This document discusses faults and earthquakes. It begins by defining an objective to describe the three types of faults and how they relate to stress. It then discusses normal faults which occur during extension and form where the hanging wall moves down. It also discusses thrust faults which occur during compression and form where the hanging wall moves up. Strike-slip faults are described where the fault blocks move horizontally past each other. The document concludes with tasks for students to complete fault simulations and assess their understanding of faults and earthquakes.
Comparing Evolved Extractive Text Summary Scores of Bidirectional Encoder Rep...University of Maribor
Slides from:
11th International Conference on Electrical, Electronics and Computer Engineering (IcETRAN), Niš, 3-6 June 2024
Track: Artificial Intelligence
https://www.etran.rs/2024/en/home-english/
The ability to recreate computational results with minimal effort and actionable metrics provides a solid foundation for scientific research and software development. When people can replicate an analysis at the touch of a button using open-source software, open data, and methods to assess and compare proposals, it significantly eases verification of results, engagement with a diverse range of contributors, and progress. However, we have yet to fully achieve this; there are still many sociotechnical frictions.
Inspired by David Donoho's vision, this talk aims to revisit the three crucial pillars of frictionless reproducibility (data sharing, code sharing, and competitive challenges) with the perspective of deep software variability.
Our observation is that multiple layers — hardware, operating systems, third-party libraries, software versions, input data, compile-time options, and parameters — are subject to variability that exacerbates frictions but is also essential for achieving robust, generalizable results and fostering innovation. I will first review the literature, providing evidence of how the complex variability interactions across these layers affect qualitative and quantitative software properties, thereby complicating the reproduction and replication of scientific studies in various fields.
I will then present some software engineering and AI techniques that can support the strategic exploration of variability spaces. These include the use of abstractions and models (e.g., feature models), sampling strategies (e.g., uniform, random), cost-effective measurements (e.g., incremental build of software configurations), and dimensionality reduction methods (e.g., transfer learning, feature selection, software debloating).
I will finally argue that deep variability is both the problem and solution of frictionless reproducibility, calling the software science community to develop new methods and tools to manage variability and foster reproducibility in software systems.
Exposé invité Journées Nationales du GDR GPL 2024
Richard's aventures in two entangled wonderlandsRichard 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.
Phenomics assisted breeding in crop improvementIshaGoswami9
As the population is increasing and will reach about 9 billion upto 2050. Also due to climate change, it is difficult to meet the food requirement of such a large population. Facing the challenges presented by resource shortages, climate
change, and increasing global population, crop yield and quality need to be improved in a sustainable way over the coming decades. Genetic improvement by breeding is the best way to increase crop productivity. With the rapid progression of functional
genomics, an increasing number of crop genomes have been sequenced and dozens of genes influencing key agronomic traits have been identified. However, current genome sequence information has not been adequately exploited for understanding
the complex characteristics of multiple gene, owing to a lack of crop phenotypic data. Efficient, automatic, and accurate technologies and platforms that can capture phenotypic data that can
be linked to genomics information for crop improvement at all growth stages have become as important as genotyping. Thus,
high-throughput phenotyping has become the major bottleneck restricting crop breeding. Plant phenomics has been defined as the high-throughput, accurate acquisition and analysis of multi-dimensional phenotypes
during crop growing stages at the organism level, including the cell, tissue, organ, individual plant, plot, and field levels. With the rapid development of novel sensors, imaging technology,
and analysis methods, numerous infrastructure platforms have been developed for phenotyping.
Salas, V. (2024) "John of St. Thomas (Poinsot) on the Science of Sacred Theol...Studia Poinsotiana
I Introduction
II Subalternation and Theology
III Theology and Dogmatic Declarations
IV The Mixed Principles of Theology
V Virtual Revelation: The Unity of Theology
VI Theology as a Natural Science
VII Theology’s Certitude
VIII Conclusion
Notes
Bibliography
All the contents are fully attributable to the author, Doctor Victor Salas. Should you wish to get this text republished, get in touch with the author or the editorial committee of the Studia Poinsotiana. Insofar as possible, we will be happy to broker your contact.
