. You will
More informationGIS: Introductory Guide to MapPlace. Workshop Agenda. How the Maps Work. Geographic Information Systems. -The MapPlace is a web GIS application
1 Introductory Guide to MapPlace Workshop 2007 Larry Jones MapPlace & Geoscience Databases Pat Desjardins Corporate GIS Gib McArthur Manager, Resource Information Kirk Hancock MINFILE Geologist Ward Kilby
More informationMSIP Final Report. Chabad Hebrew Academy Science Seminar Class
MSIP Final Report Chabad Hebrew Academy Science Seminar Class Introduction: 1. Updated scientific question: Will Sand Geysers erupt in the same region and same time in different years? 2. Why is this important?
More informationUNIVERSITY OF MARYLAND ASTRONOMY DEPARTMENT. Mars Cratering. Crater count isochrons of Arsia and Pavonis Mons
UNIVERSITY OF MARYLAND ASTRONOMY DEPARTMENT Mars Cratering Crater count isochrons of Arsia and Pavonis Mons Paul Hearding and Ben McIlwain 5/21/2007 Imagery of Arsia and Pavonis Mons taken by Mars Global
More informationLava Tubes. Camden Fairview High School NASA Lunar Research Team March 29, 2012
Lava Tubes Camden Fairview High School NASA Lunar Research Team March 29, 2012 Lava Tubes Lava Tubes on Earth are formed when lava flowing out from volcanic activity cools and hardens to make tube like
More informationMAPPING MARS TEACHER PAGE
TEACHER PAGE Background Information This lesson introduces students to some common map projections and representations (e.g., globes or close-ups) and asks them to consider the ways that each representation
More informationExercise 6: Coordinate Systems
Exercise 6: Coordinate Systems This exercise will teach you the fundamentals of Coordinate Systems within QGIS. In this exercise you will learn: How to determine the coordinate system of a layer How the
More informationMars locations overview latitude longitude
VHEC Onelight.com Publishing 2011 Mars Session, Preparation for Teleportation to Mars I believe at this time there are humans from surface Earth which are on Mars, who have been on Mars for some time.
More informationCatchment Delineation Workflow
Catchment Delineation Workflow Slide 1 Given is a GPS point (Lat./Long.) for an outlet location. The outlet could be a proposed Dam site, a storm water drainage culvert on a rural highway, or any other
More informationChanges in Seasonal Albedo with Land Cover Class
Name: Date: Changes in Seasonal Albedo with Land Cover Class Guiding question: How does albedo change over the seasons in different land cover classes? Introduction. Now that you have completed the Introduction
More informationInvestigating Weather and Climate with Google Earth Teacher Guide
Google Earth Weather and Climate Teacher Guide In this activity, students will use Google Earth to explore global temperature changes. They will: 1. Use Google Earth to determine how the temperature of
More informationSUPPLEMENTARY INFORMATION
SUPPLEMENTARY INFORMATION Supplementary Materials for Ancient ocean on Mars supported by global distribution of deltas and valleys Gaetano Di Achille 1* & Brian M. Hynek 1,2 1 Laboratory for Atmospheric
More informationWindNinja Tutorial 3: Point Initialization
WindNinja Tutorial 3: Point Initialization 6/27/2018 Introduction Welcome to WindNinja Tutorial 3: Point Initialization. This tutorial will step you through the process of downloading weather station data
More informationCratering and the Martian Surface
Lab 4 Cratering and the Martian Surface 4.1 Overview Exercise four continues our study of terrestrial surface evolution, shifting from the Moon to Mars and exploiting an extensive reservoir of recent high-resolution
More informationIntroduction to Google Earth
Introduction to Google Earth Name Goals 1. To become proficient at using the basic features of Google Earth. 2. To recognize differences in coastal features between the east and west coast of North America.
