Seismology PowerPoint Presentations - PPT

Seismology and the Earth’s Deep Interior
Seismology and the Earth’s Deep Interior - pdf

trish-goza

Seismometry Seismometer –examplesSeismometer –examples ugx x0 xr Seismology and the Earth’s Deep Interior Seismometry Seismometer –examplesSeismometer –examples ugx x0 xr Seis

Glacial Hazard Monitoring
Glacial Hazard Monitoring - presentation

karlyn-boh

With Seismology. Fabian Walter. 2009 – Dr. sc. ETH Zürich. 2004 – MSc University of Colorado, USA. 2002 – BSc Brigham Young University, USA. Host: Laboratory of Hydraulics, Hydrology and Glaciology .

Seismologist
Seismologist - presentation

trish-goza

. By: Valentina, Laurel, Miriam, Crystal, Isaiah, Adam, Landon, and Emma.. What Does a Seismologist . S. tudy?. A seismologist studies earthquakes, faults, and seismology. Seismologist also use a Richter Scale to measure earthquakes. .

Seismology:
Seismology: - presentation

jane-oiler

● What is Seismology?. ● What are Seismic Waves?: Types of Seismic waves. ● Where do Earthquakes Happen?. ● Why do Earthquakes Happen?. ● How is the Epicenter of an Earthquake Located?. ● How are Earthquakes Magnitude Measured?.

Rethinking Array Seismology in
Rethinking Array Seismology in - presentation

danika-pri

Nuclear-Test-Ban Treaty Monitoring . Steven J. Gibbons. Workshop on Arrays in Global Seismology,. Raleigh, North Carolina, May 15-16 2013. .. Rethinking Array Seismology in Nuclear-Test-Ban Treaty Monitoring .

in Seismology
in Seismology - pdf

test

1 Glossary Active faul t A fault that has moved in historic (e.g., past 10,000 years) or recent geological past (e.g., past 500,000 years). Aftershock An earthquake that follows a large magnitude e

Introduction to Engineer
Introduction to Engineer - pdf

faustina-d

ing Seismology Lecture 5 Dr. P. Anbazhagan 1 of 2 7 Lecture 5 : Concept of Seismic magnitude and Intensity , earthquake size, different magnitude scales and relations. Topics Introduction Intensit

EX40001 Earth and Planetary Systems 3 0 0 3
EX40001 Earth and Planetary Systems 3 0 0 3 - pdf

test

EX40003 Earthquake Seismology 3 1 0 4 EX43005 Seismic Methods of Prospecting 3 1 0 4 Seismic Methods of Prospecting Lab 0 0 3 2 EX43007 Stationary Field and Electrical Methods 3 0 0 3 EX40004 Ti

Seismology and the Earth’s Deep Interior
Seismology and the Earth’s Deep Interior - pdf

giovanna-b

Seismogram Interpretation Wavefieldsin the Earth: SH wavesWavefieldsin the Earth: SH waves Wavefieldfor Seismology and the Earth’s Deep Interior Seismogram Interpretation Wavefieldsin the Earth:

Introduction to Engineer ing Seismology Lecture Dr
Introduction to Engineer ing Seismology Lecture Dr - pdf

cheryl-pis

P Anbazhagan of Lecture Concept of Seismic magnitude and Intensity earthquake size different magnitude scales and relations Topics Introduction Intensity Comparison of different intensity scales Problems associated with Non instrumental measuremen

Geology 5640/6640 Introduction to Seismology
Geology 5640/6640 Introduction to Seismology - presentation

celsa-spra

15 Feb 2017. © A.R. Lowry . 2017. Read for . Wed 17 . Feb: . S&W. 62-75 (§2.5). Last time:. . Seismology as Investigative Tool. Deep-Earth . investigations use earthquakes as sources,. three-component broadband seismometers as receivers,.

SEISMOLOGY
SEISMOLOGY - presentation

trish-goza

(All shook up.). Earthquakes can be frightening events. .. (Click on left image for short video.). Earthquakes. Usually happen near . faults.. (What are faults?). Many faults are near plate boundaries, but they can be anywhere and everywhere..

Small scale reflection seismology
Small scale reflection seismology - presentation

ellena-man

CMP gather. 3D seismic reflection. The goal is a 3D image of structure. (data cube). Visualization. (slice & dice). 3-D image. Volume construction of salt dome image. Typical Geometry for 3D Acquisition .