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.
hematic appreciation test is a psychological assessment tool used to measure an individual's appreciation and understanding of specific themes or topics. This test helps to evaluate an individual's ability to connect different ideas and concepts within a given theme, as well as their overall comprehension and interpretation skills. The results of the test can provide valuable insights into an individual's cognitive abilities, creativity, and critical thinking skills
Deep Behavioral Phenotyping in Systems Neuroscience for Functional Atlasing a...Ana Luísa Pinho
Functional Magnetic Resonance Imaging (fMRI) provides means to characterize brain activations in response to behavior. However, cognitive neuroscience has been limited to group-level effects referring to the performance of specific tasks. To obtain the functional profile of elementary cognitive mechanisms, the combination of brain responses to many tasks is required. Yet, to date, both structural atlases and parcellation-based activations do not fully account for cognitive function and still present several limitations. Further, they do not adapt overall to individual characteristics. In this talk, I will give an account of deep-behavioral phenotyping strategies, namely data-driven methods in large task-fMRI datasets, to optimize functional brain-data collection and improve inference of effects-of-interest related to mental processes. Key to this approach is the employment of fast multi-functional paradigms rich on features that can be well parametrized and, consequently, facilitate the creation of psycho-physiological constructs to be modelled with imaging data. Particular emphasis will be given to music stimuli when studying high-order cognitive mechanisms, due to their ecological nature and quality to enable complex behavior compounded by discrete entities. I will also discuss how deep-behavioral phenotyping and individualized models applied to neuroimaging data can better account for the subject-specific organization of domain-general cognitive systems in the human brain. Finally, the accumulation of functional brain signatures brings the possibility to clarify relationships among tasks and create a univocal link between brain systems and mental functions through: (1) the development of ontologies proposing an organization of cognitive processes; and (2) brain-network taxonomies describing functional specialization. To this end, tools to improve commensurability in cognitive science are necessary, such as public repositories, ontology-based platforms and automated meta-analysis tools. I will thus discuss some brain-atlasing resources currently under development, and their applicability in cognitive as well as clinical neuroscience.
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.
The use of Nauplii and metanauplii artemia in aquaculture (brine shrimp).pptxMAGOTI ERNEST
Although Artemia has been known to man for centuries, its use as a food for the culture of larval organisms apparently began only in the 1930s, when several investigators found that it made an excellent food for newly hatched fish larvae (Litvinenko et al., 2023). As aquaculture developed in the 1960s and ‘70s, the use of Artemia also became more widespread, due both to its convenience and to its nutritional value for larval organisms (Arenas-Pardo et al., 2024). The fact that Artemia dormant cysts can be stored for long periods in cans, and then used as an off-the-shelf food requiring only 24 h of incubation makes them the most convenient, least labor-intensive, live food available for aquaculture (Sorgeloos & Roubach, 2021). The nutritional value of Artemia, especially for marine organisms, is not constant, but varies both geographically and temporally. During the last decade, however, both the causes of Artemia nutritional variability and methods to improve poorquality Artemia have been identified (Loufi et al., 2024).
Brine shrimp (Artemia spp.) are used in marine aquaculture worldwide. Annually, more than 2,000 metric tons of dry cysts are used for cultivation of fish, crustacean, and shellfish larva. Brine shrimp are important to aquaculture because newly hatched brine shrimp nauplii (larvae) provide a food source for many fish fry (Mozanzadeh et al., 2021). Culture and harvesting of brine shrimp eggs represents another aspect of the aquaculture industry. Nauplii and metanauplii of Artemia, commonly known as brine shrimp, play a crucial role in aquaculture due to their nutritional value and suitability as live feed for many aquatic species, particularly in larval stages (Sorgeloos & Roubach, 2021).
DERIVATION OF MODIFIED BERNOULLI EQUATION WITH VISCOUS EFFECTS AND TERMINAL V...Wasswaderrick3
In this book, we use conservation of energy techniques on a fluid element to derive the Modified Bernoulli equation of flow with viscous or friction effects. We derive the general equation of flow/ velocity and then from this we derive the Pouiselle flow equation, the transition flow equation and the turbulent flow equation. In the situations where there are no viscous effects , the equation reduces to the Bernoulli equation. From experimental results, we are able to include other terms in the Bernoulli equation. We also look at cases where pressure gradients exist. We use the Modified Bernoulli equation to derive equations of flow rate for pipes of different cross sectional areas connected together. We also extend our techniques of energy conservation to a sphere falling in a viscous medium under the effect of gravity. We demonstrate Stokes equation of terminal velocity and turbulent flow equation. We look at a way of calculating the time taken for a body to fall in a viscous medium. We also look at the general equation of terminal velocity.
Travis Hills' Endeavors in Minnesota: Fostering Environmental and Economic Pr...Travis Hills MN
Travis Hills of Minnesota developed a method to convert waste into high-value dry fertilizer, significantly enriching soil quality. By providing farmers with a valuable resource derived from waste, Travis Hills helps enhance farm profitability while promoting environmental stewardship. Travis Hills' sustainable practices lead to cost savings and increased revenue for farmers by improving resource efficiency and reducing waste.
ANAMOLOUS SECONDARY GROWTH IN DICOT ROOTS.pptxRASHMI M G
Abnormal or anomalous secondary growth in plants. It defines secondary growth as an increase in plant girth due to vascular cambium or cork cambium. Anomalous secondary growth does not follow the normal pattern of a single vascular cambium producing xylem internally and phloem externally.
2. Kumusta ka?
On a scale
of 1 to 5,
kindly
share to us
how do you
feel today
☺
3. Curiosities Activities
OBJECTIVES:
1. Define fault and explain how it is formed.
2. Describe the three types of fault and relate the types of
stress associated with each type.
3. Describe the effects of bending of rocks along faults.
4. Simulate how movements along faults generate
earthquakes using models.
4. A V D V G T E I T K J E
M S H A K E F R U D S V
O B T P C O O Q M Z U I
V W D R I M L P B U D T
E M K A E J E S L F D C
M V I R D S Q D E Y E U
E I T O U C S B P H N R
N X J N Z R Y O K L F T
T U G V I O L E N T P S
O S H O C K B N I L R E
E D N O I T A R B I V D
5. A V D V G T E I T K J E
M S H A K E F R U D S V
O B T P C O O Q M Z U I
V W D R I M L P B U D T
E M K A E J E S L F D C
M V I R D S Q D E Y E U
E I T O U C S B P H N R
N X J N Z R Y O K L F T
T U G V I O L E N T P S
O S H O C K B N I L R E
E D N O I T A R B I V D
v
v
6. The words from the puzzle are related to this
this geologic event. What is it?
7. E A R T H Q U A K E
The words from the puzzle are related to this
this geologic event. What is it?
8. ❑Have you experience an Earthquake?
When did you experience it?
❑What did you feel when the earthquake
happens?
❑What did you do while it is occurring?
❑What did you do after the earthquake?
Earthquake and I
9. Try It: Fault in Paper
Material: Paper
CAUTION: BE CAREFUL IN DOING THE ACTIVITY TO AVOID PAPER CUT WOUND.
Procedure:
1. Get a piece of paper.
2. Hold the paper with two hands. Try to pull the paper apart from each
other. Write and draw your observation on the table below.
3. Get another piece of paper. Place it on smooth surface. Place your
hands on the top of the paper. Push your left hand while pull your right
hand. You can used strong force. Observe what happen.
4. Using another sheet of paper, try to push the paper from the sides to
the center. What happen?
5. Do not throw the paper immediately. Place it on smooth surface.
10.
11. Questions
1. What happen to the paper as you pull it
apart, slide it and push it towards its
center?
2. When you exert forces on the paper as
you perform the activity, you can see that
there are changes in the paper. What is
the common change that you see on the
papers?
3. Does your paper tear? If yes, try to put
the paper back together. What does it look
like?
4. When you placed the tear papers back
together, you can see crack on the paper
and that could be similar to the fault
found on the large blocks on earth. How
would you describe a fault?
12. Questions
1. What happen to the paper as you pull it apart, slide it and push it towards
its center? If force is enough the paper will tear apart or crumpled.
2. When you exert forces on the paper as you perform the activity, you can
see that there are changes in the paper. What is the common change that
you see on the papers?
3. Does your paper tear? If yes try to put the paper back together. What does
it look like?
4. When you placed the tear papers back together, you can see crack on the
paper and that could be similar to the fault found on the large blocks on
earth. How would you describe a fault?
13. Questions
1. What happen to the paper as you pull it apart, slide it and push it towards
its center? If force is enough the paper will tear apart or crumpled.
2. When you exert forces on the paper as you perform the activity, you can
see that there are changes in the paper. What is the common change that
you see on the papers? There is tear or crumple.
3. Does your paper tear? If yes try to put the paper back together. What does
it look like?
4. When you placed the tear papers back together, you can see crack on the
paper and that could be similar to the fault found on the large blocks on
earth. How would you describe a fault?
14. Questions
1. What happen to the paper as you pull it apart, slide it and push it towards
its center? If force is enough the paper will tear apart or crumpled.
2. When you exert forces on the paper as you perform the activity, you can
see that there are changes in the paper. What is the common change that
you see on the papers? There is tear or crumple.
3. Does your paper tear? If yes try to put the paper back together. What does
it look like? Yes, there is a crack in it.
4. When you placed the tear papers back together, you can see crack on the
paper and that could be similar to the fault found on the large blocks on
earth. How would you describe a fault?
15. Questions
1. What happen to the paper as you pull it apart, slide it and push it towards
its center? If force is enough the paper will tear apart or crumpled.
2. When you exert forces on the paper as you perform the activity, you can
see that there are changes in the paper. What is the common change that
you see on the papers? There is tear or crumple.
3. Does your paper tear? If yes try to put the paper back together. What does
it look like? Yes, there is a crack in it.
4. When you placed the tear papers back together, you can see crack on the
paper and that could be similar to the fault found on the large blocks on
earth. How would you describe a fault? Fault is a crack that separate the
two large block of rock
16. What do you expect about earthquake?
✓Movements of the ground
or rocks.
Earthquake
✓Movements may come in
different directions.
17. Because of tremendous
movement or friction
between rocks, it leaves a
crack or fracture along the
earth’s surface called
Fault
18. Faults
❖ A break, a crack or a
line along the earth’s
surface.
❖ A fracture on the earth’s
surface due rock mass
movement.
21. When do faults formed along the earth’s ground?
It may formed along the
earth’s surface if the force
acts on ground will exceed
on its limit.
Elastic Rebound Theory
22. Features of fault:
▪A fault divides rock into two fault blocks
▪ HANGING WALL
▪ FOOTWALL
23. Hanging wall vs Footwall
▪Hanging Wall is the
block positioned
over the fault
▪Foot Wall is the
block positioned
under it.
Hanging wall
Foot wall
26. NORMAL FAULTS (extensional
fault)
•occurs when the crust is
extended.
• The hanging wall moves
downward, relative to the
footwall.
•Form in regions of lateral
extension
27. EXAMPLES OF
NORMAL FAULTS
Conjugate Normal Faults,
Canyonlands National Park
darkwing.uoregon.edu/~millerm/conjN1.html
Normal Fault Scarps, Turkey
www.msnucleus.org/.../pt/hazards/4/pth4_1a.html
Outcrop scale normal faults
28. THRUST or REVERSE FAULTS
▪occur in areas undergoing
compression (squishing).
▪which the hanging wall
moves up relative to the
footwall
▪Form in regions of lateral
compression
29. EXAMPLES OF
THRUST
FAULTS
Thrust Fault in Concrete from 1964 Quake,
Anchorage, Alaska
www.ucmp.berkeley.edu/.../alaska/0709log.html
Thrust Fault in Sediments
www001.upp.so-net.ne.jp/fl-fg/05-01.htm
Outcrop scale thrust faults
www.pitt.edu/.../7Structures/ReverseFaults.html
30. • STRIKE-SLIP FAULTS
- where fault moves side by sides.
▪RIGHT-LATERAL (DEXTRAL)
FAULTS: Strike-slip faults
across which the block
moves to the right
▪LEFT-LATERAL (SINISTRAL)
FAULTS: Strike-slip faults
across which the block
moves to the left.
31. EXAMPLES OF
STRIKE-SLIP FAULTS
San Andreas Fault, CA
http://education.usgs.gov/california/
pp1515/chapter2/fig2-21.jpg
Right Lateral Slip, Izmit, Turkey, 1999 Quake
http://www.geo.uib.no/jordskjelv/
index.php?topic=earthquakes&lang=en
Right Lateral Fault in Asphalt
www.uwsp.edu/.../fault_transform_photo.html
32. ____________ occur on ____________. A ___________is
a thin zone of crushed rock separating blocks of the
earth's crust. When an/a____________ occurs on one
of these ____________, the rock on one side of the
____________ slips with respect to the other. ... The
____________ surface can be vertical, horizontal, or at
some angle to the surface of the earth.
Complete the passage about earthquake. Read and understand
the sentences. Indicate whether it is EARTHQUAKE or FAULT.
33. ____________ occur on ____________. A ___________is
a thin zone of crushed rock separating blocks of the
earth's crust. When a/an ____________ occurs on one
of these ____________, the rock on one side of the
____________ slips with respect to the other. ... The
____________ surface can be vertical, horizontal, or at
some angle to the surface of the earth.
Complete the passage about earthquake. Read and understand
the sentences. Indicate whether it is EARTHQUAKE or FAULT.
Earthquake Fault Fault
Fault
Earthquake
Fault
Fault
36. 1.Which of the following can cause the earth’s surface to
break and form a fault?
A. If the rock particles bounce with each other
B. If the rock particles get wet because it absorb
water underneath
C. If the rocks give in from the force because it
goes beyond its limit
D. if the rocks have different thickness
37. 2. Earthquake is the movement of the earth’s ground.
Which of the following statements BEST describes
the cause of earthquake?
A. Earthquake is due to the friction of the different
rocks inside the earth.
B. Earthquake is due to the amount of water absorb
by the ground.
C. Earthquake is due to the transferred energy coming
from the sun.
D. Earthquake is due to the absorb heat from the
atmosphere.
38. 3. It is the break on the earth’s ground due to
excessive force underneath
A. Earthquake
B. Fault
C. Foot wall
D. Hanging wall
39. 4. Study the diagram. If A is the hanging wall and
B is the foot wall, in which direction of forces
will cause the hanging wall to collapse downward?
A.
B.
C.
D.
40. 5. Study the diagram. If A is the hanging wall and
B is the foot wall, in which direction of forces
will cause the foot wall to collapse downward?
A.
B.
C.
D.
41. 1.Which of the following can cause the earth’s
surface to break and form a fault?
A. If the rock particles bounce with each other
B. If the rock particles get wet because it absorb
water underneath
C. If the rock gives in from the force because it
goes beyond its limit
D. if the rocks have different thickness
42. 2. Earthquake is the movement of the earth’s ground.
Which of the following statements BEST describes
the cause of earthquake?
A. Earthquake is due to the friction of the different
rocks inside the earth.
B. Earthquake is due to the amount of water absorb
by the ground.
C. Earthquake is due to the transferred energy coming
from the sun.
D. Earthquake is due to the absorb heat from the
atmosphere.
43. 3. It is the break on the earth’s ground due to
excessive force underneath.
A. Earthquake
B. Fault
C. Foot wall
D. Hanging wall
44. 4. From the diagram, if part A is the hanging wall and
the part B is the foot wall which direction of forces
caused the hanging wall to collapse downward?
A.
B.
C.
D.
45. 5. From the diagram, if part A is the hanging wall and
the part B is the foot wall which direction of forces
caused the foot wall to collapsed downward?
A.
B.
C.
D.
46. Have fun learning!
Home Study Tasks
Quarter 2, Week 1
Day 1
Online Class
Day 2
Modular Class
Day 3
Independent Learning
✓ Answer the Quarter 2
Pre-Test (check the link
posted in the Google
Classroom)
✓ Attend online class
✓ Watch the videos
related to the topic (links
are posted in the Google
Classroom)
✓ Do the following tasks:
1. Activity 1:
Creation of Faults
pp.5-6
2. Activity 3: The
Stresses and the
Faults pp.8-9
✓ Accomplish “What
I Can Do” (Part 1
only) p.11
47. Have fun learning!
Home Study Tasks
Quarter 2, Week 1
Day 1
Modular Class
Day 2
Online Class
Day 3
Independent Learning
✓ Answer the Quarter 2
Pre-Test (check the link
posted in the Google
Classroom)
✓ Watch the videos
related to the topic
(links are posted in the
Google Classroom)
✓ Attend online class
✓ Do the following tasks:
1. Activity 1:
Creation of Faults
pp.5-6
2. Activity 3: The
Stresses and the
Faults pp.8-9
✓ Accomplish
“What I Can Do”
(Part 1 only) p.11