More informationMars Exploration Script
Mars Exploration Script By Michael Hardegree-Ullman 8/14/15 Revised: 8/12/16 Script Bulletpoints Sphere Flatscreens/ Mars has been known as a planet for thousands of years. The first records come from
More informationDavid Baxter. GK-12 Summer Research Program Brown University Oliver Hazard Perry Middle School NASA Explorer School
David Baxter GK-12 Summer Research Program Brown University Oliver Hazard Perry Middle School NASA Explorer School Department of Geological Sciences Planetary Geology Group Dr. Michael Wyatt Dr. James
More informationMars Opposition Friday 27 th July 2018
Mars Opposition Friday 27 th July 2018 Mars is about 6,780 kilometres in diameter or roughly half the size of the Earth whose diameter is 12,742km. As they orbit the Sun, the minimum distance between the
More informationLecture Outlines. Chapter 10. Astronomy Today 8th Edition Chaisson/McMillan Pearson Education, Inc.
Lecture Outlines Chapter 10 Astronomy Today 8th Edition Chaisson/McMillan Chapter 10 Mars Units of Chapter 10 10.1 Orbital Properties 10.2 Physical Properties 10.3 Long-Distance Observations of Mars 10.4
More informationGeologic Features of Mars
Name Purpose Geologic Features of Mars To learn to identify landforms on the surface of Mars and the geological processes that produced them. Introduction In many ways, Mars is similar to Earth. The same
More informationPhysics Lab #5: Starry Night Observations of the Sun and Moon
Physics 10293 Lab #5: Starry Night Observations of the Sun and Moon Introduction Today, we are going to use the Starry Night software to learn about motion of the stars, sun and moon on the celestial sphere.
More informationActivity #1 - Getting Started in Mars Exploration
Materials Activity #1 - Getting Started in Mars Exploration Paper, staples, glue, tape, markers, a collection of Mars images, etc., to construct a journal Preparation Collect newspaper or magazine articles
More informationSignature: Name: Banner ID#:
1 GEOLOGICAL SCIENCES 0050 I am aware of the Brown University Honor Code [see the Student Handbook, which can be accessed through the Geo0050 web site], understand that this exercise falls under that code,
More informationCHARTING THE HEAVENS USING A VIRTUAL PLANETARIUM
Name Partner(s) Section Date CHARTING THE HEAVENS USING A VIRTUAL PLANETARIUM You have had the opportunity to look at two different tools to display the night sky, the celestial sphere and the star chart.
More informationI m p a c t C r a t e r s o n M a r s
Asteroids, Comets and NEOs I m p a c t C r a t e r s o n M a r s Impact Craters on Mars Author: Sarah Roberts Asteroids, Comets and NEOs - Impact craters on Mars Introduction In this activity, Google Mars
More informationExploring Mars in Three Dimensions:
Exploring Mars in Three Dimensions: Classroom Activities and Lessons on Mars Exploration by David V. Black Walden School of Liberal Arts, 2011 elementsunearthed@gmail.com http://elementsunearthed.com/downloads
More informationPhysics Lab #3:! Starry Night! Observations of the Sun and Moon!
Physics 10293 Lab #3: Starry Night Observations of the Sun and Moon Introduction Today, we are going to use the Starry Night software to learn about motion of the stars, sun and moon on the celestial sphere.
More informationPROJECTIONS AND COORDINATES EXPLORED THROUGH GOOGLE EARTH EXERCISE (SOLUTION SHEET)
PROJECTIONS AND COORDINATES EXPLORED THROUGH GOOGLE EARTH EXERCISE (SOLUTION SHEET) Name: Date: Period: Note: Correct answers on some problems are indicated with a yellow highlight. PROJECTIONS 1. Here
More informationType of Exercise: In-Class Activity or Laboratory Exercise.
