Geological map of Leeds area

Slides:



Advertisements
Similar presentations
Relative Age Dating Activity.
Advertisements

Unconformities and Faults
WJEC A2 Geology BGS Mapwork I.G.Kenyon Recognising Geological Structures.
AS MAPPING.
- The interaction of the world’s tallest building with the geology of the Basin the city is built in By Matthew Timmis and Mark Banham.
Table of Contents Chapter 3: Rocks Section 4: Sedimentary Rocks.
Sedimentary Rocks Chapter 4 Section 4.
Nonconformity - sedimentary rocks over crystalline (metamorphic or igneous) rocks N. Lindsley-Griffin, 1998.
This sedimentary rock texture means bits and pieces of rock. Clastic.
Steno’s Laws of Stratigraphy
The relative age of rocks and geological events.
Earth History- Table of Contents RELATIVE vs. ABSOLUTE LAWS UNCONFORMITIES GEOLOGIC SECTIONS.
The Phantom Science: How Geology Created The Phantom Science: How Geology Created the Amazing Natural Resources of Central Texas the Amazing Natural Resources.
HYDROCARBON PETROLEUM SYSTEM
Principles of Relative Dating
LESSON 2 THE RELATIVE AGE OF ROCKS
TODAY WE ARE: ANALYZING CROSS SECTIONS SO THAT WE CAN: INTERPRET AND ANALYZE DATA FROM THE FOSSIL RECORD TO SUPPORT A CLAIM THAT ORGANISMS AND ENVIRONMENTS.
Coal The specification states that you should be able to: Describe and explain the origin of coal and coal seams as part of a cyclothem. Describe the development.
 The specification says:  Describe the deposition in deltaic environments of delta top (topsets) to form coal, sandstones of the delta slope (foresets)
Exercise set 2: The 3 point problem
Cross sections of folded and dipping beds
GIS-based TOOL FOR REGIONAL GROUNDWATER RISK ASSESSMENT IN POORLY PRODUCTIVE AQUIFERS Janmaizatulriah JANI, David N LERNER, Steve WISE Catchment Science.
NNPC FSTP Geoscience Course Code: Lesson. Geological Maps and Cross-Sections Contents.
Important Stratigraphic and Geomorphic Concepts Facies.
Key Ideas State the principle of uniformitarianism.
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.
Earth Science Topic #13 Review Game
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.
WJEC A2 Geology BGS Mapwork Exercises I.G.Kenyon.
Geologic and Rock Cycles, Fossils and Unconformities.
Earth History- Table of Contents RELATIVE vs. ABSOLUTE LAWS UNCONFORMITIES GEOLOGIC SECTIONS.
Virginia Physical Geography
Ch.6 Earth’s History. Who’s got the TIME? RELATIVE: order/sequence known, but not the actual date of occurrence. “Time Line” ABSOLUTE: actual date determined.
Virginia Physical Geography. The Physiographic Provinces of Virginia Virginia has had a long, complex geologic history, over 1.1 billion years Events.
Index Fossils and Geologic Time “The Past is the Key to the Present”
LEQ: How do geologists and paleontologists determine the relative age of rocks? Part 2 Key Terms: Uniformitarianism, Original horizontality, cross- cutting.
Sedimentary Rocks Chapter 4 Section 4. Sedimentary Rocks Sediments are loose materials like rock fragments, mineral grains, and bits of shell. Sediments.
Stratigraphy Stratigraphy is the branch of geology that deals with the arrangement of rocks in layers.
The Geologist as Detective Chapter 6 : Interpreting Geologic History.
Physiographic Provinces of Virginia Earth Science.
Chapter 21 Section 4Geologic Time. Chapter 21 Section 4 – What You’ll Learn - page Before you read - write the reading’s objectives in this space: 1 –
GEOLOGICAL TIME. GEOLOGY NEEDS A TIME SCALE An investigation of the history of Earth Understanding how features of landscape developed and formed Reconstructing.
May 13, 2014 Open up your ISN. Call the next available left side page #84. Title the page “Vocabulary”. Call the following page #85. Title the page “The.
Interpreting Ancient Environments
Fossils, Geologic Time, Absolute & Relative Dating, and Natural Resources Chapters 5 & 6.
Rock Relationships and Geological Histories You must have the presentation on Slide Show mode. On opening the presentation, you may be asked to enable.
EBS101 ENGINEERING GEOLOGY DR HAREYANI ZABIDI
Earth’s History Introduction: The earth is about 4.6 billion years old. Much of its history is recorded in the rock. Observations of fossils, rock types,
Earth History Dating geologic events like volcanic eruptions, uplift, subsidence, deposition, impacts, intrusion, ice ages, etc.
= coastal plain (rivers + floodplain) = tidal marsh = lagoon
Geologic Sequencing: The order of geologic events
Earth History- Table of Contents
Stratigraphy: Historical Geology Dr. Prabha Joshi
Table of Contents Chapter 3: Rocks Section 4: Sedimentary Rocks.
How do we determine a sequence of events for rock layers?
Rocks made of bits & pieces of other rocks.
Borehole Image Interpretation Results Wells: E17a-A1, A2 & A3 Gaz de France - Suez – Netherlands Mourad KOURTA Schlumberger, CEU.
Fossils, Geologic Time, Absolute & Relative Dating, and Natural Resources Chapters 5 & 6.
Relative Dating.
Department of Geology, University of Dhaka Maps and Map Reading Lab.
Relative dating… First (oldest) Middle Last (youngest)
Exercise set 2: The 3 point problem
Exercise set 1: V-Outcrop Patterns
Rocks made of bits & pieces of other rocks.
Learning Objective: I will be able to explain how old rock layers are in an outcrop using the laws of geologic time.
Inferred Lithology - Prediction
Rocks made of bits & pieces of other rocks.
Presentation transcript:

Geological map of Leeds area Exercise set 6: Geological map of Leeds area To view this exercise just press F5 now. Then click the mouse to continue through the slides. School of Earth and Environment

Geological map of Leeds area This presentation is to be completed in conjunction with exercise worksheet 6. Objectives: The aim of this exercise is to gain more experience of: Using and understanding geological maps Drawing sketch maps Drawing a simplified cross section to illustrate the structure Identify and interpret faults Locate areas of economic interest School of Earth and Environment

Geological map of Leeds area Using exercise worksheet 6, the geology of Britain viewer and any internet resources available to you, complete each question then click for the answer before continuing onto the next. First go to: http://www.bgs.ac.uk/discoveringGeology/geologyOfBritain/viewer.html Or navigate to it from the BGS website via: www.BGS.ac.uk Click on “Open geology of Britain viewer” Click “Go to location” Type “Leeds” Click “Switch basemap” then choose “OpenStreetMap” School of Earth and Environment

Geological map of Leeds area Study the map and geological key (by clicking on “1:50 000 geology key”) Then by clicking on the rock types name, more information can be found out about that particular unit. Using this information in conjunction with internet resources, answer the questions on the following slides. School of Earth and Environment

Geological map of Leeds area What geological periods are represented and what age range do they span? The geological periods represented are: Superficial deposits Bedrock geology Name Description Period Age (Ma) Alluvium Clay, silt sand and gravel Flandrian 0-0.012 Till Mixed Devensian 0.010-0.011 Mid Pleistocene 0.126-0.781 River terrace deposits Sand and gravel Quaternary 0-2.588 Name Description Period Age (Ma) Thornhill rock Sandstone Duckmantian 311-314 Various other sandstones All Langsettian 316-314 Penine lower coal measure Mudstone, siltstone, sandstone Langsettian Rough rock/flags Yeadonian 316-318 School of Earth and Environment

Geological map of Leeds area What is the oldest carboniferous formation on the map? Name a specific locality where you might find an outcrop. Write a brief rock description including depositional environment of the Pennine lower coal measure. On what formation is the University of Leeds situated? (you may have to zoom a little for this) The oldest carboniferous formation on the map is the Rough rock sandstone This can be found in the North-West of the map. Example: around Abbey road. Interbedded grey mudstone, siltstone and pale grey sandstone, commonly with mudstones containing marine fossils in the lower part and more numerous coal seams in the upper part. These rocks were formed in marginal coastal plains with lakes and swamps periodically inundated by the sea; or estuaries and deltas, and shallow seas. The University of Leeds is partly located on the Pennine lower coal measure and partly on the sandstone. School of Earth and Environment

Geological map of Leeds area Why are many of the units disjointed? What is the general trend of faulting in the area? What is the displacement along the fault that the University of Leeds is situated upon? Due to faulting in the area. The general trend of faults is SW-NE. Using the scale bar at the bottom, it is roughly 1.3km. You may need to zoom to measure this. School of Earth and Environment

Geological map of Leeds area On the rough base map provided: Sketch the approximate boundaries between the lithological units and also the overlaying superficial deposits. School of Earth and Environment

Geological map of Leeds area Mark on the map where there used to be a river bed. School of Earth and Environment

Geological map of Leeds area Mark on the map the general direction of younging of the bedrock. School of Earth and Environment

Geological map of Leeds area Mark on the map the unconformity. School of Earth and Environment

Geological map of Leeds area What is the reason for the shape of the outcrop highlighted by the circle? This displacement of younger middle Pennine coal measure into the older lower Pennine coal measure is due to a large fault. School of Earth and Environment

Summary You should now be more familiar with: Using more complex geological maps. The geology of the Leeds area. The appearance of faults on geological maps. The appearance of superficial deposits on geological maps. How to draw a quick sketch map. School of Earth and Environment