The 1906 San Francisco earthquake struck Northern California on April 18th with a magnitude of 7.8. Over 3,000 people were killed and 80% of San Francisco was destroyed by the earthquake and subsequent fires. The earthquake was caused by movement along the San Andreas Fault, where the Pacific and North American tectonic plates meet. Survivors were left homeless and faced hardship as the city worked to recover from the devastating natural disaster.
Barcelona Study Tour Abroad Research PaperDaryl Kern
Can Architecture Affect Positive Social Change in Port Cities? The Barcelona Model: A Case Study of Applying Micro-scale Solutions to Waterfront Renewal Projects
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Essay on The Epicenter of an Earthquake
Earthquakes can devastate a city. They are a force of nature that can destroy any structure. The earth is made up of moving tectonic plates. Earthquakes occur along or near tectonic plate boundaries where two plates meet. These plates are solid rock and sit on the mantle which is a layer of molten rock. This molten rock is constantly moving in a convection current. The earth s core is what generates the heat. The hotter rock rises away from the core and pushes up against the crust. Here it cools and then moves away on both sides. The now cooled rock sinks back to take the place of the hotter rock that has risen as shown in the diagram on the right. When the rock pushes against the crust it moves sideways. This moves the tectonic plates...show more content...As shown in the diagram on the right, the fault runs straight through San Francisco and right along the coast. When the two plates slide along they create huge quakes that shake the ground. There have been many earthquakes generated from this fault line but the worst one was in 1906.
At 5:12 am on the 18th of April 1906 in San Francisco the foreshock hit the slumbering city. The force of the earthquake was so great that the tremors were felt right throughout the San Francisco and it reached as far inland as Nevada (500km away). Along the San Andreas fault the plate slipped up to 21 feet. 20 seconds after the initial foreshock the main earthquake hit, lasting for about 1 minute. Although it lasted for merely a minute it wrecked mass destruction. After the quake people walked the streets confused. Some people had no idea how much damage had been done. Some people walked to work as per usual only
An earthquake also known as a quake, tremor or temblor is the perceptible shaking of the surface of the Earth, which can be violent enough to destroy major buildings and kill thousands of people. The severity of the shaking can range from barely felt to violent enough to toss people around. Earthquakes have destroyed whole cities. They result from the sudden release of energy in the Earth's crust that creates seismic waves. The seismicity, seismism or seismic activity of an area refers to the frequency, type and size of earthquakes experienced over a period of time.
Earthquakes, (also known as quakes or a tremors) are violent movements of the rocks in the Earth's crust.
Earthquakes are usually quite brief, but may repeat over a period of time. They are the result of a sudden release of energy in the Earth's crust. This creates seismic waves, which are waves of energy that travel through the Earth. The study of earthquakes is called seismology. Seismology studies the frequency, type and size of earthquakes over a period of time.
There are large earthquakes and small earthquakes. Large earthquakes can take down buildings and cause death and injury. Earthquakes are measured using observations from seismometers. The magnitude of an earthquake, and the intensity of shaking, is usually reported on the Richter scale. On the scale, 3 or less is scarcely noticeable, and magnitude 7 (or more) causes damage over a wide area.
An earthquake under the ocean can cause a tsunami. This can cause just as much death and destruction as the earthquake itself. Landslides can happen, too. This is an important part of the Earth's rock cycle.
Multi-source connectivity as the driver of solar wind variability in the heli...Sérgio Sacani
The ambient solar wind that flls the heliosphere originates from multiple
sources in the solar corona and is highly structured. It is often described
as high-speed, relatively homogeneous, plasma streams from coronal
holes and slow-speed, highly variable, streams whose source regions are
under debate. A key goal of ESA/NASA’s Solar Orbiter mission is to identify
solar wind sources and understand what drives the complexity seen in the
heliosphere. By combining magnetic feld modelling and spectroscopic
techniques with high-resolution observations and measurements, we show
that the solar wind variability detected in situ by Solar Orbiter in March
2022 is driven by spatio-temporal changes in the magnetic connectivity to
multiple sources in the solar atmosphere. The magnetic feld footpoints
connected to the spacecraft moved from the boundaries of a coronal hole
to one active region (12961) and then across to another region (12957). This
is refected in the in situ measurements, which show the transition from fast
to highly Alfvénic then to slow solar wind that is disrupted by the arrival of
a coronal mass ejection. Our results describe solar wind variability at 0.5 au
but are applicable to near-Earth observatories.
Nutraceutical market, scope and growth: Herbal drug technologyLokesh Patil
As consumer awareness of health and wellness rises, the nutraceutical market—which includes goods like functional meals, drinks, and dietary supplements that provide health advantages beyond basic nutrition—is growing significantly. As healthcare expenses rise, the population ages, and people want natural and preventative health solutions more and more, this industry is increasing quickly. Further driving market expansion are product formulation innovations and the use of cutting-edge technology for customized nutrition. With its worldwide reach, the nutraceutical industry is expected to keep growing and provide significant chances for research and investment in a number of categories, including vitamins, minerals, probiotics, and herbal supplements.