Refraction Seismology
Refraction Seismology - presentation

yoshiko-ma

Chapter :: 6. Snell’s Revenge!. Snell’s Law & Critical Refraction. Because seismic sources radiate waves in all directions. Some ray must hit interface at exactly the critical angle, . i. c. This critically oriented ray will then travel along the interface between the two layers.

Broadband Array in Taiwan for Seismology (BATS)
Broadband Array in Taiwan for Seismology (BATS) - presentation

trish-goza

http://bats.earth.sinica.edu.tw. . Institute of Earth Sciences. Academia . Sinica. Yifan. Yin*, Wen-Tzong Liang,. Chun-Chi Liu and Bor-Shouh Huang. History of BATS. Our missions:. To better monitor the earthquake activity in the Taiwan region.

Earthquake Seismology:
Earthquake Seismology: - presentation

pamella-mo

Rayleigh waves. Love waves. Dispersion. Follows mainly on:. Lay and Wallace, Modern global seismology, Academic Press.. Stein and . Wysession. , an introduction to seismology, earthquakes and Earth structure, Blackwell Publishing.

FUNDAMENTALS of ENGINEERING SEISMOLOGY
FUNDAMENTALS of ENGINEERING SEISMOLOGY - presentation

yoshiko-ma

GROUND MOTIONS FROM SIMULATIONS. 1. Observed data adequate for regression except. close to large ‘quakes . Observed data not adequate for regression, . use simulated data . 2. Ground-Motions for Regions Lacking Data from Earthquakes in Magnitude-Distance Region of Engineering Interest.

FUNDAMENTALS of ENGINEERING SEISMOLOGY
FUNDAMENTALS of ENGINEERING SEISMOLOGY - presentation

trish-goza

EARTHQUAKE FOCAL MECHANISMS (FAULT PLANE SOLUTIONS). Credits:. -Some slides provided by Dino Bindi (INGV) and A. Kelly (USGS). -Cox and Hart. Plate Tectonics – How it works.. -Stein and Wysession, An Introduction to seismology, earthquakes and .

FUNDAMENTALS of ENGINEERING SEISMOLOGY
FUNDAMENTALS of ENGINEERING SEISMOLOGY - presentation

calandra-b

GROUND MOTIONS FROM SIMULATIONS. 1. Observed data adequate for regression except. close to large ‘quakes . Observed data not adequate for regression, . use simulated data . 2. Ground-Motions for Regions Lacking Data from Earthquakes in Magnitude-Distance Region of Engineering Interest.

FUNDAMENTALS of ENGINEERING SEISMOLOGY
FUNDAMENTALS of ENGINEERING SEISMOLOGY - presentation

trish-goza

EARTHQUAKE MAGNITUDES. Earthquake source characterization. Magnitude. Fault dimensions (covered before). Slip distribution (kinematics). Fourier transform refresher. Point source representation. Spectral shape.

Tucson SITS 2018 – Theo
Tucson SITS 2018 – Theo - presentation

kittie-lec

Laudat. – 30/10/2018. blueSeis-3A rotational seismometer. Outline. 1. iXblue & Fog technology. 2. blueSeis-3A rotational seismometer. 3. Characterization of performances. 4. Let’s get started!.

FUNDAMENTALS of ENGINEERING SEISMOLOGY
FUNDAMENTALS of ENGINEERING SEISMOLOGY - presentation

liane-varn

LOCATING EARTHQUAKES. The release of the accumulated elastic strain energy by the sudden rupture of the fault is the cause of the earthquake shaking. Ground Motion Deconvolution. (Steidl). Earthquakes are not located randomly around the Earth.

FUNDAMENTALS of ENGINEERING SEISMOLOGY
FUNDAMENTALS of ENGINEERING SEISMOLOGY - presentation

conchita-m

MEASURING GROUND MOTION. The first known instrument for earthquakes measurement is the Chang seismoscope built in China in 132 B.C. . Balls were held in the dragons’ mouths by lever devices connected to an internal pendulum. The direction of the epicenter was reputed to be indicated by the first ball released..

Geology 5640/6640 Introduction to Seismology
Geology 5640/6640 Introduction to Seismology - presentation

cheryl-pis

24 . Feb . 2017. © A.R. Lowry . 2017. Last time: . Ray Theory. • Rays follow . Snell’s . Law. :. where . . is . angle of incidence. • From Snell. ’. s Law, the . ray parameter . (where .

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