Using Lava Flows & Volcanic Structures on Mars to Introduce the Concept of Relative Dating in Introductory Courses Audeliz Matias Skidmore College, Saratoga Springs, NY 12866 amatias@skidmore.edu Type
More informationEXERCISE 2 (16 POINTS): LUNAR EVOLUTION & APOLLO EXPLORATION
1 GEOLOGICAL SCIENCES 0050 I am aware of the Brown University Honor Code [see the Student Handbook, which can be accessed through the Geo0050 web site], understand that this exercise falls under that code,
More informationMars: The Red Planet. Roman God of war Blood Reflects 30% of its incident sunlight 2 small moons : Phobos and Deimos
Mars: The Red Planet Roman God of war Blood Reflects 30% of its incident sunlight 2 small moons : Phobos and Deimos Property Earth Mars Radius 6378km 3394km ~ 0.51R E Mass 5.97x10 24 kg 6.42x10 23 kg =
More informationAutomated Identification and Characterization of Landforms on Mars
Automated Identification and Characterization of Landforms on Mars Tomasz F. Stepinski Lunar and Planetary Institute Collaborators: Wei Luo Students: Brain Bue Ian Molloy Erik Urbach Michael Mendenhall
More informationQuestion Moon An Introduction to the Process of Science
Question Moon An Introduction to the Process of Science Generating Research Ideas Student Guide Question Moon An Introduction to the Process of Science Student Guide Lunar Student Imaging Project (LSIP)
More informationInitial Observations and Strategies
STUDENT WORKSHEET 1 Initial Observations and Strategies Name(s) Date Look at the Thermal Emission Imaging System (THEMIS) Daytime Infrared (IR) image mosaic your teacher has given you. You will be investigating
More informationMARS, THE RED PLANET.
ENGLISH ENTRY TEST, FEB 2013. STUDENT S NAME.... READ THE TEXT CAREFULLY, CHECK THE VOCABULARY AND THEN DO THE ACTIVITIES. MARS, THE RED PLANET. It is easy to forget that Earth is not the only planet in
More informationModule 7, Lesson 1 Water world
Module 7, Lesson 1 Water world Imagine that the year is 2100. Scientists have determined that the rapidly warming climate of the earth will cause the ice sheets of Antarctica to break apart and melt at
More informationPSRD: Did Martian Meteorites Come From These Sources?
1 of 7 posted January xx, 2007 Did Martian Meteorites Come From These Sources? --- Researchers find large rayed craters on Mars and consider the reasons why they may be launching sites of Martian meteorites.
More informationESCI 110: Planetary Surfaces Page 3-1. Exercise 3. Surfaces of the Planets and Moons
ESCI 110: Planetary Surfaces Page 3-1 Introduction Exercise 3 Surfaces of the Planets and Moons Our knowledge of the solar system has exploded with the space exploration programs of the last 40 years.
More informationOutflow Channels May Make a Case for a Bygone Ocean on Mars Written by Linda M.V. Martel Hawai'i Institute of Geophysics and Planetology
1 of 5 posted June 14, 2001 Outflow Channels May Make a Case for a Bygone Ocean on Mars Written by Linda M.V. Martel Hawai'i Institute of Geophysics and Planetology High-resolution elevation data from
More informationAncient Floodwaters and Seas on
1 of 9 posted July 16, 2003 Ancient Floodwaters and Seas on Mars --- Surface deposits within the northern lowlands support the oceans hypothesis. Written by Linda M. V. Martel Hawai'i Institute of Geophysics
More information1. Double-click the ArcMap icon on your computer s desktop. 2. When the ArcMap start-up dialog box appears, click An existing map and click OK.
