GOAL: To create a poster that explains the phenomena of blue sky using the concept of wavelength and frequency of visible light.
SITUATION: As the creative head in the science club of Macasandig National High School, you are tasked to create a poster showcasing the phenomena of blue sky on Science Club bulletin board.
PRODUCT: A creative poster explains the phenomena of blue sky. The poster should be in 1/8 illustration board.
faults generate earthquakes.
S8ES-IIa- 14
Objectives:
1. Describe what fault is and how these faults related to earthquakes.
2. Determine the extent of damage an earthquake can do in a particular location.
Article Reading
Earthquake wreaks havoc in the Philippines more than 1,000 people are killed when a 7.7-magnitude earthquake strikes Luzon Island in the Philippines on this day in 1990. The massive tremor wreaked havoc across a sizeable portion of Luzon, the country’s largest island, with Baguio City suffering the most devastating effects.
The epicenter of the quake, which struck at 4:26 p.m., was north of Manila in the Nueva Ecija province. Reports indicate that the shaking went on for nearly a full minute. Collapsing buildings were the main cause of damage and death. Getting out of a multi-story building was a good safety precaution that afternoon, although many people were injured and a few even died in stampedes of others doing the same thing.
At Christian College, a six-story building completely collapsed, trapping approximately 250 students and teachers inside. Heroic rescue efforts saved many, but some victims who did not die in the collapse were found dead later from dehydration because they were not pulled out in time.
All types of buildings, including several resort hotels in Baguio, known as the
Philippines’ Summer Capital, suffered tremendous damage. Most of the city’s 100,000
residents slept outdoors that evening and during the following week, afraid to return to
their homes amid the frequent aftershocks. For days, workers pulled bodies from the
demolished buildings in Baguio. The best estimate is that 1,000 bodies were eventually
recovered. At least another 1,000 people suffered serious injuries. Rescue efforts were
hampered severely because the three main roads into the city were blocked by landslides. Hundreds of motorists were stranded on the roads as well.
A fault is a fracture or zone of fractures between two blocks of
rock. Faults allow the blocks to move relative to each other.
This movement may occur rapidly, in the form of an earthquake - or may occur slowly, in the form of creep. Faults may range in length from a few millimeters to thousands of kilometers. Most faults produce repeated displacements over geologic time.
The ground in the area of fault tends to remain not moving
because of frictional force between the two opposing plates (boxes). As stronger forces (rubber band) shakes up the fault, the friction (tape) can no longer hold up the plates (box) thus resulting to a slip in the plates t
Normal Labour/ Stages of Labour/ Mechanism of LabourWasim Ak
Normal labor is also termed spontaneous labor, defined as the natural physiological process through which the fetus, placenta, and membranes are expelled from the uterus through the birth canal at term (37 to 42 weeks
GOAL: To create a poster that explains the phenomena of blue sky using the concept of wavelength and frequency of visible light.
SITUATION: As the creative head in the science club of Macasandig National High School, you are tasked to create a poster showcasing the phenomena of blue sky on Science Club bulletin board.
PRODUCT: A creative poster explains the phenomena of blue sky. The poster should be in 1/8 illustration board.
faults generate earthquakes.
S8ES-IIa- 14
Objectives:
1. Describe what fault is and how these faults related to earthquakes.
2. Determine the extent of damage an earthquake can do in a particular location.
Article Reading
Earthquake wreaks havoc in the Philippines more than 1,000 people are killed when a 7.7-magnitude earthquake strikes Luzon Island in the Philippines on this day in 1990. The massive tremor wreaked havoc across a sizeable portion of Luzon, the country’s largest island, with Baguio City suffering the most devastating effects.
The epicenter of the quake, which struck at 4:26 p.m., was north of Manila in the Nueva Ecija province. Reports indicate that the shaking went on for nearly a full minute. Collapsing buildings were the main cause of damage and death. Getting out of a multi-story building was a good safety precaution that afternoon, although many people were injured and a few even died in stampedes of others doing the same thing.
At Christian College, a six-story building completely collapsed, trapping approximately 250 students and teachers inside. Heroic rescue efforts saved many, but some victims who did not die in the collapse were found dead later from dehydration because they were not pulled out in time.
All types of buildings, including several resort hotels in Baguio, known as the
Philippines’ Summer Capital, suffered tremendous damage. Most of the city’s 100,000
residents slept outdoors that evening and during the following week, afraid to return to
their homes amid the frequent aftershocks. For days, workers pulled bodies from the
demolished buildings in Baguio. The best estimate is that 1,000 bodies were eventually
recovered. At least another 1,000 people suffered serious injuries. Rescue efforts were
hampered severely because the three main roads into the city were blocked by landslides. Hundreds of motorists were stranded on the roads as well.
A fault is a fracture or zone of fractures between two blocks of
rock. Faults allow the blocks to move relative to each other.
This movement may occur rapidly, in the form of an earthquake - or may occur slowly, in the form of creep. Faults may range in length from a few millimeters to thousands of kilometers. Most faults produce repeated displacements over geologic time.
The ground in the area of fault tends to remain not moving
because of frictional force between the two opposing plates (boxes). As stronger forces (rubber band) shakes up the fault, the friction (tape) can no longer hold up the plates (box) thus resulting to a slip in the plates t
Normal Labour/ Stages of Labour/ Mechanism of LabourWasim Ak
Normal labor is also termed spontaneous labor, defined as the natural physiological process through which the fetus, placenta, and membranes are expelled from the uterus through the birth canal at term (37 to 42 weeks
This slide is special for master students (MIBS & MIFB) in UUM. Also useful for readers who are interested in the topic of contemporary Islamic banking.
Exploiting Artificial Intelligence for Empowering Researchers and Faculty, In...Dr. Vinod Kumar Kanvaria
Exploiting Artificial Intelligence for Empowering Researchers and Faculty,
International FDP on Fundamentals of Research in Social Sciences
at Integral University, Lucknow, 06.06.2024
By Dr. Vinod Kumar Kanvaria
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it describes the bony anatomy including the femoral head , acetabulum, labrum . also discusses the capsule , ligaments . muscle that act on the hip joint and the range of motion are outlined. factors affecting hip joint stability and weight transmission through the joint are summarized.
A workshop hosted by the South African Journal of Science aimed at postgraduate students and early career researchers with little or no experience in writing and publishing journal articles.
2. What are Plates?
• The Earth’s crust and upper mantle
(Lithosphere) are broken into sections
called plates
A section of the lithosphere that slowly
moves over the asthenosphere, carrying
pieces of continental and oceanic crust.
Plates move around on top of the mantle like rafts
3. What is the Theory of Plate Tectonics?
The theory that pieces of Earth’s lithosphere are
in constant motion, driven by convection
currents in the mantle.
• Plates move
slowly in
different
directions
Cause different
geologic events
(like
earthquake,
volcano, etc.)
4. What makes the plates move?
Convection Currents in the mantle move the plates as the core heats
the slowly-flowing asthenosphere (the elastic/plastic-like part of the
mantle).
5.
6. FAULT – Breaks in Earth’s crust where rocks
have slipped past each other.
The edges of Earth’s plates
meet at plate boundaries.
Extended deep into the
lithosphere
7. What are the three types of boundaries?
Divergent Boundaries
Convergent Boundaries
Transform Boundaries
8. Divergent Boundaries
A plate boundary where two plates move away from each other.
RIFTING
causes
SEAFLOOR SPREADING
9. How is the rock pulled at Divergent
Boundaries?
Rock gets THIN in the middle as it is pulled
apart.
This STRESS is called
10. What happens when the rock SNAPS from
the Stress of Tension?
A Normal Fault (fault is a break in Earth’s
crust)
Rock drops down as it breaks
11. What happens next at Divergent Boundaries?
• A geologic feature or event…
May form RIFT VALLEYS on
continents
SEA-FLOOR
SPREADING in the ocean
12. Helpful Hints…
• Divergent is like “dissecting” or
“dividing”
• If you pull warm bubble gum or silly
putty, it will thin in the middle until it is
stressed so much that it breaks.
• Happens on land
& under H2O
14. How is the rock pushed at convergent
boundaries?
A plate boundary where two plates
move towards each other.
Boundaries between two
plates that are colliding
This stress is called COMPRESSION
16. There are 3 types of Convergent
Boundaries…
Ocean plate colliding with a less dense
continental plate
Subduction Zone: The process by which
oceanic crust sinks beneath a deep-ocean
trench and back into the mantle at a
convergent plate boundary.
20. • Ocean plate colliding with another ocean plate
• The less dense plate slides under the more dense plate creating a subduction
zone called a TRENCH
22. A continental plate colliding with
another continental plate
Have Collision Zones:
A place where folded and thrust
faulted mountains form.
23. • May form Mountain Ranges.
These are Folded Mountains, like the Himalayas or the Rockies.
24. What happens when the rock is squeezed
from the Stress of Compression?
A REVERSE FAULT
Rock is forced upward as it
is squeezed.
25. Helpful Hints…
• Convergent = “Connecting” boundaries
• May work like a trash compactor smashing rock.
– Rock goes crunches up to make folded mountains.
– Rock goes down “under” @ subduction zone.
27. How is the rock broken at Transform
Boundaries?
Rock is pushed
in two opposite
directions (or
sideways, but
no rock is lost)
This stress is
called
SHEARING
28. What happens next at Transform Boundaries?
• May cause Earthquakes
when the rock snaps from
the pressure.
• A famous fault @ a
Transform Boundary is the
San Andreas Fault in
California.
30. What happens when the rock is sheared
(or “cut”) from the Stress of Shearing?
A STRIKE-SLIP FAULT
Rocks on each side of the fault slip
past each other as they break.
31. Helpful Hints…
Shearing means cutting (“Shears” are like scissors)
Transform boundaries run like trains going past each other in different
directions & they shake the ground!
32. Can you match the
boundary name
correctly with its
diagram?
A._____________
B._____________
C._____________
Plate Boundaries: