GE 2400 Test #2 3/26/03. Name

Similar documents
a. The distance from a shot point in which no refracted energy is recorded is termed the.

EOS 350 MIDTERM OCT 4, 2013 STUDENT NAME: TEAM #:

Magnetic field nomenclature

Winmeen Tnpsc Group 1 & 2 Self Preparation Course Physics UNIT 10. Magnetism

2c. No incident magnetic field. 2d. Earth's field causes material to become magnetized.

Magnetism.

3. Magnetic Methods / 62

PHYS 1444 Lecture #10

ENVI.2030L - Plate Tectonics - Geomagnetism, Earthquakes, and Gravity

Department of Geophysics Faculty of Earth Sciences King Abdulaziz University

Available online Journal of Scientific and Engineering Research, 2016, 3(2):1-7. Research Article

10. Paleomagnetism and Polar Wandering Curves.

CHAPTER X. Second Half Review 2017


GEOL.3250 Geology for Engineers Plate Tectonics - Geomagnetism, Earthquakes, and Gravity

Geophysics Physics of the Earth

MAGNETIC MODELING OF THE SUBSURFACE STRUCTURE OF SHIP ROCK, NEW MEXICO

INTRODUCTION TO APPLIED GEOPHYSICS

224 D4 Instrumentation and data collection techniques for magnetic exploration

ENV-5004B/ENVK5005B. Figure 6. Student Registration No. ENV-5004B/ENVK5005B Version 2

Lecture 36: WED 19 NOV CH32: Maxwell s Equations II

CHAPTER 20 Magnetism

What Forces Drive Plate Tectonics?

With a group, get a bar magnet, some plastic wrap, iron filings and a compass.

Physics of Magnetism. Chapter references are to Essentials of Paleomagnetism, UC Press, 2010

Lecture #13 notes, Geology 3950 Spring 2006: CR Stern Magnetic reversals (text pages th edition and in the 5 th edition)

Kirchhoff s rules, example

Civilization exists by geologic consent, subject to change without notice William Durant

Magnetic Case Study: Raglan Mine Laura Davis May 24, 2006

THE INDIAN COMMUNITY SCHOOL, KUWAIT

C5 Magnetic exploration methods data analysis techniques

Geomagnetics. Magnetic Surveying

B for a Long, Straight Conductor, Special Case. If the conductor is an infinitely long, straight wire, θ 1 = 0 and θ 2 = π The field becomes

Phys102 Lecture 16/17 Magnetic fields

Chapter 19. Magnetism

Earth in 2-D, 3-D & 4-D

Global Models of the Magnetic Field in Historical Times: Augmenting Declination Observations with Archeo- and Paleo- Magnetic Data D.

CHARGE TO MASS RATIO FOR THE ELECTRON

Magnetic Forces and Magnetic Fields

C3: Magnetic anomalies produced by simple geological structures. Remember that objects can acquire both induced and remnant magnetization.

Latitude and Longitude Pre Test

The Geodynamo and Paleomagnetism Brown and Mussett (1993) ch. 6; Fowler p

(ii) Observational Geomagnetism. Lecture 5: Spherical harmonic field models

An Introduction to Geophysical Exploration

TAKE HOME EXAM 8R - Geology

Current Loop as a Magnetic Dipole & Dipole Moment:

1-1 Magnetism. q ν B.(1) = q ( ) (2)

TEACHING PLATE TECTONICS FROM THE EVIDENCE. Stephen T. Allard Associate Professor of Geoscience Winona State University

PHYS 1444 Section 003 Lecture #15

physics 590 ruslan prozorov magnetic measurements Nov 9,

Seafloor Spreading and Paleomagnetism Activity

(D) Blv/R Counterclockwise

Geothermal Energy Resources Exploration using Gravity and magnetics. By Mariita, N.O. KenGen

Is the Troodos ophiolite (Cyprus) a complete, transform. fault bounded Neotethyan ridge segment?

Chapter 02 The Sea Floor

Earth s Interior: Big Ideas. Structure of the Earth

The Magnetic Field of the Earth

OCN 201 Seafloor Spreading and Plate Tectonics. Question

22. PALEOMAGNETIC EVIDENCE FOR MOTION OF THE PACIFIC PLATE FROM LEG 32 BASALTS AND MAGNETIC ANOMALIES 1

Lecture 4. Things we might want to know about the geomagnetic field. Components of the geomagnetic field. The geomagnetic reference field

Elements of magnetism and magnetic measurements

PSc 201 Chapter 3 Homework. Critical Thinking Questions

Chapter 3 Models of the Earth. 3.1 Finding Locations on the Earth. 3.1 Objectives

Global geophysics and wave propagation

Chapter 21. Magnetic Forces and Magnetic Fields

Plate Tectonics. entirely rock both and rock

Report of Gridding and Magnetic Surveys. On the. Munro Property. Munro and Beatty Townships, Ontario. Larder Lake Mining Division

Lesson Overview. Climate. Lesson Overview. 4.1 Climate

MIDTERM PRACTICE EXAM

Theory of Plate Tectonics

CHAPTER 2 THE WAY THE EARTH WORKS: EXAMINING PLATE TECTONICS

Tsunami, earthquakes and volcanic eruptions. Tsunami, earthquakes and volcanic eruptions. Destruction of Moawhitu. Plate tectonics: terminology

Earth as a planet: Interior and Surface layers


Waves and Weather. 1. Where do waves come from? 2. What storms produce good surfing waves? 3. Where do these storms frequently form?

