Holden NE crater Main Goals:

Slides:



Advertisements
Similar presentations
Structural Analysis Lecture 10 SLIDE 1
Advertisements

Relative Dating : Which Came First?
Geology of the Thaumasia region, Mars: plateau development, valley origins, and magmatic evolution by James M. Dohm, Kenneth L. Tanaka.
AQUEOUS SEDIMENTARY DEPOSITS IN HOLDEN CRATER: LANDING SITE FOR THE MARS SCIENCE LABORATORY Rossman P. Irwin III and John A. Grant Smithsonian Institution,
Surface Magnetization of Terra Meridiani, Mars Renee French Earth 438 Winter 2014 Opportunity looking out on Santa Maria Crater, sol 2466 (~7 years)
Structural Geology Crustal Deformation
Ch 15 (Part I): Crustal deformation
Prentice Hall EARTH SCIENCE
_____/5 “logistics” Title, scale (bar and ratio), author, date, N arrow, explanation (rock units (oldest at the bottom) with symbols and ages, strike and.
Geological history exercise Using seismic to deduce the geological history of an area.
GEOLOGIC STRUCTURES.
Evolution and Change Chapter Fourteen: Earth and Life History 14.1 Evidence from Rocks 14.2 How Earth Changes 14.3 Natural Selection.
Holden Stratal Geometries & Depositional Hypotheses Dawn Sumner, Gilles Dromart, Ralph Milliken, Ken Edgett, Mike Malin (by way of Ken) with input from.
Latitudinal Trend of Roughness and Circumpolar Mantles on Mars M. A. Kreslavsky J. W. Head III Brown University.
Mars Student Imaging Program The Three Principles Impact Craters Features you must know and understand. Ejecta – Material, from the crater, that was thrown.
Planetary image interpretation and mapping Phil Stooke USGS map I-515.
Mars Science Laboratory 1st Landing Site Workshop Pasadena, CA — 31 May – 2 June Northern Sinus Meridiani Landing Sites for MSL K. S. Edgett and.
MSL Science Team Field Site Discussions — Eberswalde CraterEdgett, p. 1 Eberswalde Crater MSL Candidate Field Site in Context by K. Edgett, 9 June 2010.
Bradley Central High School
11 CHAPTER 11 Mountain Building. Factors Affecting Deformation 11.1 ROCK DEFORMATION  Factors that influence the strength of a rock and how it will deform.
Textbook for geologists (2002) Geologic map of the Sheep Mt. Anticline, Wyoming, based on air photos. From Banjeree and Mitra AAPG Bulletin 88(9):
Dohm’s Mystery Area James Dohm. Stratigraphy Unit Ch – Channel material: (1) Elongate polygons (geometric shape), (2) networking polygons, (3) occurs.
2 Types.  Relative Dating  Absolute Dating  1. Law of superposition – youngest layer on top; oldest layer on bottom.
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,
A Wealth of Opportunities The signature of water is pervasive in and around the proposed ellipse, which resides ~600 km ENE of Opportunity –Ellipse: Over.
1 Presenter: Paige Valderrama Graff
Mountain Building Orogenesis – factors that produce a mountain belt.
Gale Crater Stratigraphic Measurements and Preliminary Interpretations Ryan Anderson April, 2009.
Structure An Introduction to Deformation. Standards Describe the composition and structure of Earth’s materials.
The Law of Superposition Any method of determining whether an event or object is older or younger than another event. Comparing rock layers or fossils.
Models of the Earth Section 3 Section 3: Types of Maps Preview Key Ideas Topographic Maps Topographic Maps and Contour Lines Index Contour, Contour Interval,
Tahsin Islam University of Barisal.. Stratigraphy: Stratigraphy is the study of rock layers (strata) and their relationship with each other. Stratigraphy.
FOLDS, FAULTS AND GEOLOGIC MAPS
Lecture 1: Introduction
Department of Geology and Geological Engineering
Eric H Christiansen.
Stratigraphy.
Geologic Maps Geologic Principles Original horizontality Superposition
11.1 Rock Deformation Factors Affecting Deformation
Crustal Deformation Chapter 10.
Chapter 3 Section 3 Types of Maps Objectives
FACULTY OF ENGINEERING TECHNOLOGY & RESEARCH
Harry Williams, Geomorphology(21)
Field measurements Preparation to field work
Submition : geology Group:2.
Geologic Maps Geologic Principles Original horizontality Superposition
Crustal Deformation Folds Faults Mountain Building
Modification of Rocks by Folding and Fracturing
Geologic Maps Geologic Principles Original horizontality Superposition
Cross-Sections Depict units as they would appear in a vertical slice through the crust, like in a cliff exposure. Cross-sections can be constructed by.
Time and Stratigraphy Basics
DO NOW Pick up notes and Review #11. Turn IN Review #10.
Earth’s History: The Law of Superposition Guided Notes
Thank you for not chewing gum 
William W. Sager, Department of Oceanography, Texas A&M University
How Old is Old? Geologic Time.
Old Red Sandstone formation, St. Annes Whales
Structural Geology Structural geology is the study of rocks deformed by stress and strain This involves trying to understand stress and strain forces to.
William W. Sager, Department of Oceanography, Texas A&M University
Attitude of Beds Attitude: A general term for the orientation of a line or plane. Attitude refers to the three dimensional orientation of planar and linear.
Geomorphology of Eastern Meridiani Planum
Mapping.
Tracing Contacts Complex map patterns are due to
Structure Contour Maps
Stratigraphic Analysis of the Distributary Fan in Holden NE Crater
TOPIC XIII INTERPRETING GEOLOGIC HISTORY
Earth’s History: The Law of Superposition Guided Notes
Principles of Relative Age Dating
GY111L Physical Geology Lab
GY111L Physical Geology Lab
Presentation transcript:

Holden NE crater Main Goals: Discriminate between Lacustrine Delta/Alluvial Fan hypotheses Analysis of the complex stratigraphy within the fan Look for evidence for/against persistent flow

Holden Layers Roughly 150 meters of layered deposits within the Holden fan Stereo data shows distinct layers clearly Profiles can be extracted along continuous outcrops of a single layer

Holden NE Layer Profiles Current focus: determining strike and dip of layers, with the goal of examining structure perpendicular to channels

Meridiani Circular Feature Main goals: Determine Formation Process Investigate regional stratigraphy

Geologic Map of Meridiani Hematite Unit Etched Terrain Region of Interest Region of interest is a small part of the geology of Meridiani Units in the region of interest lie stratigraphically below hematite unit

Region of Interest Layered Blanket Dozens of layers Linear features 1 km

Meridiani DEM 4 stereo DEMs were produced of the circular feature All DEMs had good correlation, but all had some degree of ‘jitter’

Stereo vs. MOLA Top – Stereo derived, gridded DEM profile Bottom – MOLA gridded DEM profile Both profiles show a fold in the topography Circular feature tilted to the north Depression has anomalously low depth/diameter ratio

Geologic Model Stratigraphy in this area is more complex than expected This may be a clue to the depositional history of these units

Formation Hypotheses 1) Crater with sedimentary deposits 2) Crater with Fluidized Ejecta 3) Circular Anticline (dome)

Radial Profile