Module 2, Lesson 1 The earth moves In this activity, you will observe worldwide patterns of seismic activity (earthquakes) and volcanic activity (volcanoes). You will analyze the relationships of those
More informationUsing Earthscope and B4 LiDAR data to analyze Southern California s active faults
Using Earthscope and B4 LiDAR data to analyze Southern California s active faults Exercise 8: Simple landscape morphometry and stream network delineation Introduction This exercise covers sample activities
More information39 Mars Ice: Intermediate and Distant Past. James W. Head Brown University Providence, RI
39 Mars Ice: Intermediate and Distant Past James W. Head Brown University Providence, RI james_head@brown.edu 37 Follow the Water on Mars: 1. Introduction: Current Environments and the Traditional View
More informationEXPLORING THE GEOLOGY OF SEVERAL WORLDS FROM SPACE
NAME DATE PARTNER(S) EXPLORING THE GEOLOGY OF SEVERAL WORLDS FROM SPACE We have investigated to understand how scientists can map the sea floor and land surfaces of the Earth. Now let=s extend our vision
More informationStudying Topography, Orographic Rainfall, and Ecosystems (STORE)
Introduction Studying Topography, Orographic Rainfall, and Ecosystems (STORE) Lesson: Using ArcGIS Explorer to Analyze the Connection between Topography, Tectonics, and Rainfall GIS-intensive Lesson This
More informationMoon 101. Bellaire High School Team: Rachel Fisher, Clint Wu, Omkar Joshi
Moon 101 Bellaire High School Team: Rachel Fisher, Clint Wu, Omkar Joshi Part I Formation of the Moon Planetary Formation In the solar nebula, dust particles coalesced to form smaller planetesimals and
More informationproviding 100-m per pixel resolution in nine ~1.0 µm wide infrared bands centered from
Supporting Text The THEMS instrument consists of separate infrared and visible imagers providing 100-m per pixel resolution in nine ~1.0 µm wide infrared bands centered from 6.78 to 14.88 µm, and 18-m
More informationOutline 9: Origin of the Earth: solids, liquids, and gases. The Early Archean Earth
Outline 9: Origin of the Earth: solids, liquids, and gases The Early Archean Earth Origin of Earth s Matter The earth is made of recycled elements formed in stars that existed prior to our Sun. Supernova
More informationGeomorphic and geologic settings of the Phoenix Lander mission landing site
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 114,, doi:10.1029/2009je003416, 2009 Geomorphic and geologic settings of the Phoenix Lander mission landing site T. L. Heet, 1 R. E. Arvidson, 1 S. C. Cull, 1 M. T.
More informationOutline 9: Origin of the Earth: solids, liquids, and gases
Outline 9: Origin of the Earth: solids, liquids, and gases The Early Archean Earth Origin of Earth s Matter The earth is made of recycled elements formed in stars that existed prior to our Sun. Supernova
More informationVENUS: DETAILED MAPPING OF MAXWELL MONTES REGION
VENUS: DETAILED MAPPING OF MAXWELL MONTES REGION Yu. N. Alexandrov, A. A. Crymov, V. A. Kotelnikov, G. M. Petrov, O. N. Rzhiga, A. I. Sidorenko, V. P. Sinilo, A. I. Zakharov, E. L. Akim, A. T. Basilevski,
More informationSea Ice and Satellites
Sea Ice and Satellites Overview: Students explore satellites: what they are, how they work, how they are used, and how to interpret satellite images of sea ice using Google Earth. (NOTE: This lesson may
More informationDust in the Atmosphere of Mars 2017 (LPI Contrib. No. 1966)
REGIONALITY OF DUST HAZE TRANSPORT IN THE MARS ATMOSPHERE REVEALED BY ENSEMBLE SIMULATIONS. K. Ogohara 1, 1 University of Shiga Prefecture (2500, Hassaka, Hikone, Shiga, Japan, ogohara.k@e.usp.ac.jp).
More informationCorrection to Localized gravity/topography admittance and correlation spectra on Mars: Implications for regional and global evolution
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 109,, doi:10.1029/2004je002286, 2004 Correction to Localized gravity/topography admittance and correlation spectra on Mars: Implications for regional and global evolution
More informationGIS in Water Resources. Fall Homework #1
GIS in Water Resources Fall 2015 Homework #1 Goal The goal of this homework is to reinforce the lecture material on Geodesy, Map Projections and Coordinate Systems by having you identify attributes and
More informationCreate A Watershed Profile
Name Date Follow the steps below with Chesapeake Bay FieldScope to create a watershed profile for your location. Part 1. Take a trip down your tributaries. Create A Watershed Profile 1. Find your field
More informationDesigning a Quilt with GIMP 2011
Planning your quilt and want to see what it will look like in the fabric you just got from your LQS? You don t need to purchase a super expensive program. Try this and the best part it s FREE!!! *** Please
More informationWe will apply two of these principles to features on the lunar surface in the following activities.
STUDENT ACTIVITY 4 Studying the Geologic Past Scientists who study the processes that shape the surface of Earth are called geologists. They have scientific rules, which help them figure out the history
More informationCOSMORPHOLOGY - May 2009
Name COSMORPHOLOGY - May 2009 Geologic landforms Purpose: By studying aerial photographs you will learn to identify different kinds of geologic features based on their different morphologies and learn
More information