Dr Liam Herringshaw: An Introduction To Geological Maps.

Slides:



Advertisements
Similar presentations
Ge 101: Introduction to Geology and Geochemistry
Advertisements

GEOLOGIC MAPPING 2014 EVENT OVERVIEW.
Geologic Time Chapter
Earth Science 12.1 Discovering Earth’s History: Geologic Time
Science Starters Week 1 ILO 1 Observations and Inferences.
SPOT THE DIFFERENCE! Start Geology Roam. Try and find 3 functions not available in Roam (Ordnance Survey): SPOT THE DIFFERENCE! Start Geology Roam.
Dr Liam Herringshaw: York: A Rocky History.
Nonconformity - sedimentary rocks over crystalline (metamorphic or igneous) rocks N. Lindsley-Griffin, 1998.
Learning Objective: I will make a foldable of the three different types of rocks by closely reading the chapter with my group.
Unconformity. It is one of the most common geological feature found in rocks or in succession. It is different then all other geological structures viz.
Interpreting Geologic History
Chapter 6 Earth’s History
GEOLOGIC STRUCTURES “Architecture of bedrock” Structural Geology- –shapes, –arrangement, –interrelationships of bedrock –units & forces that cause them.
Geologic Maps Geology 100 Geology for Environmental Scientists.
Dr Liam Herringshaw: An Introduction To Geological Maps.
G322 Geomorphology – Introduction to Landscape Interpretation For each of the 11 slides of landscape features, make observations and interpretations of.
Overview of Structural Geology (Chapter 1 in D &R)
Telling Time. James Hutton “The Father of Geology” Uniformitarianism.
What’s so remarkable about Hutton’s Ideas?
8 th Grade Science Professional Development Tuesday, February 10, 2009 So Happy to See You Today!
SPOT THE DIFFERENCE! Start Geology Roam. Try and find 3 functions not available in Roam (Ordnance Survey): SPOT THE DIFFERENCE! Start Geology Roam.
Exercise set 3: Basic cross sections
Components of Geologic Maps GEOL 3000 By Mark A. Jirsa and Terrence J. Boerboom 2003.
Components of Geologic Maps By Mark A. Jirsa and Terrence J. Boerboom 2003.
Understanding Planet Earth (EPSC 201) ( Instructor: A.E. (Willy) Williams-Jones Textbooks:
Introduction Stress versus strain: The two most important terms used throughout this course are STRESS and STRAIN. What structural geologists actually.
WJEC A2 Geology BGS Mapwork I.G.Kenyon. BGS 1: scale maps 1mm on the map represents 50m on the ground Grid squares are 1 km² and have sides of 2cm.
Faults and Folds Normal Fault In normal faulting, the hanging wall block moves down relative to the footwall block. The fault plane.
Unit 1 BEDROCK GEOLOGY. The geologic history of the Earth is determined by Earth Science principles such as _________________________ _________________________.
Unit 1 Introduction To Earth Science. Topic 1: Earth Systems As A Science  Earth Science differs from other sciences in that: 1. Earth Science has a.
Powered by Rock Dr Liam Herringshaw Earth's Energy Systems.
LEQ: How do geologists and paleontologists determine the relative age of rocks? Part 2 Key Terms: Uniformitarianism, Original horizontality, cross- cutting.
What is science? an introduction to life science.
Final Exam Review CORC 1332 / EESC 1010 Final Exam: Tuesday, 12/17/13 from 6:05-7:45pm in room 1310N Bring with you a #2 pencil, calculator, ruler, string.
Aim: How do we determine the relative age of rocks?  Do Now: 1. What have we already learned about rock age in the last unit (Think about the laws pertaining.
GNS Science Natural Hazards Research Platform Progress in understanding the Canterbury Earthquakes Kelvin Berryman Manager, Natural Hazards Research Platform.
History of Earth MS-ESS1-4
This Is Planet Earth Dr Liam Herringshaw ( – An Introduction To Geology.
Stratigraphy Stratigraphy is the branch of geology that deals with the arrangement of rocks in layers.
Unit 1: Tools of the Trade. I. What is Science? A. What is it to you? What is it to me? What is it to the text book? A. What is it to you? What is it.
Introduction to Geology Week 1. Geology is.. The scientific study of the Earth and its processes. the physical earth composition processes the historical.
Lecture 2: Deformation, reference frame,
1 Earth’ s History Unit 6. 2 Vocabulary List 1.Relative Dating 2.Absolute Dating 3.Superposition 4.Cross-cutting relationships 5.Uniformitarianism 6.Original.
GEOLOGICAL TIME. GEOLOGY NEEDS A TIME SCALE An investigation of the history of Earth Understanding how features of landscape developed and formed Reconstructing.
2 Types.  Relative Dating  Absolute Dating  1. Law of superposition – youngest layer on top; oldest layer on bottom.
Geology and the Environment ERSC 1F90 Summer 2009.
NS Physical Science Studies Landscapes (Topographic Maps)
Observation vs. Inferences The Local Environment.
Rider Structural Geology GCHERMAN Lab 11. Unconformities & Igneous Rocks Adapted from: Lisle, R. J., 2004, Geological Structures and Maps, A Practical.
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,
Earth Science Notes Relative Age of Rocks. Objectives I can… Distinguish relative and absolute dating. Describe the 6 laws of relative dating. Use the.
Science is a process, or method, that usually starts with an observation.
Rock Relationships and Geological Histories You must have the presentation on Slide Show mode. On opening the presentation, you may be asked to enable.
MSc. Paleontology and Stratigraphy
GLG 101 CART The Power of Possibility/glg101cart.com GLG Week 6 Assignment: Metamorphic Rocks Lab PART ½ (UOP) FOR MORE CLASSES VISIT
EBS101 ENGINEERING GEOLOGY DR HAREYANI ZABIDI
GLG 101 Assignment Groundwater Lab For more classes visit Resource: pp. 213–227 of Geoscience Laboratory and Appendix N. Answer the.
GLG 101 TUTORIAL Learn by Doing / glg101tutorial.com.
Q. What is a crosscutting relationship?
Scientific revolutions
Look at the block diagram below.
Principle of Superposition
Time and Stratigraphy Basics
Thank you for not chewing gum 
Seismic Interpretation
منهج البحث العلمي ( Scientific Research Method )
Earth’s Surface, Earth’s History and Maps
Dr Liam Herringshaw: Geology of York Dr Liam Herringshaw:
Geologic Maps Lecture 38.
Presentation transcript:

