This document summarizes an earthquake that occurred in Sikkim, India in 2011. It discusses the magnitude of the earthquake at 6.9 and the aftershocks that followed throughout the night. It then provides definitions and explanations of key earthquake terms like focus, epicenter, fault, body waves and surface waves. Finally, it discusses the impacts of the earthquake in Sikkim and surrounding areas, including damage to buildings and roads, relief efforts provided, and studies conducted on dams and infrastructure.
This presentation includes introduction to Earthquakes, Seismic Waves, Shallow Focus and Deep Focus Earthquakes, Aftershocks, Earthquake Storms, Effects/Impacts of Earthquakes, Earthquake Predictions.
This presentation includes introduction to Earthquakes, Seismic Waves, Shallow Focus and Deep Focus Earthquakes, Aftershocks, Earthquake Storms, Effects/Impacts of Earthquakes, Earthquake Predictions.
Introduction of earthquake
focus and epicenter of an earthquake.
Relate earthquake activity to plate tectonics
Describe the types of waves emitted during an earthquake.
Distinguish between earthquake intensity and magnitude.
Review some current methods of earthquake prediction.
Preparation and steps during and after earthquake.
Introduction of earthquake
focus and epicenter of an earthquake.
Relate earthquake activity to plate tectonics
Describe the types of waves emitted during an earthquake.
Distinguish between earthquake intensity and magnitude.
Review some current methods of earthquake prediction.
Preparation and steps during and after earthquake.
An earthquake is a violent and abrupt shaking of the ground, caused by movement between tectonic plates along a fault line in the earth's crust. Earthquakes can result in the ground shaking, soil liquefaction, landslides, fissures, avalanches, fires and tsunamis.
How do you describe an earthquake?
A large earthquake far away will feel like a gentle bump followed several seconds later by stronger rolling shaking that may feel like sharp shaking for a little while. A small earthquake nearby will feel like a small sharp jolt followed by a few stronger sharp shakes that pass quickly.
Civil Engineering
Earth Quake Data
Earth Layers
Plate Tectonics
Seismic Waves
Effects of Earthquake
Epicenter of Earthquake
Damages by Earthquake
GEOGRAPHY IGCSE: EARTHQUAKES. It contains: earthquakes, energy and epicentre, measuring the power, effects of an earthquake, factors affecting the impact, earthquakes and volcanoes in LEDC and MEDC. Kobe 1995, Kashmir 2005.
An earthquake (also known as a quake, tremor or temblor) is is the shaking of the surface of the Earth, resulting from the sudden release of energy in the Earth's lithosphere that creates seismic waves. Earthquakes can range in size from those that are so weak that they cannot be felt to those violent enough to the people around and destroy whole cities.
Earthquake
1.Interior of earth
2.Convection currents cause the movement of plates
3.Tectonic Plate
4.Why do earthquakes occur?
5.Where do earthquakes occur.
6.Definitions
7.Seismic waves: forms
8.Measuring earthquakes
9.Classification of earthquake
10.Locating the shaking
11.Earthquake risk and prediction
12.Short-term predictions
13.Impacts of Earthquake Prediction
The Art Pastor's Guide to Sabbath | Steve ThomasonSteve Thomason
What is the purpose of the Sabbath Law in the Torah. It is interesting to compare how the context of the law shifts from Exodus to Deuteronomy. Who gets to rest, and why?
Read| The latest issue of The Challenger is here! We are thrilled to announce that our school paper has qualified for the NATIONAL SCHOOLS PRESS CONFERENCE (NSPC) 2024. Thank you for your unwavering support and trust. Dive into the stories that made us stand out!
Synthetic Fiber Construction in lab .pptxPavel ( NSTU)
Synthetic fiber production is a fascinating and complex field that blends chemistry, engineering, and environmental science. By understanding these aspects, students can gain a comprehensive view of synthetic fiber production, its impact on society and the environment, and the potential for future innovations. Synthetic fibers play a crucial role in modern society, impacting various aspects of daily life, industry, and the environment. ynthetic fibers are integral to modern life, offering a range of benefits from cost-effectiveness and versatility to innovative applications and performance characteristics. While they pose environmental challenges, ongoing research and development aim to create more sustainable and eco-friendly alternatives. Understanding the importance of synthetic fibers helps in appreciating their role in the economy, industry, and daily life, while also emphasizing the need for sustainable practices and innovation.
How to Make a Field invisible in Odoo 17Celine George
It is possible to hide or invisible some fields in odoo. Commonly using “invisible” attribute in the field definition to invisible the fields. This slide will show how to make a field invisible in odoo 17.
Ethnobotany and Ethnopharmacology:
Ethnobotany in herbal drug evaluation,
Impact of Ethnobotany in traditional medicine,
New development in herbals,
Bio-prospecting tools for drug discovery,
Role of Ethnopharmacology in drug evaluation,
Reverse Pharmacology.
The French Revolution, which began in 1789, was a period of radical social and political upheaval in France. It marked the decline of absolute monarchies, the rise of secular and democratic republics, and the eventual rise of Napoleon Bonaparte. This revolutionary period is crucial in understanding the transition from feudalism to modernity in Europe.
For more information, visit-www.vavaclasses.com
The Roman Empire A Historical Colossus.pdfkaushalkr1407
The Roman Empire, a vast and enduring power, stands as one of history's most remarkable civilizations, leaving an indelible imprint on the world. It emerged from the Roman Republic, transitioning into an imperial powerhouse under the leadership of Augustus Caesar in 27 BCE. This transformation marked the beginning of an era defined by unprecedented territorial expansion, architectural marvels, and profound cultural influence.
The empire's roots lie in the city of Rome, founded, according to legend, by Romulus in 753 BCE. Over centuries, Rome evolved from a small settlement to a formidable republic, characterized by a complex political system with elected officials and checks on power. However, internal strife, class conflicts, and military ambitions paved the way for the end of the Republic. Julius Caesar’s dictatorship and subsequent assassination in 44 BCE created a power vacuum, leading to a civil war. Octavian, later Augustus, emerged victorious, heralding the Roman Empire’s birth.
Under Augustus, the empire experienced the Pax Romana, a 200-year period of relative peace and stability. Augustus reformed the military, established efficient administrative systems, and initiated grand construction projects. The empire's borders expanded, encompassing territories from Britain to Egypt and from Spain to the Euphrates. Roman legions, renowned for their discipline and engineering prowess, secured and maintained these vast territories, building roads, fortifications, and cities that facilitated control and integration.
The Roman Empire’s society was hierarchical, with a rigid class system. At the top were the patricians, wealthy elites who held significant political power. Below them were the plebeians, free citizens with limited political influence, and the vast numbers of slaves who formed the backbone of the economy. The family unit was central, governed by the paterfamilias, the male head who held absolute authority.
Culturally, the Romans were eclectic, absorbing and adapting elements from the civilizations they encountered, particularly the Greeks. Roman art, literature, and philosophy reflected this synthesis, creating a rich cultural tapestry. Latin, the Roman language, became the lingua franca of the Western world, influencing numerous modern languages.
Roman architecture and engineering achievements were monumental. They perfected the arch, vault, and dome, constructing enduring structures like the Colosseum, Pantheon, and aqueducts. These engineering marvels not only showcased Roman ingenuity but also served practical purposes, from public entertainment to water supply.
2024.06.01 Introducing a competency framework for languag learning materials ...Sandy Millin
http://sandymillin.wordpress.com/iateflwebinar2024
Published classroom materials form the basis of syllabuses, drive teacher professional development, and have a potentially huge influence on learners, teachers and education systems. All teachers also create their own materials, whether a few sentences on a blackboard, a highly-structured fully-realised online course, or anything in between. Despite this, the knowledge and skills needed to create effective language learning materials are rarely part of teacher training, and are mostly learnt by trial and error.