Introduction:
RNA interference (RNAi) or Post-Transcriptional Gene Silencing (PTGS) is an important biological process for modulating eukaryotic gene expression.
It is highly conserved process of posttranscriptional gene silencing by which double stranded RNA (dsRNA) causes sequence-specific degradation of mRNA sequences.
dsRNA-induced gene silencing (RNAi) is reported in a wide range of eukaryotes ranging from worms, insects, mammals and plants.
This process mediates resistance to both endogenous parasitic and exogenous pathogenic nucleic acids, and regulates the expression of protein-coding genes.
What are small ncRNAs?
micro RNA (miRNA)
short interfering RNA (siRNA)
Properties of small non-coding RNA:
Involved in silencing mRNA transcripts.
Called “small” because they are usually only about 21-24 nucleotides long.
Synthesized by first cutting up longer precursor sequences (like the 61nt one that Lee discovered).
Silence an mRNA by base pairing with some sequence on the mRNA.
Discovery of siRNA?
The first small RNA:
In 1993 Rosalind Lee (Victor Ambros lab) was studying a non- coding gene in C. elegans, lin-4, that was involved in silencing of another gene, lin-14, at the appropriate time in the
development of the worm C. elegans.
Two small transcripts of lin-4 (22nt and 61nt) were found to be complementary to a sequence in the 3' UTR of lin-14.
Because lin-4 encoded no protein, she deduced that it must be these transcripts that are causing the silencing by RNA-RNA interactions.
Types of RNAi ( non coding RNA)
MiRNA
Length (23-25 nt)
Trans acting
Binds with target MRNA in mismatch
Translation inhibition
Si RNA
Length 21 nt.
Cis acting
Bind with target Mrna in perfect complementary sequence
Piwi-RNA
Length ; 25 to 36 nt.
Expressed in Germ Cells
Regulates trnasposomes activity
MECHANISM OF RNAI:
First the double-stranded RNA teams up with a protein complex named Dicer, which cuts the long RNA into short pieces.
Then another protein complex called RISC (RNA-induced silencing complex) discards one of the two RNA strands.
The RISC-docked, single-stranded RNA then pairs with the homologous mRNA and destroys it.
THE RISC COMPLEX:
RISC is large(>500kD) RNA multi- protein Binding complex which triggers MRNA degradation in response to MRNA
Unwinding of double stranded Si RNA by ATP independent Helicase
Active component of RISC is Ago proteins( ENDONUCLEASE) which cleave target MRNA.
DICER: endonuclease (RNase Family III)
Argonaute: Central Component of the RNA-Induced Silencing Complex (RISC)
One strand of the dsRNA produced by Dicer is retained in the RISC complex in association with Argonaute
ARGONAUTE PROTEIN :
1.PAZ(PIWI/Argonaute/ Zwille)- Recognition of target MRNA
2.PIWI (p-element induced wimpy Testis)- breaks Phosphodiester bond of mRNA.)RNAse H activity.
MiRNA:
The Double-stranded RNAs are naturally produced in eukaryotic cells during development, and they have a key role in regulating gene expression .
Observation of Io’s Resurfacing via Plume Deposition Using Ground-based Adapt...Sérgio Sacani
Since volcanic activity was first discovered on Io from Voyager images in 1979, changes
on Io’s surface have been monitored from both spacecraft and ground-based telescopes.
Here, we present the highest spatial resolution images of Io ever obtained from a groundbased telescope. These images, acquired by the SHARK-VIS instrument on the Large
Binocular Telescope, show evidence of a major resurfacing event on Io’s trailing hemisphere. When compared to the most recent spacecraft images, the SHARK-VIS images
show that a plume deposit from a powerful eruption at Pillan Patera has covered part
of the long-lived Pele plume deposit. Although this type of resurfacing event may be common on Io, few have been detected due to the rarity of spacecraft visits and the previously low spatial resolution available from Earth-based telescopes. The SHARK-VIS instrument ushers in a new era of high resolution imaging of Io’s surface using adaptive
optics at visible wavelengths.
Richard's entangled aventures in wonderlandRichard Gill
Since the loophole-free Bell experiments of 2020 and the Nobel prizes in physics of 2022, critics of Bell's work have retreated to the fortress of super-determinism. Now, super-determinism is a derogatory word - it just means "determinism". Palmer, Hance and Hossenfelder argue that quantum mechanics and determinism are not incompatible, using a sophisticated mathematical construction based on a subtle thinning of allowed states and measurements in quantum mechanics, such that what is left appears to make Bell's argument fail, without altering the empirical predictions of quantum mechanics. I think however that it is a smoke screen, and the slogan "lost in math" comes to my mind. I will discuss some other recent disproofs of Bell's theorem using the language of causality based on causal graphs. Causal thinking is also central to law and justice. I will mention surprising connections to my work on serial killer nurse cases, in particular the Dutch case of Lucia de Berk and the current UK case of Lucy Letby.