Dr Liam Herringshaw: An Introduction To Geological Maps

Recommended text Geological Structures and Maps (Lisle) (or Bennison et al. / Barnes & Lisle)

Course structure 1. Introduction 2. Uniformly dipping strata 3. Folded strata 4. Faults 5. Unconformities 6. Igneous Rocks 7. Metamorphic cleavage 8. Maps in 4D

Introduction Maps & Geology Why map geology and how? How to read geological maps?

Introduction Scarborough sheet: First impressions?

Why map? Ordnance Survey: – military Geological Survey: – economic – scientific

What is a geological map? How does it differ from a 'normal' map? – Interpretive, not just descriptive – = Predictive science

William 'Strata' Smith Origins

Smith & Nephew The Mapping of Yorkshire

What to map? Depends on scale and subject – what are you trying to show?

What to map? What units are mappable? 1:1000 scale 1 mm on map = 1 m wide 1:250,000 scale 1 mm on map = 250 m wide Observed vs inferred features

Topography Learn to read the landscape

What to map? Superficial: also known as 'Drift' mapping

What to map? Bedrock or 'Solid' Geology

Next week: Uniformly dipping strata

Next week: Uniformly dipping strata Useful tools: Protractor, ruler, pencils, paper

Resources ( Geology of Britain Viewer: iGeology: Vale of York bedrock/superficial maps: Link to paper Maps Before Maps: