Trigonometry Overview tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.

Slides:



Advertisements
Similar presentations
Unconformities and Faults
Advertisements

11.2A Folds, Faults, and Mountains
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and.
Magnetic Methods (IV) Environmental and Exploration Geophysics I
Unit 35 Trigonometric Problems Presentation 1Finding Angles in Right Angled Triangles Presentation 3Problems using Trigonometry 2 Presentation 4Sine Rule.
Environmental and Exploration Geophysics II tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
Right Triangle Trigonometry
Cross Section Construction
GY403 Structural Geology Lab
Exercise set 2: The 3 point problem
BROOKLYN COLLEGE GEOLOGY DEPARTMENT Review for Exam 1 Maps You will be responsible to answer similar questions as you had on your map assignment. This.
Angle of Elevation & Angle of Depression
4.8 Solving Problems with Trigonometry. What you’ll learn about More Right Triangle Problems Simple Harmonic Motion … and why These problems illustrate.
Trigonometry Overview Part 2 tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
Word Problems for Right Triangle Trig. Angle of Elevation: The angle above the horizontal that an observer must look at to see an object that is higher.
TRIGONOMETRY Lesson 3: Solving Problems Involving Right Triangles.
Locating Points on a Circle Sine Cosine Tangent. Coordinates Systems Review There are 3 types of coordinate systems which we will use: Absolute Incremental.
Tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
Slide 8- 1 Copyright © 2006 Pearson Education, Inc. Publishing as Pearson Addison-Wesley.
Crustal Deformation Review of Chapter 11. Isostasy Balance in possible vertical movement of the plates –Gravity bears down –Heated aesthenosphere is buoyant.
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.
Chapter 8 By Jonathan Huddleston. 8-1 Vocab.  Geometric Mean- The positive square root of the product of two positive numbers.
Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
MATH 306 Chapter 1.
Word Problems: Finding a Side of a Right Triangle (given a side and an angle) Note to Instructor: These word problems do not require Law of Sines or Law.
Trigonometry Overview tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
Copyright © 2011 Pearson, Inc. 4.8 Solving Problems with Trigonometry.
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and.
Tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV Equation Manipulation illustrated around.
Warm up… Page 481 # Angles of Elevation and Depression.
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics II tom.h.wilson Department of Geology.
Environmental and Exploration Geophysics II tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
Projectile Motion 2 Launch Angles (symmetrical and asymmetrical trajectories) Physics 12.
Tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
9.5 Trigonometric Ratios Advanced Geometry.
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and.
Numerical Trigonometry. Trigonometry Trigonometric ratios used with right triangles.
Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and Geography West Virginia University Morgantown,
Tom Wilson, Department of Geology and Geography tom.h.wilson Department of Geology and Geography West Virginia University Morgantown,
When solving a right triangle, we will use the sine, cosine, and tangent functions, rather than their reciprocals.
Right Triangle Trigonometry
Trigonometric Functions
Tom Wilson, Department of Geology and Geography tom.h.wilson Department of Geology and Geography West Virginia University Morgantown,
Lesson 3: Solving Problems Involving Right Triangles
Environmental and Exploration Geophysics II tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
Investigate Tangent Ratios 1. Select one angle measure from 20º, 30º, 40º, or 50º. 2. Each person draw a right triangle ( ∆ ABC) where  A has the selected.
Coincident Source receiver Concepts
Objective To use angles of elevation and depression to solve problems.
Warm-up. Law of Sines and Cosines Students will be able to apply the Law of Sines and the Law of Cosines to solve problems involving oblique triangles.
Environmental and Exploration Geophysics II tom.h.wilson Department of Geology and Geography West Virginia University Morgantown,
9.5: Trigonometric Ratios. Vocabulary Trigonometric Ratio: the ratio of the lengths of two sides of a right triangle Angle of elevation: the angle that.
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and.
Geologic Geometry. TOPOGRAPHIC MAPS Many problems in mining and civil engineering are solved by graphic communication.
Chapter 3 Two-Dimensional Motion and Vectors. Question In terms of A and B, what vector operation does R represent? A B R A -B.
8.5 Angles of Elevation and Depression
1 Maps in Environmental Geology Lecture by Dr. Ken Galli, Boston College EESC Environmental Issues and Resources July 14, 2016 Please do not distribute.
Right Triangle Trigonometry 4.8
Chapter 17: Trigonometry
Angles of Elevation & Angles of Depression
Right-angled Trigonometry
Look at the block diagram below.
Layer Thickness and Map Width
Geomath Geology Final Review - Part 1 tom.h.wilson
Geologic Maps and Cross Sections
Structure Contour Maps
Brunton Compass Good to w/in ca. +/- 1 degree. Metal is bad!
Geologic Cross-Sections
Copyright © Cengage Learning. All rights reserved.
Geomath Geology Final Review - Part 2 tom.h.wilson
Presentation transcript:

Trigonometry Overview tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV

Examine the map and measure the distances from the church to the transmitter. If from an exposure, the church is seen to be located 45 o west of north whilst the transmitter is due west, where is the exposure? How far is the exposure from the church and how far from the transmitter?

Given the outcrop width of 1.25 kilometers for this massive sand which dips northwest at 36 o ….. what is the true (bed normal) thickness of the sand?

h x  Cliff Face 1. At the base of a cliff you are standing on top of geological Unit A. The cliff face is formed along a normal fault (nearly vertical). The top of Unit A is also exposed at the top of the cliff face. You walk a distance x = 200 feet away from the fault scarp. Looking back toward the cliff, you use your Brunton and measure and note that the top of the cliff is 23 o above the horizon. What is the offset along this fault? IN-CLASS PROBLEMS

A group trekking through the Himalayas quickly gets lost having forgotten their top maps. They did bring their radio transmitter though. How can they help searchers determine their location? Assume they have a digital altimeter/barometer and all-purpose Brunton compass.

2. In the example illustrated below, a stream erodes less resistant fault gauge leaving an exposed fault scarp on the distant bank. You are unable to traverse the stream or make your way to the top of the exposure. Using your Brunton compass, you stand on the left edge of the stream and measure the angle (a) formed by the top of the cliff and the horizontal. You walk to the left 175 feet and measure angle (b). Angle a measure 31 o and angle b, 19 o. How can you determine the cliff height? What is the width of the stream? h d a b Stream Fault Scarp

-4300’ -4700’ -5000’ N 4. The three point problem uses elevations measured at three points on a stratigraphic surface to determine the strike and dip of that surface. The elevations and locations of these points can be measured at the surface or, more likely, in the borehole. In the following problem, you have data from three boreholes (located in the map below) indicating subsea depths to the top of the Oriskany Sandstone as shown. Scale: 1:1000

The following figures were taken from visit this site for a more comprehensive overview of the three-point problem

Now, how can you determine the dip? Measure length of line 3. Given this length and the drop in elevation you can figure the dip  directly -  2080 feet 300 feet

a b c A B C 1. The 180 o rule Sine rule Cosine rule

Triangles which do not contain a right angle

Question: Does the vector sum of C and D equal B? If not, how has velocity changed? What geological processes are accommodated by this change.