By: Shane DePinto (NAU, Geophysics) Mentored by: Chris Okubo (USGS, Astrogeology) MAPPING APPARENT POROSITY OF SURFICIAL ROCKS DISCOVERED BY THE MARS EXPLORATION.

Slides:



Advertisements
Similar presentations
By Connor Hanna, Elliott Dwire 4 th Sharon Shannon Elementary school.
Advertisements

Space Exploration Mars Rovers, Apollo program, Voyager satellites, and SETI All Presented by the Peter C Period: 2 (two) As in 1+1=2 Or 2x1=2 ®
The Rock Cycle. Crust Mantle Outer Core Inner Core The Structure of the Earth.
Martian Craters with Interior Deposits: Global Survey Results and Wind Model P21D-1875 Kristen A. Bennett 1 and Mark Schmeeckle 2 1 School of Earth and.
Identifying Rocks Sedimentary rocks. Rocks are partly identified by origin: Igneous Sedimentary Metamorphic.
By Madison Bailey.  Igneous  Sedimentary  Metamorphic.
The Rock Cycle. Basics Continual process that breaks down, alters, and re-forms rock into one of three types Types of rock can be converted to other types.
Most commonly found in Sedimentary Rock. As time passes, more layers are dropped on top of old layers. This means newer fossils on top old fossils.
8.1 The Rock Cycle 7.4.a Students know Earth processes today are similar to those that occurred in the past and slow geologic processes have large cumulative.
Collecting and Mapping Planetary Data. Direct measurements (in situ) Collecting data directly at the site of scientific interest Ground stations on Earth.
Astronomy190 - Topics in Astronomy Astronomy and Astrobiology Lecture 15 : Ancient Mars Ty Robinson.
Sedimentary Magma Weathering/ Erosion Compaction/ Cementation Heat/ Pressure Metamorphic Melting Cooling Igneous Sediments.
Dane Henderson (NAU) Mentor: R. Greg Vaughan (USGS / NAU)
Warm-Up Did anyone ever have a rock collection? Where do you think these rocks came from? Do these rocks last forever?
Mars By Chelsea Hoyle. Mars Exploration Mars is mainly explored by rovers. The rovers are called Spirit, curiosity and Opportunity. They were put on mars.
Name of Planet You and Your Partner’s Names Period Provide a caption for each image. Ex: This is a compilation image showing the seasons on Saturn. The.
Igneous Rock Sedimentary Rock Metamorphic Rock Terms Grab Bag
UNIT 5: GEOLOGIC HISTORY. AT THE END OF THIS UNIT YOU WILL BE ABLE TO  Calculate the absolute age of a substance based on its decay rate  Correlate.
1 Earth’s History Planet Earth is approximately 4.6 billion years old –Rocks of the crust provide clues to Earth’s past By analyzing these clues we can.
Name of Planet You and Your Partner’s Names Provide a caption for each image. Ex: This is a compilation image showing the seasons on Saturn. The images.
Mars Exploration Rovers (MER) Entry, Descent, Landing, and Deployment.
Rock Formation Activity #19.
Name of Planet Keyon and Naimah Provide a caption for each image. Ex: This is a compilation image showing the seasons on Saturn. The images were taken.
Discussion of High Thermal Inertia Craters on Mars in the Isidis and Syrtis Major Regions Jordana Friedman Arizona State University.
Rocks and the Rock Cycle.  As we already learned, rocks are made from minerals and can be classified into 3 major families (or types) based on how they.
Earth’s History The Rock Cycle Complete on page 135.
W6 BY: Antonio, And Max Howenstine High School, Mr. Martin 6 th period class, 9 th grade, 4/20/07.
The Solar System a1 Mercury Sun Venus Earth Mars Asteroids Jupiter Saturn Uranus Neptune Other objects Observe our solar system Four inner planets.
Rocks: Mineral Mixtures
1 There’s lots of evidence for water on Mars…in the past River beds and teardrop-shaped “perched” craters. Lake beds Minerals have been found that only.
Topic 2: Rocks and The Rock Cycle  Rocks are classified into 3 major groups:  Igneous Rock  Sedimentary Rock  Metamorphic Rock.
By: J. Trent Pettus, Calynn Trent, and Morgan Mason MARS.
Interlude  Viking mission operations ended in the early 1980s  Viking missions gave scientists the most complete picture of Mars to date. What does this.
The Study of Earth’s Landforms. Where Do You Live? =
REGOLITH LANDFORM MAPPING OF MERIDIANI PLANUM AND SURROUNDS J. D. A. Clarke 1 C. F. Pain 2 and M. Thomas 1, 1 Australian Centre for Astrobiology, Macquarie.
Mars Science Laboratory 1st Landing Site Workshop Pasadena, CA — 31 May – 2 June Fine-layered Meridiani crater for the MSL Landing Site L. V. Posiolova,
Three Major Types of Rocks  Igneous  Sedimentary  Metamorphic.
Unit 4. A rock formed from layers of sediment or bits of broken rock joined together. Example: sandstone.
Jessica Kaminski Mentor Greg Mehall – Mars Space Flight Facility NASA Space Grant Symposium Arizona State University April 18, 2009.
Marjorie A. Chan Rich New Mars Exploration Rover Data: Earth to Mars Sol 727.
NAI Mars Focus Group Videocon Science and Landing Site Priorities for the Mars 2003 Mission Presentations by: n Ronald Greeley (ASU) & Ruslan Kuzmin (Vernadsky.
Brittany Grinner Paul Lim PATHFINDER & SOJOURNER.
Earth History Sandstone & Shale Formation. Basin An area of relative low elevation where water and sediments collect.
Three Types of Rock.
Workshop proposal to ISSI Quantifying the Martian Geochemical reservoirs.
Identifying Rocks Sedimentary rocks. Rocks are partly identified by origin: Origin-beginning Original.
World Wide Telescope 1 Web Search What is the climate of a place? How is this different from the weather? 2 Video Search/Thinking What month are.
Mineral Analysis of Martian Dunes
Rock Web Quest By: Katie Kartchner
Curiosity Mars Rover By:.
Topic: Sedimentary Rocks
Geology Spring 2015 – 8th Grade.
Chapter Menu Lesson 1: Relative Ages of Rocks
Rock Cycle.
Rocks And The Rock Cycle
Chapter Menu Lesson 1: Relative Ages of Rocks
Swarm Robotics in Space Exploration
This imaginative painting shows a possible future human settlement on ___________. Settlers might live in domes to protect themselves from the harsh climate.
Introduction To Earth and Space Science Mr. Lehman
Curious about Curiosity?
Rock Formation Activity #19.
Natural Sciences and Technology Grade 6
Geology Spring 2016 – 8th Grade.
Rock Cycle 1.
Mars-2005.
Table of Contents: Rocks Writing Prompt: Rocks, what are they?
Chapter 6 – Sedimentary and Metamorphic Rocks
Types of Rocks.
Lesson 64 Photocopy: Assignment Log Learning Objective Log
Presentation transcript:

By: Shane DePinto (NAU, Geophysics) Mentored by: Chris Okubo (USGS, Astrogeology) MAPPING APPARENT POROSITY OF SURFICIAL ROCKS DISCOVERED BY THE MARS EXPLORATION ROVERS

THE BIG PICTURE Research on Mars helps us to understand the geologic history and past habitability of the planet Understanding porosity of rocks on Mars provides insight into potential hydrologic conditions in the past and the mechanical strength of these crust materials

HOW WE DID IT… During the early part of its mission, the Mars Explorer Rover Opportunity (MERB) ground and brushed in situ rock samples (45mm x 5mm) to remove weathering effects and loose sediment Its Microscopic Imager (MI) was used to take series of photos of each sample I compiled a database of MI data over the sample sites using the MER Analyst Notebook (a public database) and prepared/analyzed them

MY DATA Mosaicked photos from each site together Overlaid transparent layers on top and then deleted all apparent pore space from surface Compared pixel data from unaltered overlay layer and altered overlay to calculate apparent visible porosity for each sample

EXAMPLE: SOL x magnification

ANALYSIS I analyzed a total of 7 samples The samples had apparent porosities ranging from 20.4%-59.61% The porosity values are a bit high compared to Earth sedimentary porosity values, which are typically less than 20% Porosities as high as 50% are not unheard of, especially in evaporite-rich sediments The Mars rocks I analyzed are evaporite-rich sandstone Turns out Martian rocks are similar to Earth’s

PROBLEMS THAT I FOUND They stopped doing it! Sometime between sol … Lighting is variable between photos and that makes analysis difficult Porosity is a 3-dimensional aspect and analyzing it from a 2-D perspective is not extremely accurate

CONCLUSIONS It appears as if Martian sedimentary rocks have a similar structure to Earth’s sedimentary rocks This means cool things! Engineering aspects possibly, and verification of some of our geologic principles

ACKNOWLEDGEMENTS Thanks to my Mentor Chris Okubo! You were extremely helpful in every stage of this project and helped me with all questions Thank you NASA Thanks NAU Thank you Space Grant Symposium Questions?