this is one of my projects that I had made for my class X holiday homework, I hope this can help you gain some information about tsunamis and if you also want to make a project like this, I hope I have helped you. - mansvini
This is a PowerPoint Presentation based strictly on Tsunami.
Here one can find the following details about Tsunami:
Definition of Tsunami
Major Causes of Tsunami
Pictures Related to Tsunami
Analytical and Statistical information
And other more useful details .
So Hope you like it
Thankyou
this is one of my projects that I had made for my class X holiday homework, I hope this can help you gain some information about tsunamis and if you also want to make a project like this, I hope I have helped you. - mansvini
This is a PowerPoint Presentation based strictly on Tsunami.
Here one can find the following details about Tsunami:
Definition of Tsunami
Major Causes of Tsunami
Pictures Related to Tsunami
Analytical and Statistical information
And other more useful details .
So Hope you like it
Thankyou
Tsunami is a Japanese word Tsu means ‘harbour’ and nami means ‘wave’.
They are called tidal waves but they have actually nothing to do with the tides. However their appearance from shore is similar to rapidly rising or falling tides.
Tsunami is a series of wave created when water is moved very quickly.
Tsunami is gravity wave system, triggered by vertical disturbances in ocean. They are long waves sometime with hundreds of miles b/w their crests, just like the concentric waves generated by an object dropped into a pool.
First tsunami was recorded in 1480 B.C. in eastern Mediterranean, when the Minoan civilization was wiped out.
A large tsunami accompanied by the earthquake of Lisbon in 1755.
The Kutch earthquake of June 16, 1819 generated strong tsunami which submerged the coastal areas and damage to ships and country made boats of fishermen.
North and South American records have dated such
events back to 1788 for Alaska and 1562 for Chile. Records of Hawaiian tsunami go back to 1821.
Tsunami hits the Mona Passage off Puerto Rico in 1918, grand banks of Canada in 1929.
this is a presentation of cyclone.in this ppt, various types of cyclones are given.its effects, formation, different names, types, emergency response on cyclone is given
Tsunami is a Japanese word Tsu means ‘harbour’ and nami means ‘wave’.
They are called tidal waves but they have actually nothing to do with the tides. However their appearance from shore is similar to rapidly rising or falling tides.
Tsunami is a series of wave created when water is moved very quickly.
Tsunami is gravity wave system, triggered by vertical disturbances in ocean. They are long waves sometime with hundreds of miles b/w their crests, just like the concentric waves generated by an object dropped into a pool.
First tsunami was recorded in 1480 B.C. in eastern Mediterranean, when the Minoan civilization was wiped out.
A large tsunami accompanied by the earthquake of Lisbon in 1755.
The Kutch earthquake of June 16, 1819 generated strong tsunami which submerged the coastal areas and damage to ships and country made boats of fishermen.
North and South American records have dated such
events back to 1788 for Alaska and 1562 for Chile. Records of Hawaiian tsunami go back to 1821.
Tsunami hits the Mona Passage off Puerto Rico in 1918, grand banks of Canada in 1929.
this is a presentation of cyclone.in this ppt, various types of cyclones are given.its effects, formation, different names, types, emergency response on cyclone is given
A series of waves in a water body caused by the displacement of a large volume of water, generally in an ocean or a large lake. Earthquakes, volcanic eruptions and other underwater explosions (including detonations, landslides, glacier calvings, meteorite impacts and other disturbances) above or below water all have the potential to generate a tsunami. Unlike normal ocean waves, which are generated by wind, or tides, which are generated by the gravitational pull of the Moon and the Sun, a tsunami is generated by the displacement of water by a large event.
Natural farming @ Dr. Siddhartha S. Jena.pptxsidjena70
A brief about organic farming/ Natural farming/ Zero budget natural farming/ Subash Palekar Natural farming which keeps us and environment safe and healthy. Next gen Agricultural practices of chemical free farming.
"Understanding the Carbon Cycle: Processes, Human Impacts, and Strategies for...MMariSelvam4
The carbon cycle is a critical component of Earth's environmental system, governing the movement and transformation of carbon through various reservoirs, including the atmosphere, oceans, soil, and living organisms. This complex cycle involves several key processes such as photosynthesis, respiration, decomposition, and carbon sequestration, each contributing to the regulation of carbon levels on the planet.
