This presentation is a summary about world climates addressed to my bilingual students in 3rd ESO. It consists of some information about the main climates together with representative pictures. It is a descriptve study.
Created by María Jesús Campos, teacher of Social Studies, Geoography and History in a bilingual section in Madrid.
learningfromgeography.wikispaces.com
learningfromhistory.wikispaces.com
Developed by María Jesús Campos Fernández, teacher in a bilingual section in Madrid
learningfromgeography.wikispaces.com
learningfromhistory.wikispaces.com
This presentation is a summary about world climates addressed to my bilingual students in 3rd ESO. It consists of some information about the main climates together with representative pictures. It is a descriptve study.
Created by María Jesús Campos, teacher of Social Studies, Geoography and History in a bilingual section in Madrid.
learningfromgeography.wikispaces.com
learningfromhistory.wikispaces.com
Developed by María Jesús Campos Fernández, teacher in a bilingual section in Madrid
learningfromgeography.wikispaces.com
learningfromhistory.wikispaces.com
Developed by María Jesús Campos Fernández, teacher of History, Geography and Art in a bilingual section in Alcorcón (Madrid, Spain)
learningfromhistory.wikispaces.com
learningfromgeography.wikispaces.com
Developed by María Jesús Campos Fernández, teacher of History, Geography and Art at a bilingual section in Alcorcon (Madrid, Spain)
learningfromhistory.wikispaces.com
learningfromgeography.wikispaces.com
Creado por María Jesús Campos Fernández, Jefe del Departamento de Geografía e Historia del IES Parque de Lisboa (Alcorcón, España), profesora de Geografía e Historia en sección bilingüe de inglés. Embajadora eTwinning
Creado por María Jesús Campos Fernández, Jefe del Departamento de Geografía e Historia del IES Parque de Lisboa (Alcorcón, España), profesora de Geografía e Historia en sección bilingüe de Inglés. Embajadora eTwinning.
Reflexiones sobre aprendizaje colaborativo y aprendizaje basado en proyectos. Cuestiones a tener en cuenta para crear un borrador de proyecto colaborativo
Developed by María Jesús Campos Fernández, Geography and History teacher in a bilingual section in Alcorcón, Madrid, Spain
learningfromhistory.wikispaces.com
learningfromgeography.wikispaces.com
Developed by María Jesús Campos Fernández, Geography and History teacher in a bilingual section in Alcorcon, Madrid (Spain)
learningfromhistory.wikispaces.com
learningfromgeography.wikispaces.com
Developed by María Jesús Campos Fernández, Geography and History teacher in a bilingual section in Alcorcón, Madrid (Spain)
learningfromhistory.wikispaces.com
learningfromgeography.wikispaces.com
Developed by María Jesús Campos Fernández, teacher of Geography, History and Art in a bilingual section in IES Parque de Lisboa (Alcorcón, Madrid, Spain)
learningfromgeography.wikispaces.com
learningfromhistory.wikispaces.com
Developed by María Jesús Campos Fernández, teacher at a bilingual section in Alcorcón (Madrid, Spain)
learningfromgeography.wikispaces.com
learningfromhistory.wikispaces.com
Operation “Blue Star” is the only event in the history of Independent India where the state went into war with its own people. Even after about 40 years it is not clear if it was culmination of states anger over people of the region, a political game of power or start of dictatorial chapter in the democratic setup.
The people of Punjab felt alienated from main stream due to denial of their just demands during a long democratic struggle since independence. As it happen all over the word, it led to militant struggle with great loss of lives of military, police and civilian personnel. Killing of Indira Gandhi and massacre of innocent Sikhs in Delhi and other India cities was also associated with this movement.
Synthetic Fiber Construction in lab .pptxPavel ( NSTU)
Synthetic fiber production is a fascinating and complex field that blends chemistry, engineering, and environmental science. By understanding these aspects, students can gain a comprehensive view of synthetic fiber production, its impact on society and the environment, and the potential for future innovations. Synthetic fibers play a crucial role in modern society, impacting various aspects of daily life, industry, and the environment. ynthetic fibers are integral to modern life, offering a range of benefits from cost-effectiveness and versatility to innovative applications and performance characteristics. While they pose environmental challenges, ongoing research and development aim to create more sustainable and eco-friendly alternatives. Understanding the importance of synthetic fibers helps in appreciating their role in the economy, industry, and daily life, while also emphasizing the need for sustainable practices and innovation.