Displacement Current. Ampere s law in the original form is valid only if any electric fields present are constant in time

Intro to magnetic methods

Physics 17 Part M Dr. Alward

KEMESS SOUTH MAGNETIC MODELING. CONDOR CONSULTING, INC. OCTOBER 2017

25. PALEOMAGNETISM OF IGNEOUS SAMPLES 1

EWING S MOLECULAR THEORY OF MAGNETISM AND ITS FAILURES

OCN 201 Mantle plumes and hot spots

Oceanic crust forms at ocean ridges and becomes part of the seafloor. Review Vocabulary. basalt: a dark-gray to black fine-grained igneous rock

LATITUDES AND LONGITUDES

2. Determine the excess charge on the outer surface of the outer sphere (a distance c from the center of the system).

4. An electron moving in the positive x direction experiences a magnetic force in the positive z direction. If B x

PART A: Short-answer questions (50%; each worth 2%)

Unit A (225 m.y. old) Unit B (how old is it?) Unit C (275 m.y. old)

Engineering Geology. Earth Structure. Hussien aldeeky

ANTENNA AND WAVE PROPAGATION

Physics 2220 Fall 2010 George Williams THIRD MIDTERM - REVIEW PROBLEMS

1/3/2011. This course discusses the physical laws that govern atmosphere/ocean motions.

Crustal Boundaries. As they move across the asthenosphere and form plate boundaries they interact in various ways. Convergent Transform Divergent

Lab 2: Plate tectonics

Final Review session 2

Chapter 27 Magnetism 1/20/ Magnets and Magnetic Fields Magnets and Magnetic Fields Magnets and Magnetic Fields

Physics Week 5(Sem. 2) Name. Magnetism. Chapter Summary. Magnetic Fields

PALAEOMAGNETISM. Results from palaeomagnetism Polar wander curves: continental drift and rotation.

2. Draw the Magnetic Field lines created by the below two bar magnets. Homework 3. Draw the Magnetic Field lines created by the below bar magnets.

Chapter 20. Plate Tectonics

Transcription:

GE 2400 Test #2 3/26/03 Name 9. Fill in the blank. a. minerals have a negative magnetic susceptibility. b. Ground surveys that use gradiometer magnetometers generally measure the. c. Horizontal derivatives of potential field data (especially gravity data) produce gradients that are steepest over the of tabular bodies. d. The degree to which a body becomes magnetized is determined by this fundamental physical property. e. Upward continuation of a potential field produces a map where (longer, shorter) wavelengths are preserved. f. The presence of linear magnetic anomalies on the ocean floor suggest that the Konigsberger ratio (Q) of the ocean floor basalts is (greater than, less than) one. g. The angle between the horizontal component (H o ) and the total field vector (T o ) is termed the. h. The partitioning of an incident wave's energy at an interface is determined by the of the two layers and by the angle of the angle of incidence. i. The magnetic field one Earth radius above the North Magnetic Pole is (8x, 4x, 2x, 1 / 2 x, 1 / 4 x, 1 / 8 x) the value of the field at the pole. j. Particle motion in this surface wave is transverse to the direction of propagation of the wave:. k. 1 nanotesla = gammas = gauss = Teslas = webers/m 2 l. This type of remanent magnetization is acquired by lava flows as they cool in the presence of Earth s magnetic field. m. If a wave impinges upon an irregular surface with a sharp radius of curvature, the seismic wave bends around the feature giving rise to. n. Magnetic permeability of free space (µ o ) in the cgs system is equal to. o. In these materials the spin magnetic moments of unpaired electrons between neighboring atoms are magnetically coupled, moments are parallel and equal.

2. Two magnetic anomalies are evident on the profile shown below. Both are caused by sources having the same size, shape, and directions of magnetization. Which source body a. is the deepest? b. has the strongest magnetization? Defend your answers. 3. What is the name given to the phenomenon shown in the figure below and what is the cause of this phenomenon?

4. If the magnetic field of Earth were due entirely to a dipole aligned along its rotation axis and position at its center, i.e. geocentric axial dipole (GAD), what is the relationship between magnetic latitude and geographic latitude? Paleomagnetic measurements on the Portage Lake volcanics indicate that these rocks formed during a period of time when the inclination of Earth s magnetic field in the Houghton vicinity was 30 o. At what latitude was Houghton at during the eruption of these volcanics? If the average declination determined from these volcanics was zero, what is the location of the North Magnetic Pole? Assume a GAD model for the field. If 5. Many airports on the Hawaiian Islands are built over areas underlain by lava tubes. The Keohole Airport on the big island of Hawaii is a case in point. Geological evidence points to the existence of shallow east-west trending master-tube system in the vicinity of the proposed airport expansion. These tubes have an average diameter of 5 meters and typically lie 1 meter below ground surface. What would the maximum gravity anomaly in gu be directly over one of these tubes? Density of the volcanic rocks is 2950 kg/m 3. 6. Given a P-wave travelling through a rock unit (V p = 1200 m/sec). This rock unit is in contact with another unit that has greater seismic wave velocities (V p = 3800 m/sec; V s = 1900 m/sec). At what angle must the ray strike the contact between these two units to produce a compressional head wave? a shear head wave?

7. Alkali-vapor and proton precession magnetometers are said to be scalar magnetometers while fluxgate magnetometers are said to be vector magnetometers. Why? 8. The diagram below depicts the H, Z, and T anomalies over a uniformly magnetized sphere with radius 1 m and whose center lies at 3 m depth at position x = 15 m. Earth s inducing field (T o ) is 50,000 nt, inclination (I o ) is 60 o, declination is zero, and k = 0.05 SI units. What s wrong with these anomalies? North is to the right. What is the correct H value at x = 15 m?

9. The magnetic anomalies shown below are caused by buried spheres (dipoles) magnetized by induction in the Northern Hemisphere. In the circle to the right of each anomaly draw the orientation of the inducted magnetization vector (J i ) responsible for the anomaly.