Knowledge and skills frameworks, generally called competency frameworks, for ELT teachers, trainers and managers have existed for a few years now. However, until I created one for my MA dissertation, there wasn’t one drawing together what we need to know and do to be able to effectively produce language learning materials.
This webinar will introduce you to my framework, highlighting the key competencies I identified from my research. It will also show how anybody involved in language teaching (any language, not just English!), teacher training, managing schools or developing language learning materials can benefit from using the framework.
3. India is vulnerable to different
natural hazards due to its proximity
to geodynamically active locales and
unique climatic pattern.
Both these factors in different
combinations lead to the occurrence
of disasters resulting from natural
hazards like floods, earthquakes,
draught, cyclones and landslides in
different parts of the country at
frequent intervals.
It is estimated that about 60% of
landmass of the country is vulnerable
to earthquakes of different
magnitudes.
4. Sikkim experienced a major
destructive earthquake of 6.9 (Mw)
heating badly causing deaths of no
of people and d.
At least 20 aftershocks at
magnitudes of 5.7, 5.1, and 4.6 (Mw)
within 30 minutes of the initial
earthquake occurred back-to-back
throughout the night created panic
in the Gangtok.
5. Q:What is earthquake?
A:” When the edge of two pieces of the earth
grind together and cause rumbling and shaking
underneath the surface of the earth. The
shaking or trembling caused by the sudden
release of energy is earthquake. Usually it is
associated with faulting or breaking of rocks”.
6. Q:What are the causes of earthquake?
A:”The earth is divided into three main layers – a
hard outer crust, a soft middle crust, and a
center core. The outer crust is broken into
massive irregular pieces called “plates”. These
plates are moving very slowly, driven by energy
forces deep within the earth. Earthquakes
occur when these moving plates grind and
scrape against each other.”
7. What is the Elastic Rebound Theory?
Explains how energy is
stored in rocks
– Rocks bend until the
strength of the rock
is exceeded
– Rupture occurs and
the rocks quickly
rebound to an
undeformed shape
– Energy is released in
waves that radiate
outward from the
fault
8. Causes of Earthquake
Two Types aftershock and foreshock
” An aftershock is a small earthquake that
follows the main earthquake.
A foreshock is a small earthquake that often
precedes a major earthquake”.
15. Focus, Epicenter, and Fault
The point within Earth’s interior where the energy
waves are produced and where faulting begins is the
focus, or hypocenter
The point on Earth’s
surface directly above
the earthquake focus
is Epicenter
Fault is fracture
in Earth where
movement has
occurred
16. Locating an Epicenter
Epicenter Location
– If information is received
from the earthquake at three
stations, then the epicenter
can be located
– A circle is drawn around each
station on a map
• The radius is equal to the
distance from the station to
the epicenter
– The point in which all three
circles intersect is the
earthquake epicenter
17. Types of Faults
” Strike-slip Fault
– Earth’s plates move sideways to one another
– Creates a shear force
– Rocks on either side of the fault surface are
moving past each other without much upward
or downward movement”.
18. Q: Where are earthquakes most prone to occur?
A: ‘’There is no technology available in any part
of the world to determine the place, time, or
magnitude, of an earthquake. However, they
are most likely to occur where the plates meet.
They are most prone to the fault line of the
plates. Because the plates are in constant
motion.
19. Q:Where Do Earthquakes Occur and
How Often?
A: 80% of all earthquakes occur in
the circum-Pacific belt
– most of these result from
convergent margin activity
– ~15% occur in the
Mediterranean-Asiatic belt
– remaining 5% occur in the
interiors of plates and on
spreading ridge centers
– more than 150,000 quakes
strong enough to be felt are
recorded each year
20. •Record seismic waves
•A drum with a sheet
of paper vibrates and
a stationary pen
marks the vibrations
on the paper
•The height of the
lines are used to
measure the energy
released from the
earthquake called the
magnitude
•The magnitude of
Sikkim Earthquake
was 6.9 on Richter
Scale
Seismograph
22. Q:What are Seismic Waves?
A: Response of material to the arrival of
energy fronts released by rupture. Two
types:
– Body waves
• P and S
– Surface waves
• R and L
23. Body Waves: P and S waves
• Body waves
– P or primary waves
• fastest waves
• travel through solids,
liquids, or gases
• compressional wave,
material movement is
in the same direction
as wave movement
– S or secondary waves
• slower than P waves
• travel through solids
only
• shear waves - move
material
perpendicular to wave
movement
24. Surface Waves: R and L waves
• Surface Waves
– Travel just below or along the ground’s surface
– Slower than body waves; rolling and side-to-
side movement
– Especially damaging to buildings
30. •Past seismicity of the region
Historical and instrumentally recorded data on earthquakes
show that the Sikkim and adjoining area lies in a region prone
to be affected by moderate to great earthquakes in the past.
Some noteworthy earthquakes that have affected the region
are:
Cachar earthquake of 10.01.1869 (M: 7.5),
Shillong plateau earthquake of 12.06.1897 (M: 8.7),
Dhubri earthquake of 02.07.1930 (M: 7.1),
Bihar-Nepal Border earthquake of 15.01.1934 (M: 8.3),
Arunachal Pradesh – China Border earthquake of 15.08.1950
(M: 8.5),
Nepal-India Border earthquake of 21.08.1988 (M: 6.4)
Sikkim earthquake of 14.02.2006 (M: 5.7)
Bhutan earthquake of 21.09.2009 (M:6.2)
33. Impact
Country Deaths Injured Displaced
Damaged
Houses /
Buildings
Partially
Damaged
Buildings
Total Loss
Billion US
Dollars
India 115 184 16500 15000 3,186 22.3
China 7 136 13790 156 2960 NA
Nepal 6 25 - 4360 2800 NA
Bhutan 1 16 - 6000 - NA
Bangladesh 0 - - - - NA
Total 129 - - - - -
34.
35. Landslides are one of the natural
hazards that affect
at least 15% of land area of our
country exceeding 0.49
million km2. Landslides of different
types occur frequently
in geodynamically active domains in
Himalaya,
36. Tremors
The strong tremor jolted buildings across northern and
eastern India, including Delhi, Uttar Pradesh,
Uttarakhand, Jharkhand, Bihar, West Bengal, Assam
and Mizoram, prompting people to run out of their
homes in panic.
37. Destruction from Earthquakes
Landslides
With many earthquakes, the greatest damage
to structures is from landslides and ground
subsidence, or the sinking of the ground triggered
by vibrations
Fire
In the San Francisco earthquake of 1906, most
of the destruction was caused by fires that
started when gas and electrical lines were cut.
38. Tsunami Movement: ~600 mph in deep water
~250 mph in medium depth water
~35 mph in shallow water
Movement of a Tsunami
39. Tsunamis
Caused by the movement of the ocean floor
– Causes a disruption in the water
– Some are so wide that a large ship can
travel over the wave without knowing
– Recent earthquake in the Indian Ocean
created a tsunamis that was 100 feet
high and moving at 500 mph
40. Nepal
The magnitude of the earthquake was
5.8Mw in the region.
Bangladesh
Earthquake was 10 km (6.2 miles) deep.
41. The Economics and Societal Impacts of EQs
Damage in Oakland, CA,
1989
• Building collapse
• Fire
• Tsunami
• Ground failure
42. Effects of EQ on Sikkim Govt.
1. The Sikkim Government has disbursed Rs 14.21 crore
(142 million Rs)
as relief among quake-hit people in Sikkim.
2. The India govt. has asked seismic experts from the
IIT-Roorkee to conduct "earthquake impact studies" at
the dam sites of state-owned NHPC Ltd and North
Eastern Electric Power Corp. Ltd (Neepco).
4.Many roads are blocked by landslides
5. Indian Prime Minister Manmohan Singh immediately
convened a meeting of the National Disaster Management
Authority Chamling to express his full support.
6. The Indian Air Force flew five cargo planes with relief
material and rescue personnel
for deployment in West Bengal and Sikkim.