Human activities, particularly fossil fuel combustion and deforestation, have significantly altered the natural carbon cycle, leading to increased atmospheric carbon dioxide concentrations and driving climate change. Understanding the intricacies of the carbon cycle is essential for assessing the impacts of these changes and developing effective mitigation strategies.
By studying the carbon cycle, scientists can identify carbon sources and sinks, measure carbon fluxes, and predict future trends. This knowledge is crucial for crafting policies aimed at reducing carbon emissions, enhancing carbon storage, and promoting sustainable practices. The carbon cycle's interplay with climate systems, ecosystems, and human activities underscores its importance in maintaining a stable and healthy planet.
In-depth exploration of the carbon cycle reveals the delicate balance required to sustain life and the urgent need to address anthropogenic influences. Through research, education, and policy, we can work towards restoring equilibrium in the carbon cycle and ensuring a sustainable future for generations to come.
Willie Nelson Net Worth: A Journey Through Music, Movies, and Business Venturesgreendigital
Willie Nelson is a name that resonates within the world of music and entertainment. Known for his unique voice, and masterful guitar skills. and an extraordinary career spanning several decades. Nelson has become a legend in the country music scene. But, his influence extends far beyond the realm of music. with ventures in acting, writing, activism, and business. This comprehensive article delves into Willie Nelson net worth. exploring the various facets of his career that have contributed to his large fortune.
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Introduction
Willie Nelson net worth is a testament to his enduring influence and success in many fields. Born on April 29, 1933, in Abbott, Texas. Nelson's journey from a humble beginning to becoming one of the most iconic figures in American music is nothing short of inspirational. His net worth, which estimated to be around $25 million as of 2024. reflects a career that is as diverse as it is prolific.
Early Life and Musical Beginnings
Humble Origins
Willie Hugh Nelson was born during the Great Depression. a time of significant economic hardship in the United States. Raised by his grandparents. Nelson found solace and inspiration in music from an early age. His grandmother taught him to play the guitar. setting the stage for what would become an illustrious career.
First Steps in Music
Nelson's initial foray into the music industry was fraught with challenges. He moved to Nashville, Tennessee, to pursue his dreams, but success did not come . Working as a songwriter, Nelson penned hits for other artists. which helped him gain a foothold in the competitive music scene. His songwriting skills contributed to his early earnings. laying the foundation for his net worth.
Rise to Stardom
Breakthrough Albums
The 1970s marked a turning point in Willie Nelson's career. His albums "Shotgun Willie" (1973), "Red Headed Stranger" (1975). and "Stardust" (1978) received critical acclaim and commercial success. These albums not only solidified his position in the country music genre. but also introduced his music to a broader audience. The success of these albums played a crucial role in boosting Willie Nelson net worth.
Iconic Songs
Willie Nelson net worth is also attributed to his extensive catalog of hit songs. Tracks like "Blue Eyes Crying in the Rain," "On the Road Again," and "Always on My Mind" have become timeless classics. These songs have not only earned Nelson large royalties but have also ensured his continued relevance in the music industry.
Acting and Film Career
Hollywood Ventures
In addition to his music career, Willie Nelson has also made a mark in Hollywood. His distinctive personality and on-screen presence have landed him roles in several films and television shows. Notable appearances include roles in "The Electric Horseman" (1979), "Honeysuckle Rose" (1980), and "Barbarosa" (1982). These acting gigs have added a significant amount to Willie Nelson net worth.