2024.06.01 Introducing a competency framework for languag learning materials ...Sandy Millin
http://sandymillin.wordpress.com/iateflwebinar2024
Published classroom materials form the basis of syllabuses, drive teacher professional development, and have a potentially huge influence on learners, teachers and education systems. All teachers also create their own materials, whether a few sentences on a blackboard, a highly-structured fully-realised online course, or anything in between. Despite this, the knowledge and skills needed to create effective language learning materials are rarely part of teacher training, and are mostly learnt by trial and error.
Knowledge and skills frameworks, generally called competency frameworks, for ELT teachers, trainers and managers have existed for a few years now. However, until I created one for my MA dissertation, there wasn’t one drawing together what we need to know and do to be able to effectively produce language learning materials.
This webinar will introduce you to my framework, highlighting the key competencies I identified from my research. It will also show how anybody involved in language teaching (any language, not just English!), teacher training, managing schools or developing language learning materials can benefit from using the framework.
The Roman Empire A Historical Colossus.pdfkaushalkr1407
The Roman Empire, a vast and enduring power, stands as one of history's most remarkable civilizations, leaving an indelible imprint on the world. It emerged from the Roman Republic, transitioning into an imperial powerhouse under the leadership of Augustus Caesar in 27 BCE. This transformation marked the beginning of an era defined by unprecedented territorial expansion, architectural marvels, and profound cultural influence.
The empire's roots lie in the city of Rome, founded, according to legend, by Romulus in 753 BCE. Over centuries, Rome evolved from a small settlement to a formidable republic, characterized by a complex political system with elected officials and checks on power. However, internal strife, class conflicts, and military ambitions paved the way for the end of the Republic. Julius Caesar’s dictatorship and subsequent assassination in 44 BCE created a power vacuum, leading to a civil war. Octavian, later Augustus, emerged victorious, heralding the Roman Empire’s birth.
Under Augustus, the empire experienced the Pax Romana, a 200-year period of relative peace and stability. Augustus reformed the military, established efficient administrative systems, and initiated grand construction projects. The empire's borders expanded, encompassing territories from Britain to Egypt and from Spain to the Euphrates. Roman legions, renowned for their discipline and engineering prowess, secured and maintained these vast territories, building roads, fortifications, and cities that facilitated control and integration.
The Roman Empire’s society was hierarchical, with a rigid class system. At the top were the patricians, wealthy elites who held significant political power. Below them were the plebeians, free citizens with limited political influence, and the vast numbers of slaves who formed the backbone of the economy. The family unit was central, governed by the paterfamilias, the male head who held absolute authority.
Culturally, the Romans were eclectic, absorbing and adapting elements from the civilizations they encountered, particularly the Greeks. Roman art, literature, and philosophy reflected this synthesis, creating a rich cultural tapestry. Latin, the Roman language, became the lingua franca of the Western world, influencing numerous modern languages.
Roman architecture and engineering achievements were monumental. They perfected the arch, vault, and dome, constructing enduring structures like the Colosseum, Pantheon, and aqueducts. These engineering marvels not only showcased Roman ingenuity but also served practical purposes, from public entertainment to water supply.
Biological screening of herbal drugs: Introduction and Need for
Phyto-Pharmacological Screening, New Strategies for evaluating
Natural Products, In vitro evaluation techniques for Antioxidants, Antimicrobial and Anticancer drugs. In vivo evaluation techniques
for Anti-inflammatory, Antiulcer, Anticancer, Wound healing, Antidiabetic, Hepatoprotective, Cardio protective, Diuretics and
Antifertility, Toxicity studies as per OECD guidelines
Acetabularia Information For Class 9 .docxvaibhavrinwa19
Acetabularia acetabulum is a single-celled green alga that in its vegetative state is morphologically differentiated into a basal rhizoid and an axially elongated stalk, which bears whorls of branching hairs. The single diploid nucleus resides in the rhizoid.
Model Attribute Check Company Auto PropertyCeline George
In Odoo, the multi-company feature allows you to manage multiple companies within a single Odoo database instance. Each company can have its own configurations while still sharing common resources such as products, customers, and suppliers.
