Monday, September 9, 2013

How Rocks & Minerals Are Formed

Original Site

How Rocks & Minerals Are Formed

THE EARTH'S CRUST

The whole earth is made of rocks & minerals. 
Inside the earth there is a liquid core of molten rock and on the outside there is a hard crust.
If you compare the earth to an egg, the shell on an egg is like the crust on the earth.
The crust is made up of rocks and minerals.
Much of the crust is covered by water, sand, soil and ice.
If you dig deep enough, you will always hit rocks.

Below the loose layer of soil, sand & crumbled rocks found on Earth is bedrock, which is a solid rock.
  • The Crust makes up less than 1% of the Earth’s mass (0.4%)
    It is made of oxygen, magnesium aluminum, silicon calcium, sodium potassium, iron.
    There are 8 elements that make up 99% of the Earth’s crust.
    The continents are about 35 km thick and the ocean floors are about 7 lm thick.
  • The Mantle is the solid casing of the Earth and is about 2900 km thick.
    It makes up about 70% of the Earth’s mass (68.1%).
    It is made up of silicon, oxygen, aluminum and iron.
  • The Core is mainly made of iron and nickel and makes up about 30% of the Earth’s mass (31.5%).
    The Outer Core is 2200 km thick and is liquid and the Inner core is 1270 km thick and is solid.

ROCKS

The rocks you see around you - the mountains, canyons & riverbeds, are all made of minerals.
A rock is made up of 2 or more minerals.
Think of a chocolate chip cookie as a rock.
The cookie is made of flour, butter, sugar & chocolate.
The cookie is like a rock and the flour, butter, sugar & chocolate are like minerals.
You need minerals to make rocks, but you don't need rocks to make minerals.
All rocks are made of minerals.

MINERALS

A mineral is composed of the same substance throughout.
If you were to cut a mineral sample, it would look the same throughout.
There are about 3000 different minerals in the world.
Minerals are made of chemicals - either a single chemical or a combination of chemicals.
There are 103 known chemical elements. Minerals are sorted into 8 groups.
Some common examples have been listed for each.


CRYSTALS

Crystals are minerals that have had the chance to grow in the shape that they were meant to be.
Just like your DNA determines the colour of your eyes, how tall you will get to be and the shape of your bones,
the chemicals that a mineral is made of determines what shape it gets to be.
We can tell different minerals apart by what crystal shape they are.
Sometimes minerals form in spaces where there is not a lot of room, so they don't have a crystal shape.
When there is just a big hunk of a mineral, it is called a massive mineral.
If there is a definite shape with easy to see flat sides, it is called a mineral 
crystal.
Most of the earth's crystals were formed millions of years ago.
Crystals form when the liquid rock from inside the earth cool and harden.
Sometimes crystals form when liquids underground find their way into cracks and slowly deposit minerals.
Most mineral crystals take thousands of years to "grow" but some like salt (halite)
can form so quickly that you can watch them grow at home!

Some people think of crystals as clear pretty rocks that are used for jewelry.
Amethyst is a very common quartz crystal.
Crystals do not have to be clear, but those are the kinds you will usually see in the stores.

SOIL, SAND & DIRT

When rocks break down into smaller & smaller pieces, they turn into sand.
If you look at the sand under a microscope, you will see that sand is made up of
the same minerals as the rocks that the sand came from.
When plants start to sprout up in sand, it is turning from being just small bits of rock to being soil.
For a good description of the importance of sand and How Sand Is Made,
visit http://www.madehow.com/Volume-3/Sand.html

Soil is very important to life on earth. It supports plant life. We could not live without plants.
Soil is made up of sand and decomposing plants and animals.
Soil has many names including: clay, silt, mud, dirt, topsoil, dust, potting soil and humus

THE ROCK CYCLE

Rocks are constantly being formed, worn down and then formed again.
This is known as the Rock Cycle.
It is like the water cycle but it takes a lot longer.
It takes thousands and millions of years for rocks to change.
Rocks are divided into 3 Types. They are classified by how they were formed.
Some good sites that help explain this are:

IGNEOUS ROCKS

Igneous means made from fire or heat.
When volcanoes erupt and the liquid rock comes up to the earth's surface, then new igneous rock is made.
When the rock is liquid & inside the earth, it is called magma.
When the magma gets hard inside the crust, it turns into granite.
Most mountains are made of granite. It cools very slowly and is very hard.

