Minutes of the workshop transcribed. Speaker Dr. Eligio Obille Jr.
KATHA 2014 Batch 2: Day 7
Science Track: Geology
Dr. Eligio Obille Jr.
UP NISMED
University of the Philippines Diliman
September 6, 2014
Minutes of the
Workshop
1. Introduction. The speaker first grouped the
teacher-participants into nine groups and distributed globes for each group.
The activity started with geography called “Where am I?” using the globes. The
participants showed the parts of the globes like the equator, longitude and
latitude. The speaker clarified that the equator should be shown as a line and
not as a point for the students to better understand it. Then he asked some of
the participants to define the equator in their own words. Most of the
participants gave different and various answers. The speaker clarified one of
the participant’s use of the word “imaginary” in the definition of the equator.
He emphasized that it is important to put the definition in one’s own words and
not read from a book henceforth. He still extracted the full definition of the
equator from the teachers and said that it should be equally or midway that
separates the North and South Poles. He also clarified that use of north and
south hemispheres that one of the participants shared. It should be the line
that separates the north and south hemispheres equally into two halves that is
midway between the north and south poles.
2. Latitude and Longitude. He then
proceeded with the definitions of the lines of latitude and asked the
participants to define it in their own words and based on what they see. He
clarified that there is no wrong answers and not every definition should be
governed by what they read in textbooks. One participant said that latitude is
a circular line that expands going from the north dimension which changes as it
goes in the midway down. The speaker clarified that the teachers should define
the terms as if they were teaching Grade 6 students. Another participant said
that it is a circular line that goes around the globe. Another said that each latitude
has a 15-degree separation from each other. The speaker said that all their
answers were correct but the definitions they gave may only be understood not
by everyone. He clarified that latitudes are parallel to the equator, which the
teachers had not noticed. Another said that the circumference changes, but
better use the word “change in size”. It is important to use very simple words
that everyone must understand, especially the students. He also stressed that
parallel lines mean the lines do not meet. He said that there is no top or
bottom or north and south in space that’s why it is important to avoid the use
of top or bottom in defining geographic terms. “Equation is at latitude 0”, was
an advanced answer that should not be taught immediately to the students. It is
not the job of the teacher to give the definition of the term, it is his job to
let the student discover the answer, the speaker emphasized.
The next
question is “What is the latitude at the South Pole?” Answers were raised—90
degrees south. It is important to say that South Pole latitude is 90 degrees
south because north pole latitude is 90 degrees north. It is important that the
teacher would let the students to define the other terms by themselves after
they have guided them. The teacher does not do all the teaching, they should
let the students discover the definitions and answers by themselves as well.
The speaker then
let the teachers show him the different degrees of latitude in the globes. The
teachers all got the right answers and said that it would be better if the
teachers let the students find the estimation of the latitude degrees—as he
coined—guesstimate.
The speaker then
asked the teachers to define longitude. Vertical lines, circular lines, lines
from north to south, parallel lines. The speaker asked if the longitudes are
parallel lines, which are lines that do not meet. It means that lines of longitude
are not parallel lines because they meet in the north and south poles. He also
said that they are not vertical lines. He said that the way the moon is tilted
into a diagonal line is the same way as the lines of the longitude, which all
meet at the ends of the poles. It is important to describe these concepts
instead of reading it in textbooks, the speaker emphasized.
He also
discussed the Prime Meridian, the first longitude, which passes from the North
Pole near London to South. He asked the participants to find the Great Britain
in the globe. He also discussed the Greenwich in England. The Prime Meridian is
at 0 degrees, and it is going both east and west and meets at 180 degrees in
the globe. It divides the Eastern and Western hemispheres. He further discussed
the Prime Meridian and Greenwich and further called these that as the Prime
Meridian is farther away from one country, it is called far east; the closer to
Prime Meridian, it is called near east. It means that the Philippines is far
east from the Prime Meridian. He then asked the participants to locate 25
degrees and one teacher said there is none in the globe. He illustrated and
emphasized the use of legends of W and E in relation to the Prime Meridian—that
is West and East.
He also asked
the participants to locate Manila to the nearest degree. Answers raised were all
correct—15 degrees north and 120 degrees east. The speaker gave some more
exercises and competitions for the participants. He asked the participants to
locate certain countries using the latitudes and longitude degrees. He gave at
least three problem sets of finding countries using latitude and longitude
degrees. He next gave the activity in
reverse, the participants were to identify the latitudes and longitude degrees
of certain countries like Tokyo, Melbourne and Singapore. The speaker
emphasized that the first to locate is the latitude then the longitude degree.
3. Latitude and Climate. The knowledge of
latitude and longitude may be applied to climate. The speaker reviewed the
climate of different points in the world. The relationship is that the closer
the country is to the equator, the hotter the place is, and vice versa. There
is a corresponding degree in climate and in the location of the place. Latitude
0 is called the equator. There is also a special latitude that is 23.5 degrees
north—the Tropic of Cancer, in Tropic of Capricorn 23.5 south. Between these
places are called the tropical areas. He also discussed the temperate zones and
arctic zones. It is clear that there is a great correlation between the
latitude and the climate. He also explained the cold climates due to the
latitudes and longitude degrees in the north and south poles. Questions were
raised on the long nights and long days in the north and south parts of the
country.
4. Typhoon and Cyclone: Bottle Experiment. The speaker then
distributed two bottles of water for each group and asked them to connect both
bottles and shake them. He illustrated the correct use of the bottle experiment
to illustrate the phenomenon of cyclone and typhoon. It is important to take
off the label of the bottle and both bottles should be identical. It can be
applied in different storms in the Philippines like the typhoon Yolanda. He
discussed the entrance of storms in the Philippines using the bottle experiment
to further explain how it is applied in climate. He also discussed the concept
of the eye wall and tail of the storm that passes through different countries.
5. Tracking a Storm. The speaker also
introduced how to identify and detect the eye of the storm and illustrated
newspaper clippings during the worst typhoons in the Philippines. He also
illustrated the storm approach of Yolanda in Leyte in a video. It could be
noticed that the eye of the storm suddenly disappears once it lands in the
place because it weakens. The speaker conducted an activity where the
teacher-participants would plot the storm upsurge of Yolanda in a Philippine
map given a set of data. He reviewed their answers which were measured in
latitude and longitude degrees. He emphasized that such activity can be
introduced to students where they can plot the Philippine area of
responsibility and applying their knowledge on longitude and latitude. He also
discussed the upcoming storms in PAR identified by PAG-ASA. PAR, which includes
Taiwan is for the geography of storms only, the speaker emphasized. He also
asked why the area in the east of the Philippines is a large part of PAR and rephrased
the question. Answers raised were for PAG-ASA to be prepared in the upcoming
storms in the eastern Philippine Sea. The speaker said that it is important to
have a large part of the eastern area of the Philippines to be part of PAR
because it would help PAG-ASA and the people to be prepared and this would become
a warning for the people living near the coastal areas of the eastern
Philippine Sea. He also pointed out the reason why Taiwan is included in PAR
because storms may be strong enough for the people in one country to be
prepared. He also pointed out that the teachers don’t have to give all the
answers to the students and let them think it over to accomplish critical
thinking. Questions were raised on the limited time for the teachers to extract
the answer to the students in which the time may not be enough for them to do
it. The teachers may adjust to their strategy relative to the time limit. Giving
the answers to the students in an instant is not teaching at all, the speaker
pointed out. Inquiry process is important for the students to be developed;
even though it may kill a lot of time, but can be done. The speaker checked the
answers of the participants and most of them got the right answers.
He also
presented questions: 1) Where did Yolanda fall? The participants said it was
outside PAR. He said there are three ways to answer the question: the Pacific
Ocean, the longitude and latitude and outside PAR given one has full knowledge
of the geography of the country. 2) When did Yolanda enter the PAR? November 6,
between 3pm and 6pm, where it depends on where it overlapped in the boundary of
the Philippine area, according to the participants. 3) When did Yolanda leave
PAR? November 9 and between 12am and 6am. 4) In what direction did Yolanda move?
The participants answered from Southeast to Northwest. They may also say it
moved westward. It can be observed that the question can all be answered based
on the activity. Other different questions may be added given another set of
data. The speaker illustrated the long path of the origin of Yolanda to the
participants from far east to westward in China.
6. Tropical Cyclones. The speaker
discussed the different categories of tropical cyclones, namely tropical
depression, tropical storm, typhoon and supertyphoon, which all differ in their
speed. It can be interpreted in the Filipino language in the way vehicles move
in speed. Tropical storms mainly rely on their wind speed, not on the amount of
rain it produces. He described the different types of position of the storm
especially when one is located in the eye of the storm. He also gave and
illustrated examples of different storms and emphasized that storms all come
from seas and are formed in bodies of water. Temperate and warm water ranging
from 26 degrees celsius is also one point to form a storm. The direction is
also westward for it to become a storm. Therefore the eastern parts of Luzon
are always affected. 5) Where do tropical cyclones die out? It dies out during
its landfall because there is no temperate water anymore. Landfall in water
areas may also be low in temperature that’s why it dies out. He illustrated the
inquiry teaching by letting the teachers answer the questions themselves, which
can be applied to their students. 6) Why is the Philippine prone to typhoons?
The teachers said that it is because the Philippines surrounded by large bodies
of warm and temperate waters. Also, there is no other country near the Pacific
ocean where storms can land, except for the Philippines. This entails disaster
preparedness. Observations were raised on the clockwise movement and rotation
of the Earth relative to the movement of storms being westward. The speaker
said it is the Coriolis Effect, but it was too advanced for the lecture. Convention
box—when there is a storm in the country, the wind above is warmer, where warm
air rises. The air around will replace the warm air, which is called the low
pressure area. All storms have low pressure area according to the speaker. It
may advance to tropical depression. Wind then, which is the horizontal movement
of the air then rises and creates the low pressure area. Typhoons are always
pushed by wind currents that are bigger than the current itself, and are always
attracted by low pressure area. When the air rises in a certain area, the
strong winds and low pressure area are attracted in that direction, that is why
it is westward. Another question is raised on whether the storm moves in a
clockwise or counterclockwise. In southern hemisphere it is clockwise and in
northern hemispher it is counterclockwise. This is due to the Coriolis Effect. He
briefly discussed the topic on the Coriolis Effect using the globe. This is why
there is a rotation of the storms because there is the rotation of the earth.
A final question
was raised if there is a possibility of the occurrence of a storm from the
northern hemisphere to the southern hemisphere. The speaker said there is a
possibility, but most probably it weakens because there is the equator that
stops the storm from passing by. Tropical storms in convergent and
intertropical convergent zones give rise to diagonal rises of storms where warm
air rises.
7. Earthquakes and Faults. The speaker then
gave an activity called Break and Shake. He recalled the 1990 earthquake in the
Philippines where 201 people died. The use of intensity 8 was wrong; it should
have been magnitude 7.8, where there was a simple miscommunication. He
illustrated a map of the world and all the black areas are the ones in which
earthquakes occurred. It means earthquakes do not occur in any place. There are
only certain places where earthquakes occur and are confined in certain places.
It occurs in boundaries below plates. The activity involved the use of sand and
two pieces of paper where the participants would replicate the occurrence of an
earthquake. The activity showed a similarity of a road in which it was
displaced when an earthquake occurred. The crack is called the fault, according
to the speaker. He then asked what the definition of a fault based on the
activity. The participants said that it is the place where two plates meets,
collide, crack, breaks, separates along which there is movement. He illustrated
a real fault and asked why there is a fault in that place. It is because there
is a crack and displaced movement of the plates or in the ground. The fault
should be big enough to be called one, the speaker pointed out. He illustrated
more examples of faults.
The speaker
illustrated a model of a fault in an activity, which involved carton boxes,
paper clips and rubber bands. He emphasized that the movement of the ground is
sudden, not slowly. He illustrated the pull of force of the rubber band with
the taped boxes of carton and showed an earthquake in action. At first the pull
of the rubber band is the only force exerted in the movement until there is a
strong force of pull and the ground shakes and turns into an earthquake. All
the groups were able to illustrate the phenomenon using the materials given. The
longer the rest period of the force, the stronger the earthquake would be, and
vice versa. An earthquake therefore is a big fault made by a sudden movement of
the earth’s crust. The other groups tried to tape a paper house in one box and
tested the result of the house’s destruction with the earthquake in action. He
also shared some websites on earthquakes. A question was raised on aftershocks.
There are three kinds of shocks, foreshock, the shock itself and aftershock,
where aftershocks are the small minimal earthquakes due to the aftermath of the
vibrations of the ground.
8. Heat and Earthquake. The speaker then
proceeded with heat, as in heat in the lava of a volcano. Heat temperature is
relative, depending on the layers of the earth and the place. Excessive heat
causes the plates to move above. A question was raised on the concept of
trenches and plate tectonics, but the speaker did not further discuss the
complicated topic. He also clarified the use of tectonic plate and plate
tectonics—one is the place itself while the other one is the theory. He also
slightly discussed convergent and divergent boundaries where all earthquakes
occur. A teacher clarified the complicated topic which is taught in Grade 6,
and asked the speaker to further discuss it. More questions were raised by the
participants regarding analogies on earthquake. Another teacher asked the
correlation of the earthquake and the volcanic eruption, but the speaker said
they are not.
No comments:
Post a Comment