2. Climate
It is the usual state of the atmosphere in a
place over a long period of time. The sum up
of weather in a place during more than 30
years give rise to climate.
It is studied by Climatology.
6. The earth’s has got different types of climate distributed
according to latitude and altitude:
Warm zone: located between the Tropic of Cancer
and the Tropic of Capricorn. All of its climates have
an average annual temperature above 18ºC.
Temperate zones: there are 2 temperate zones
located between the Tropics and the Polar Circles. Its
climates have an average annual temperature around
15ºC and different seasons.
Cold zones: there are 2 cold zones located within
the polar circles and in mountains higher than 2,500
metres. The temperatures are very cold, usually
below 0ºC.
7.
8.
9.
Within those climate zones
we can find at least 12
different types of climate.
Each of them is grouped in a
category according to the
characteristics that they
share and the area in which
they are found.
Climate changes over time
but very slowly.
The Earth has experienced
many different climates over
its 4.54 billion years.
11. Location
• Along the
Equator, usually
within 25º of
the Equator
Temperature Precipitation
• These areas
receive constant
direct sunlight
so temperatures
are high and
stay the same
throughout
most of the
year.
•The mean
annual
temperature is
over 25ºC
• Abundant and
regular rainfall
throughout the
year. The
regular warm
temperatures
evaporate water
and keep
humidity high
allowing it to
rain almost
every day.
• Precipitation is
over 1500 mm
annually.
Seasons
• Only 1 season
because these
area always
receive direct
sunlight
throughout the
entire year.
12.
13. Location
• Near the
Equator, on the
outer edges of
Equatorial
climate.
Temperature Precipitation
• Temperatures
are high
throughout the
year.
• Abundant
rainfall but
under 1500 mm
annually.
•The mean
annual
temperature is
over 20ºC
• Precipitation
only falls during
the summer
monts, usually
from May to
August with
June and July
having the
heaviest rain.
•
Seasons
• 2 seasons, wet
(summer) and
dry (winter).
Usually the dry
season is
longer.
14.
15. Location
• Near the
Equator, on the
outer edges of
Equatorial
climate.
Temperature Precipitation
• Temperatures
are high
throughout the
year. But they
are mild in
winter and hot
in summer.
•The mean
annual
temperature is
over 18ºC
• Precipitation is
scarce, although
more than 250
mm annually.
Seasons
• 2 seasons, wet
(summer) and
dry (winter).
Usually the dry
season is
longer.
16.
17. Location
Temperature
Precipitation
Seasons
• On the east
coast of
continents
between 20º
and 40º north
and south of the
Equator
• Hot humid
summers and
mild winters as
these areas
receive direct
sunlight for a
large part of the
years.
• The rain falls
throughout the
year, but more
in summer. This
is because the
regularly high
temperatures
evaporate water
causing
humidity and
precipitation.
• 2 seasons,
summer and
winter. However
winter is not a
cold winter.
•The mean
annual
temperature
varies between
10ºC and 20ºC
• Precipitation is
over 1000 mm
annually.
• Summer
season lasts
longer.
18.
19. Location
Temperature
Precipitation
Seasons
• Between 30º
and 45º
latitudes (N-S).
On the western
sides of
continents. It
gets its name
from the climate
found around
the
Mediterranean
Sea.
• Warm to hot,
dry summers
and mild to cool,
wet winters.
• Precipitation is
irregular. Most
precipitation
falls in spring
and autumn.
Summers have
little or no
precipitation.
• Mild climate. It
has 4 seasons
but only 2 of
them are really
clear: summer
and winter.
•The mean
annual
temperature
varies between
12º to 18º.
Temperatures
during the
summer can
reach 30º.
• Precipitation is
irregular and
varies between
300mm to 800
mm anually.
• Summers are
longer than
winters, and
winters are
usually mild.
20.
21. Location
• Along the west
coast of mid-latitude
continents. Midway
between the tropics
and the
Artic/Antartic circles.
•It is stopped by the
presence of
mountains so this
climate covers more
land in Europe than
in North America
where mountains
block the humid air
from moving farther
inland.
Temperatur Precipitation
e
• Mild climate
with few
extremes in
temperature.
•The ocean’s
influence
keeps the air
over the land
cool in
summer and
warm in
winter.
•Temperatures
vary between
10º to 20º.
• Precipitation
is regular and
abundant.
• Precipitation
between 1000
and 1500 mm
annually.
Seasons
•
Temperatures
do not vary
much during
the year so
we only
distinguish 2
seasons
clearly:
summer and
winter.
22.
23. Location
• In the interior
of continents
between 30º
and 60º latitude
(N-S), but
usually above
the 40º line.
•Mainly in the
Northen
Hemisphere
since there are
no major
landmasses in
the Southern
Hemisphere.
Temperature
Precipitation
• A wide range of • Marked
temperatures
contrast
because of
between warm,
latitude (less
rainy summers
direct sunlight
and dry cold
and warmth).
winters.
•Temperatures
are high in
summer(20ºC)
and low in
winter (less than
5ºC)
• Precipitation is
between 300
and 1000 mm
annually.
•Almost all the
regions of this
climate
experience
snow.
Seasons
• 4 seasons:
warm and humid
summer; cool
and dry autumn;
cold and harsh
winter; and
warm and wet
spring.
24.
25. Location
• Located
near the
poles.
•It covers a
20% of the
Earth.
•It is the
most
extreme
climate of
the Earth.
Temperature
Precipitation
Seasons
• It is the coldest
climate on Earth
because of its
latitude.
•It receives
indirect sunligh
during part of
the year while in
“winter” the area
is in total
darkness.
•Temperatures
are never higher
than 5ºC, and
may fall to
-50ºC.
• Scarce
precipitation ,
less than 300
mm because its
too cold to
evaporate the
water, so the
humidity in the
air is too low to
create
precipitation.
• There is not
traditional summer
but we can
distinguish 2
seasons determined
by the amount of
light.
•“Summer”:nearly
24 hours of light
(the pole is pointed
towards the sun)
•“Winter”: nearly
24hrs of total
darkness (the pole is
facing away from the
sun)
•Precipitation
falls as snow.
26.
27. Location
• Between
60-75º
latitude,
along the
coast of the
Artic Ocean.
Temperature
Precipitation
Seasons
•Because of the high
latitude, indirect
sunlight delivers light
but little heat.
•Winters are very
harsh while summers
are cool.
•Although snow melts
in summer, the deeper
parts of the soil stay
frozen, is a layer
called permafrost.
• Low levels of
precipitation as
temperatures
are too low to
cause
evaporation.
•It can be
considered a
“desert”
•Winters are
very harsh and
summers are
cool.
28.
29. Location
•In high
mountain
areas.
•In sinle
mountains
such as
Mount
Kilimanjaro
and also in
large areas
such as the
Plateau of
Tibet.
Temperature
•This climate changes
as you move up to the
mountain.
Temperature depends
on the elevation.
Precipitation
Seasons
• Precipitation
•No seasons
depends also on
elevation.
• Sometimes
the base of the
mountain may
•As you move up it will be dry while
get colder and snow
there is snow in
may appear.
the top of the
•Temperature drops
mountain. This
about 6,5º degrees
happens
every 1000 m in
because high
elevation as you move mountains force
up a mountain.
warm air to
rise, so
precipitation
falls at the top.
30.
31. Location
Temperature
• Arid means
dry. Most
deserts are
found along
the 30º
latitude or in
the center of
the
continents or
in the rain
shadow of
large
mountain
ranges.
•The temperatures will
depend on the latitude
of the desert. The
farther from the
Equator the colder
they will be.
•There are warm and
cold arid climates.
•Warm deserts have
an average annual
temperature above
18ºC with significant
oscillations between
day and night that can
exceed 20ºC or more.
Precipitation
Seasons
• Precipitation is •They don’t
infrequent and
have regular
irregular.
seasons.
•Less than 150
mm per year.
32.
33. Location
Temperature
Precipitation
Seasons
•On the edge
of Arid
climate
areas.
•The temperatures will
depend on the latitude
of the area.
• Precipitation is
infrequent and
irregular. But
they receive
more
precipitation
than arid areas.
•Precipitation
may occur in
«winter».
•They don’t
have regular
seasons. Some
difference
between
summer and
winter.
34.
35.
36. Developed by María Jesús Campos
Chusteacher
Wikiteacher
Thanks to «Climate Types for Kids»