Television Appearances
Nelson's char
Micro RNA genes and their likely influence in rice (Oryza sativa L.) dynamic ...Open Access Research Paper
Micro RNAs (miRNAs) are small non-coding RNAs molecules having approximately 18-25 nucleotides, they are present in both plants and animals genomes. MiRNAs have diverse spatial expression patterns and regulate various developmental metabolisms, stress responses and other physiological processes. The dynamic gene expression playing major roles in phenotypic differences in organisms are believed to be controlled by miRNAs. Mutations in regions of regulatory factors, such as miRNA genes or transcription factors (TF) necessitated by dynamic environmental factors or pathogen infections, have tremendous effects on structure and expression of genes. The resultant novel gene products presents potential explanations for constant evolving desirable traits that have long been bred using conventional means, biotechnology or genetic engineering. Rice grain quality, yield, disease tolerance, climate-resilience and palatability properties are not exceptional to miRN Asmutations effects. There are new insights courtesy of high-throughput sequencing and improved proteomic techniques that organisms’ complexity and adaptations are highly contributed by miRNAs containing regulatory networks. This article aims to expound on how rice miRNAs could be driving evolution of traits and highlight the latest miRNA research progress. Moreover, the review accentuates miRNAs grey areas to be addressed and gives recommendations for further studies.
UNDERSTANDING WHAT GREEN WASHING IS!.pdfJulietMogola
Many companies today use green washing to lure the public into thinking they are conserving the environment but in real sense they are doing more harm. There have been such several cases from very big companies here in Kenya and also globally. This ranges from various sectors from manufacturing and goes to consumer products. Educating people on greenwashing will enable people to make better choices based on their analysis and not on what they see on marketing sites.
Artificial Reefs by Kuddle Life Foundation - May 2024punit537210
Situated in Pondicherry, India, Kuddle Life Foundation is a charitable, non-profit and non-governmental organization (NGO) dedicated to improving the living standards of coastal communities and simultaneously placing a strong emphasis on the protection of marine ecosystems.
One of the key areas we work in is Artificial Reefs. This presentation captures our journey so far and our learnings. We hope you get as excited about marine conservation and artificial reefs as we are.
Please visit our website: https://kuddlelife.org
Our Instagram channel:
@kuddlelifefoundation
Our Linkedin Page:
https://www.linkedin.com/company/kuddlelifefoundation/
and write to us if you have any questions:
info@kuddlelife.org
Characterization and the Kinetics of drying at the drying oven and with micro...Open Access Research Paper
The objective of this work is to contribute to valorization de Nephelium lappaceum by the characterization of kinetics of drying of seeds of Nephelium lappaceum. The seeds were dehydrated until a constant mass respectively in a drying oven and a microwawe oven. The temperatures and the powers of drying are respectively: 50, 60 and 70°C and 140, 280 and 420 W. The results show that the curves of drying of seeds of Nephelium lappaceum do not present a phase of constant kinetics. The coefficients of diffusion vary between 2.09.10-8 to 2.98. 10-8m-2/s in the interval of 50°C at 70°C and between 4.83×10-07 at 9.04×10-07 m-8/s for the powers going of 140 W with 420 W the relation between Arrhenius and a value of energy of activation of 16.49 kJ. mol-1 expressed the effect of the temperature on effective diffusivity.
WRI’s brand new “Food Service Playbook for Promoting Sustainable Food Choices” gives food service operators the very latest strategies for creating dining environments that empower consumers to choose sustainable, plant-rich dishes. This research builds off our first guide for food service, now with industry experience and insights from nearly 350 academic trials.
3. Project Overview
The aim of this presentation is to study about
tsunamis waves . How are they caused , their
characteristics and their impact. Through studying all
these we can learn about tsunami waves. As the
destruction due to these waves can’t be stopped but it
can be reduced to save the precious lives.
4. Intro..
The term tsunami comes from the Japanese,
meaning “harbor" (tsu) and “wave" (nami). Tsunami are
sometimes referred to as tidal waves. In recent years,
this term has fallen out of favor, especially in the
scientific community, because tsunami actually have
nothing to do with tides. Tsunami and tides both
produce waves of water that move inland, but in the
case of tsunami the inland movement of water is much
greater and lasts for a longer period, giving the
impression of an incredibly high tide.
5. Causes
Although most tsunamis are generated by
underwater earthquakes, a tsunami can be generated
when convergent or destructive plate boundaries
abruptly move and vertically displace the overlying
water. It is very unlikely that they can form at divergent
(constructive) or conservative plate boundaries. This is
because constructive or conservative boundaries do not
generally disturb the vertical displacement of the water
column. Subduction zone related earthquakes generate
the majority of tsunami.