Earliest Galaxies in the JADES Origins Field: Luminosity Function and Cosmic ...Sérgio Sacani
We characterize the earliest galaxy population in the JADES Origins Field (JOF), the deepest
imaging field observed with JWST. We make use of the ancillary Hubble optical images (5 filters
spanning 0.4−0.9µm) and novel JWST images with 14 filters spanning 0.8−5µm, including 7 mediumband filters, and reaching total exposure times of up to 46 hours per filter. We combine all our data
at > 2.3µm to construct an ultradeep image, reaching as deep as ≈ 31.4 AB mag in the stack and
30.3-31.0 AB mag (5σ, r = 0.1” circular aperture) in individual filters. We measure photometric
redshifts and use robust selection criteria to identify a sample of eight galaxy candidates at redshifts
z = 11.5 − 15. These objects show compact half-light radii of R1/2 ∼ 50 − 200pc, stellar masses of
M⋆ ∼ 107−108M⊙, and star-formation rates of SFR ∼ 0.1−1 M⊙ yr−1
. Our search finds no candidates
at 15 < z < 20, placing upper limits at these redshifts. We develop a forward modeling approach to
infer the properties of the evolving luminosity function without binning in redshift or luminosity that
marginalizes over the photometric redshift uncertainty of our candidate galaxies and incorporates the
impact of non-detections. We find a z = 12 luminosity function in good agreement with prior results,
and that the luminosity function normalization and UV luminosity density decline by a factor of ∼ 2.5
from z = 12 to z = 14. We discuss the possible implications of our results in the context of theoretical
models for evolution of the dark matter halo mass function.
Seminar of U.V. Spectroscopy by SAMIR PANDASAMIR PANDA
Spectroscopy is a branch of science dealing the study of interaction of electromagnetic radiation with matter.
Ultraviolet-visible spectroscopy refers to absorption spectroscopy or reflect spectroscopy in the UV-VIS spectral region.
Ultraviolet-visible spectroscopy is an analytical method that can measure the amount of light received by the analyte.
2. HOW THE DISASTER SHOOK AMERICA
108 years later the San Francisco earthquake still stands as America’s worst
natural disaster in history. With over 3 000 fatalities and almost 10 000 injuries it
was a devastating experience for many. This brutal disaster left 400 000
homeless and many faced difficulty and hardship for several days.
3. THE EARTHQUAKE
The San Francisco Earthquake of 1906 hit San Francisco and Northern
California on Wednesday, April 18th at 5:12am. The earthquake itself lasted for
less than a minute, but it came with multiple uncontrollable fires that lasted for
days. Because of this, there was an estimated 3 000 fatalities and over 80% of
San Francisco was brutally destroyed. The survivors whose homes where
destroyed slept in tents in city parks, stood in long lines for food, and were
required to do their cooking in the street to minimize the threat of additional
fires. The San Francisco earthquake is one of the worst natural disasters in U.S.
history.
5. HOW THE EARTHQUAKE STARTED
The North American plate, and the Pacific plate boundaries form what is
called the San Andreas Fault. The Pacific plate is slowly moving northward,
and is "locked" at the areas around Los Angeles and San Francisco. The
central part of California’s plates are constantly moving 3/4 of an inch per
year (1.9 Cm). The plate boundaries that are "locked", build up pressure and
suddenly release causing a rough shake called an earthquake.
6. TECTONIC PLATES
There are 3 primary types of Tectonic Plate Boundaries; Divergent,
Convergent and Transform. To understand the boundaries, you must
understand what each word means. Divergent means pulling apart,
Convergent means coming together and transform is sliding against.
At divergent boundaries new crust is created as one or more plates pull away
from each other. Oceans are born and grow wider where plates diverge or
pull apart.
A convergent boundary is an actively deforming region where two or more
tectonic plates below earth’s surface move toward one another and collide.
As a result of pressure and friction, earthquakes and volcanoes are common
near convergent boundaries
Transform Boundaries are where two plates are sliding horizontally against one
another. These are also known as transform boundaries or more commonly as
faults. The San Francisco earthquake was caused by the Transform Boundaries.
8. MAGNITUDE, LOCATION
The magnitude of an earthquake shows you how rough of a shake it was. The
scale ranges from 1-10; 1 being the least violent and 10 being very violent. The
San Francisco earthquake hit with a powerful 7.8 magnitude. The epicenter of
the shake was 2 miles off the coast of San Francisco near Mussel Rock. The
shake was felt from Oregon to Los Angeles and all the way to Nevada.
Despite the mass of the earthquake, there was no after-shocks or tsunamis.
9.
10. THE SURFACE OF THE EARTH IS CONSTANTLY
CHANGING
Everyday, Earth’s plates are constantly moving and changing. Some changes
are less obvious while others are clearly moving. When the plates move, it
changes the earth because the plates are no longer in their previous position.
The changing of earth can take place in multiple ways such as weathering,
volcanos, earthquakes and erosions. As a result, the earth is always finding
new ways to change and move.
