Mars: First Order Landscapes The Great Crustal Dichotomy

Slides:



Advertisements
Similar presentations
Mars: First Order Landscapes The Great Crustal Dichotomy
Advertisements

MARS TECTONICS & VOLCANOLOGY Zachary Gallegos University of New Mexico / Mars One.
The Mars Dichotomy Evidence for Plate Tectonics or Erosion?
C.M. Rodrigue, 2014 Geography, CSULB Mars: Third Order Landscapes Geography 441/541 S/14 Dr. Christine M. Rodrigue.
Oceans on Mars By Carr and Head Presented by Mark Popinchalk An assessment of the observational evidence and possible fate.
8th Grade Science Unit 8: Changes Over Time
Mercury: The Innermost Planet 23.2 The Terrestrial Planets  Mercury is the innermost and second smallest planet; it is hardly larger than Earth’s moon.
C.M. Rodrigue, 2007 Geography, CSULB Boldly Going Where No Geographer Has Gone Before: The Martian Classroom The Los Angeles Geographical Society (7 September.
C.M. Rodrigue, 2015 Geography, CSULB Mars: Nomenclature Geography 441/541 S/15 Dr. Christine M. Rodrigue.
Landform Regions of Canada
C.M. Rodrigue, 2007 Geography, CSULB Mars: Third Order Landscapes Geography S/07 Dr. Christine M. Rodrigue.
C.M. Rodrigue, 2007 Geography, CSULB Mars: Nomenclature Geography S/07 Dr. Christine M. Rodrigue.
5a Planetary Interiors. 5a Minerals 5a 5a Isostacy.
C.M. Rodrigue, 2007 Geography, CSULB Mars: Sources of Data from the Robotic Missions Geography S/07 Dr. Christine M. Rodrigue.
C.M. Rodrigue, 2007 Geography, CSULB Mars: First Order Landscapes Geography S/07 Dr. Christine M. Rodrigue.
Mars. Some similarities between Mars & Earth Mars’ Bulk Properties Mars has days & seasons like Earth.
C.M. Rodrigue, 2007 Geography, CSULB Mars: Second Order Landscapes Geography S/07 Dr. Christine M. Rodrigue.
C.M. Rodrigue, 2007 Geography, CSULB Mars: Fourth Order Landscapes Geography S/07 Dr. Christine M. Rodrigue.
C.M. Rodrigue, 2007 Geography, CSULB Mars: Sources of Data from the Robotic Missions IV Geography S/07 Dr. Christine M. Rodrigue.
Mars Basics. Size & Distance Smaller than Earth (0.532x) Mars diam ~ 6779 km (4212 miles) Earth diam ~ 12,742 km (7918 miles) 8 Mars would fit inside.
C.M. Rodrigue, 2015 Geography, CSULB Mars: Second Order Landscapes Geography 441/541 S/15 Dr. Christine M. Rodrigue.
Red Planet Mars Chapter Thirteen. Guiding Questions 1.When is it possible to see Mars in the night sky? 2.Why was it once thought that there are canals.
The Solar System.
NOTES: MARS 0.53 Diam(earth), -140 o C to 20 o C Atmosphere 95% CO2, 3% N2, 2% Ar 24 hr day, 25 o axial tilt like Earth 1. Small liquid core and magnetic.
Study of bound water in the surface layer of Mars Workshop HEND-2002 “The First year of HEND operations on the NASA Odyssey Mars Orbiter” May 20-22, 2002.
Bodies of Water Presentation created by Robert Martinez Primary Content Source: McDougal Little World Geography.
3 Sept 2003Solar System - C. C. Lang1. 3 Sept 2003Solar System - C. C. Lang2 Northerners have cold days in January because: (a) the earth is farthest.
C.M. Rodrigue, 2015 Geography, CSULB Mars: Sources of Data from the Robotic Missions Geography 441/541 S/15 Dr. Christine M. Rodrigue.
Observing Mars By Brad Jarvis. Overview Basic facts Orbits and distance Viewing Mars from Earth The view from space Current exploration Conclusion References.
