Geologic Cross-Sections

Slides:



Advertisements
Similar presentations
Topographic Maps Obj- 7. Describe how contour lines and contour intervals are used to show elevation on topographic maps 8. List the 5 rules of topographic.
Advertisements

Unconformities and Faults
For your sketch here, look at this stream valley. Sketch how it changes course. If you see any other streams that do the same, note them.
Isopach and Isochore Maps
a ridge a valley going uphill
Mecca Hills’ Painted Canyon
Cross Section Construction
GY403 Structural Geology Lab
Exercise set 2: The 3 point problem
Section 3: Types of Maps Preview Objectives Topographic Maps
GEOTECHNICAL PROPERTIES (CE1203)
Topographic Maps.
Cross sections of folded and dipping beds
Section 3: Types of Maps Objectives
Stereographic projections. Need to project planes and lines Orthographic projections (will use in lab a little, less widely applied) Stereographic projection.
27 June 2015GLG510 Advanced Structural Geology Fold analysis and cross sections.
Supplemental Review and Exercises
Rider Structural Geology GCHERMAN Faults Some exercises adapted from Lisle, R. J., 2004, Geological Structures and Maps, Practical Guide, Third.
Field trip this Saturday! We will leave from the loading dock at 7:30 AM sharp! HYDRATE... or else! BRING >1 GALLON OF WATER!
Exercise set 3: Basic cross sections
GY403 Structural Geology Laboratory
Multiview Drawing 5.00 Demonstrate orthographic projection techniques and principles as they apply to multiview drawings.
Lab evaluations Go to Acadia Central Log in Click on Online Registration Click on Information.
News and information Partner list posted Gas up vans before tomorrow morning Leave some space in your notebook NIU students with yellow GPS come see me.
Trigonometry Overview tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
II. Basic Techniques in Structural Geology
Site Plans and Drawing Techniques – Supplementary views By; Steven and Darian :3.
4B. Outcrop_Pattern_Cross-Section_Profiles
How Do We Construct a Topographic profile? Objective: To accurately construct a profile along any two points on a contour map.
Created By: Belinda Schmahl
TOPOGRAPHIC PROFILES Nick D’Anna HHS 2007 Adapted from R. DeMarco.
Geosteering Using True Stratigraphic Thickness
Structural data processing and interpretation Czech Geological Survey
Trigonometry Overview tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
3D- STRUCTURAL MAP implementing a fictive topographic surface: the well-topography built-up by the iso-TVDSS curves implementing a fictive topographic.
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,
1 Maps in Environmental Geology Lecture by Dr. Ken Galli, Boston College EESC Environmental Issues and Resources July 14, 2016 Please do not distribute.
Chapter Menu Lesson 1: Reading Maps
Ketobe Knob, UT.
Faults Some exercises adapted from Lisle, R. J., 2004, Geological Structures and Maps, Practical Guide, Third edition
نقشه های توپوگرافی مهدی کرد.
Chapter 3 Section 3 Types of Maps Objectives
I. Basic Techniques in Structural Geology
I. Basic Techniques in Structural Geology
Look at the block diagram below.
Field measurements Preparation to field work
GY403 Structural Geology Laboratory
Types of Maps 3.
Layer Thickness and Map Width
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.
Geomath Geology Final Review - Part 1 tom.h.wilson
Lab evaluations Go to Acadia Central
Name: Answers: (a) (b) (c) From /Rider/Lisle Geol Struct and Maps.pdf
Geologic Maps and Cross Sections
Generate a line representing the sub crop trace of the coal seam.
Old Red Sandstone formation, St. Annes Whales
Exercise set 2: The 3 point problem
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.
ES089 – Working in Three Dimensions
Tracing Contacts Complex map patterns are due to
Section 7.1 Day 1-2 Area of a Region Between Two Curves
Structure Contour Maps
Brunton Compass Good to w/in ca. +/- 1 degree. Metal is bad!
Attitudes of Planes and Lines
Product Rule/Quotient Rule
Do not use a calculator for the following!!.
A B C c b a c A B H= a(sinB) B = drill plunge a =(cSinA/SinC)
GY111L Physical Geology Lab
GY111L Physical Geology Lab
This angle is also a right angle.
Presentation transcript:

Geologic Cross-Sections

Cross Sections are Based on Surface and Sub-Surface Data

Sub-Surface Interpretation (3-D)

Constructing a Cross-Section choose a line of section (perpendicular to structures)

Cross-Section Construction Cont… 2. transfer topographic data (topographic profile with no vertical exaggeration)

Structural Data – (Apparent) Dips 3. add structural data to the topographic profile

Add the Geology! 4. add geologic data (contacts) to the profile; dash in eroded structures above present-day topography

Apparent Dip

True Dip & Apparent Dip

Apparent to True Dip Trigonometry = apparent dip = angle between strike and apparent dip direction = true dip

Calculating Apparent Dip from True Dip ( )

Apparent Dip “Nomogram”

True Dip to Apparent Dip – the Easy Way!

Cross Section “Rules” calculate apparent dips of beds that are not perfectly perpendicular to your section line DO NOT use vertical exaggeration don’t extrapolate structural data too far from your section line dash in eroded structures above the present-day topography don’t extend dip data more than a few hundred meters in depth