6. Tsunamis have a small
amplitude (wave height) offshore,
and a very long wavelength (often
hundreds of kilometers long),
which is why they generally pass
unnoticed at sea, forming only a
slight swell usually about
300 millimetres (12 in) above the
normal sea surface. They grow in
height when they reach shallower
water, in a wave shoaling process.
A tsunami can occur in any tidal
state and even at low tide can still
inundate coastal areas.
7. Most tsunamis are caused by
submarine earthquakes which
dislocate the oceanic crust, pushing
water upwards.
Tsunami can also be generated by
erupting submarine volcanoes ejecting
magma into the ocean.
A gas bubble erupting in a deep
part of the ocean can also trigger a
tsunami.
8. Earthquake-Generated
Tsunami
An earthquake may generate a tsunami if the
quake:
• occurs just below a body of water,
• is of moderate or high magnitude, and
• displaces a large-enough volume of water.
9. Drawing of tectonic plate boundary
before earthquake.
Overriding plate bulges under strain,
causing tectonic uplift.
Plate slips, causing subsidence and
releasing energy into water.
The energy released produces
tsunami waves.
10. Characteristics
When the wave enters shallow water, it slows down
and its amplitude (height) increases. The wave further
slows and amplifies as it hits land. Only the largest waves
crest.
As the tsunami approaches the coast and the waters
become shallow , wave shoaling compresses the wave
and its velocity slows below 50 miles per hour. Its
wavelength diminishes to less than 12 miles and its
amplitude grows enormously , producing a distinctively
visible wave. Since the wave still has such a long
wavelength , the tsunami may take minutes to reach full
height .
11. When the tsunami's wave peak reaches the
shore, the resulting temporary rise in sea level is
termed run up. Run up is measured in meters
above a reference sea level. A large tsunami may
feature multiple waves arriving over a period of
hours, with significant time between the wave
crests. The first wave to reach the shore may not
have the highest run up.
About 80% of tsunamis occur in the Pacific
Ocean, but are possible wherever there are large
bodies of water, including lakes. They may be
caused by landslides, volcanic explosions, bolides
and seismic activity.
12. Drawback
If the first part of a tsunami to reach land is a trough—
called a drawback—rather than a wave crest, the water
along the shoreline recedes dramatically, exposing
normally submerged areas.
A drawback occurs because the tectonic plate on one
side of the fault sinks suddenly during the earthquake,
causing the overlaying water to propagate outwards with
the trough of the wave at its front. This is also why that
there would not be any drawback when the tsunami
travelling on the other side arrives ashore, as the tectonic
plate is "raised" on that side of the fault line.
13. Drawback begins before the wave arrives at an
interval equal to half of the wave's period. If the slope
of the coastal seabed is small, drawback can exceed
hundreds of meters. People unaware of the danger
sometimes remain near the shore to satisfy their
curiosity or to collect fish from the exposed seabed.
During the Indian Ocean tsunami, the sea withdrew
and many people went onto the exposed sea bed to
investigate.
14. 2004 Indian Ocean Tsunami The 2004 Indian Ocean tsunami killed over 200,000
people with many bodies either being lost to the sea or
unidentified.
According to an article in Geographical magazine
(April 2008), the Indian Ocean tsunami of December 26,
2004 was not the worst that the region could expect.
Professor Costas Synolakis of the Tsunami Research
Center at the University of Southern California co-
authored a paper in Geophysical Journal International
which suggests that a future tsunami in the Indian Ocean
basin could affect locations such as Madagascar,
Singapore, Somalia, Western Australia.
15.
16. Conclusion
In conclusion, I would like to tell tsunamis can be
very dangerous and deadly. As we do not have the
power to control or predict and detect tsunamis
because they are under water waves they become even
more dangerous and deadly and make them even more
difficult to escape. Tsunamis can damage a lot of
property and life and usually leave a panic for the
human basic necessities. So they are not a thing to be
taken lightly.
17. Bibliography
I would like to mention some sources which proved
to be helpful in making this presentation. Some of
them are as follows :
i. www.google.com
ii. www.wikipedia.com
iii. The Times Of India (newspaper)
iv. Google Images