C.M. Rodrigue, 2014 Geography, CSULB Mars: First Order Landscapes Geography 441/541 S/14 Dr. Christine M. Rodrigue.
C.M. Rodrigue, 2014 Geography, CSULB Mars: Fourth Order Landscapes Geography 441/541 S/14 Dr. Christine M. Rodrigue.
Latitudinal Trend of Roughness and Circumpolar Mantles on Mars M. A. Kreslavsky J. W. Head III Brown University.
Mars Monroe. Mons Olympus. Bigger than most states.
Chapter 10 Mars. Mars’s orbit is fairly eccentric which affects amount of sunlight reaching it 10.1 Orbital Properties.
C.M. Rodrigue, 2015 Geography, CSULB Geography on Mars: Third Order of Relief Los Angeles Geographical Society 6 March 2015 Dr. Christine M. Rodrigue Geography.
C.M. Rodrigue, 2014 Geography, CSULB Mars: Fourth Order Landscapes Geography 441/541 S/14 Dr. Christine M. Rodrigue.
Did Lava or Water Affect the Formation of Elysium Planitia?
Happy Halloween!. Homework #6 Due 6:00 pm today Exam #2 on Wednesday.
Background There are several theories that state that Martian sinkholes as the result of large evaporite deposits and erosion are impossible. The past.
C.M. Rodrigue, 2015 Geography, CSULB Mars: Climates Geography 441/541 S/15 Dr. Christine M. Rodrigue.
9. Canada – The Physical Background The Geological Evolution of Canada The Geological Evolution of Canada Physiographic Regions Physiographic Regions Meteorite.
Unit 11 Mars. Physical Properties Radius: 3400 km Moons: Deimos, Phobos Mass: 6.4 × kg Density: 3900 kg/m 3 Length of Day: 24.6 hours.
Mars Monroe. Retrograde Motion Apparent backwards motion, compared to background stars.
The Terrestrial Planets Chapter 23, Section 2. Mercury: The Innermost Planet  Mercury, the innermost and smallest planet (not counting Pluto), is hardly.
20.2. Continental Margins The line that divides the continental crust from the oceanic crust is not always obvious. Shorelines are not the true boundaries.
C.M. Rodrigue, 2007 Geography, CSULB Boldly Going Where No Geographer Has Gone Before: The Martian Classroom The Los Angeles Geographical Society (7 September.
C.M. Rodrigue, 2016 Geography, CSULB Mars: Second Order Landscapes Geography 441/541 S/16 Dr. Christine M. Rodrigue.
Surface Features of Mars. General Features Mars is a Desert World. Its surface is dominated by desert terrain dotted with Volcanoes and Craters. There.
Mars Mars is a dry dead world. There are no Martian transits.
Curiosity Curiosity pictures Rover view Old Rover View form older rover.
Mars.
ESCI 214: Mars: What and Where. (Survey of Major Geologic Features)
Moving water shapes land
Mars eccentricity = Mass = 0.11 MEarth
Surface Features Overview
Unit One Land And Water Forms
Orbital and Physical Properties
ESCI 214: Mars: How it all got there. (Overview of Martian Evolution)
ASTR/GEOL-2040: Search for life in the Universe: Lecture 21
MARS.
A Report in Natural Science I
Maps!!! Who doesn’t love a gorgeous map?
The Nature and Origin of Deposits in Uzboi Vallis
Check your knowledge--
Surface Features on Mars
Surface Features of Mars
Department of Geographic Information System and Remote Sensing
Surface Features of Mars
Walter S. Kiefer Lunar and Planetary Institute
Presentation transcript:

Mars: First Order Landscapes The Great Crustal Dichotomy Geography 441/541 S/18 Dr. Christine M. Rodrigue C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes On Earth, the orders of relief scheme Is sometimes seen in geography textbooks Organizes topographic variation in a scale-dependent manner Geographers often focus on Spatial analysis of particular phenomena Regional synthesis to integrate assemblages of phenomena Scales at which processes and regional patterns operate The interactions among phenomena at different scales C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Examples of interactions among scales In spatial statistics: the Modifiable Areal Unit Problem (MAUP) In human geography: local cultural and political responses to global economic and political processes Biogeography: alpha, beta, and gamma measures of biodiversity Geomorphology: "megageomorphology" has emerged as remote sensing technology has made the simultaneous examination of form and process at large scale (small map scale) possible C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes For Mars, a handy descriptive scheme for handling the regional variations in Mars’ physical landscapes The “First Order of Relief” = the crustal dichotomy The Northern Lowlands The Southern Highlands If Earth’s oceans evaporated (which they will …), there would remain a crustal dichotomy here Former ocean basins: low elevation, thin crust, basaltic, with a veneer of pelagic sediments Former continents: high elevation, thick crust, granitic rocks and their extrusive igneous, sedimentary, and metamorphic derivatives C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Northern Lowlands Regional subdivisions: Vastitas Borealis Utopia Planitia Embayments: Acidalia Planitia Chryse Planitia Amazonis Planitia Arcadia Planitia Isidis Planitia Elysium Planitia Mars: First Order Landscapes C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Northern Lowlands Relatively young surface Smooth with few craters This is exactly what you’d expect if Mars had had an ocean It could be expected to receive sediments from rivers, floods, and coastal processes and create terrigenous sediments nearshore, with some of them dissolving They would be turned into minerals that would eventually precipitate out of the water column onto the abyssal floor The oceans would thus cover the underlying original rock surface, much as pelagic sediments here do C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Northern Lowlands Further suggestions of an ocean: Drainage of Martian outflow channels and valley networks This is also exactly what you’d expect if Mars had had an ocean to serve as base level for stream networks C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Northern Lowlands Drainage: Valles Marineris' outflow channels, which drain into Chryse Planitia Nanedis north of Ganges Ares and Aram Chaos Argyre to Aram and Ares C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Northern Lowlands Even better: Coastlines!? Transition between the southern highlands and the northern lowlands is quite abrupt C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Northern Lowlands Even better: Coastlines!? Terraces on the Arcadia side of Alba Mons C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Vastitas Borealis Even better: Coastlines!? Tim Parker’s analysis of Viking imagery C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Northern Lowlands Even better: Coastlines!? Tim Parker’s analysis of Viking imagery (1994) His and others’ re-analysis using MOC imagery seemed to debunk his argument, which even he admitted in 2001 But it’s as though the new imagery is so fine in resolution that it can’t detect the coarser scale at which this putative ocean’s coastline features might exist MOLA suggests that, in fact, at least one of the “coastlines” is at the same elevation (water seeks a level constant with respect to the geoid) C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Northern Lowlands Plot complication That "ocean" floor is dominated by andesitic rock (on Earth, it's basalt) Not sediments with minerologies consistent with precipitation out of water. No carbonates! No ocean? C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Northern Lowlands About those andesites "Surface Type 1" (basalts dominating the southern highlands) "Surface Type 2" (andesites and andesitic basalts dominating the northern lowlands) C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Northern Lowlands Rampart craters C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Northern Lowlands Patterned ground C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Northern Lowlands Thumbprint terrain Rootless cones C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Northern Lowlands Dunes C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes The Southern Highlands Mostly 1-5 km above the mean martian geoid Versus 0-3 km below for the Northern Lowlands ~1-3 km scarp dividing the two C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Southern Highlands: Ancient, battered terrain Arabia Terra C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Southern Highlands: Ancient, battered terrain Thaumasia Highlands: snow-fed channels? C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Southern Highlands: Ancient, battered terrain Noachis Terra to right Amenthes Planum below Signs of water or fluid C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Southern Highlands: Ancient, battered terrain Hellas, with Isidis and Utopia from the Northern Lowlands beyond C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Southern Highlands: Ancient, battered terrain Noachis Terra, Holden Crater, alluvial fan/bajada? (right) Delta, too, from Uzboi Vallis entering from southwest (left) C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Southern Highlands: Ancient, battered terrain Syrtis Major Planum, volcanic province, basaltic, not dusty C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Southern Highlands: Ancient, battered terrain Dust devil track Promethei Terra on left Syrtis Major on right C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Southern Highlands: Ancient, battered terrain Terrain softening at higher latitudes Cimmeria Terra to left Noachis Terra to right C.M. Rodrigue, 2018 Geography, CSULB

Mars: First Order Landscapes The “Orders of Relief” for Martian Landscapes Basalt terrain and dust dominate the Southern Highlands while andesite is quite prevalent in the Northern Lowlands Spectra showing high proportions of basalt shown in the green Andesite shown in the red channel Hæmatite shown in blue (small area) Dust-dominated areas come out brown C.M. Rodrigue, 2018 Geography, CSULB