When the magma gets up to the surface and flows out, like what happens when a volcano erupts,
then the liquid is called lava.
Lava flows down the sides of the volcano.
When it cools & turns hard it is called obsidian
lava rock or pumice - depending on what it looks like.
  • Igneous rocks form when molten lava (magma) cools and turn to solid rock.
    The magma comes from the Earth’s core which is molten rock .
    The core makes up about 30% of the Total Earth Mass (31.5%)
  • Obsidian is nature’s glass. It forms when lava cools quickly on the surface. It is glassy and smooth.
  • Pumice is full of air pockets that were trapped when the lava cooled when it frothed out onto the surface.
    It is the only rock that floats.
     
  • There are 5 kinds of igneous rocks, depending on the mix of minerals in the rocks.
  • Granite contains quartz, feldspar & mica
  • Diorite contains feldspar & one or more dark mineral. Feldspar is dominant.
  • Gabbro contains feldspar & one or more dark mineral. The dark minerals are dominant.
  • Periodotite contains iron and is black or dark.
  • Pegmatite is a coarse-grained granite with large crystals of quartz, feldspar and mica.
To learn more about igneous rocks and how rocks are formed, take a look at this Volcano WebQuest

SEDIMENTARY ROCKS

When mountains are first formed, they are tall and jagged like the Rocky Mountains on the west coast of North America.
Over time (millions of years) mountains become old mountains like the Appalachian Mountains
on the east coast of Canada and the United States.
When mountains are old, they are rounded and much lower.
What happens in the meantime is that lots of rock gets worn away due to erosion.
Rain, freeze/thaw cycle, wind and running water cause the big mountains to crumble a little bit at a time.

Eventually most of the broken bits of the rock end up in the streams & rivers that flow down from the mountains.
These little bits of rock & sand are called sediments.
When the water slows down enough, these sediments settle to the bottom of the lake or oceans they run into.
Over many years, layers of different rock bits settle at the bottom of lakes and oceans.

Think of each layer as a page in a book. One piece of paper is not heavy.
But a stack of telephone books is very heavy & would squish anything that was underneath.
Over time the layers of sand and mud at the bottom of lakes & oceans turned into rocks.
These are called 
sedimentary rocks.
Some examples of sedimentary rocks are sandstone and shale.
Sedimentary rocks often have fossils in them.
Plants & animals that have died get covered up by new layers of sediment and are turned into stone.
Most of the fossils we find are of plants & animals that lived in the sea. They just settled to the bottom.
Other plants & animals died in swamps, marshes or at the edge of lakes.
They were covered with sediments when
the size of the lake got bigger.

When large amounts of plants are deposited in sedimentary rocks, then they turn into carbon.
This gives us our coal, oil, natural gas and petroleum.
A large sea once covered the central part of Canada and the climate was very tropical.
In time, sedimentary rocks formed there.
That is why we find dinosaur fossils in Alberta and the area is a good source of natural fuels.

  • Sedimentary rocks cover 75% of the earth’s surface.
    Most of the rocks found on the Earth’s surface is sedimentary even though sedimentary rocks
    only make up less than 5% of all the rocks that make up Earth.
  • When rocks are exposed to the elements – air, rain, sun, freeze/thaw cycle, plants –
    erosion occurs and the little bits of rock worn away get deposited as sediments.
    Over time, these sediments harden as they get buried by more sediments and turn into sedimentary rocks.
  • Sedimentary rocks are usually formed in layers called strata.
  • There are 6 main kinds of sedimentary rocks depending on the appearance of the rock.
  • Conglomerate rock has rounded rocks (pebbles, boulders) cemented together in a matrix.
  • Sandstone is a soft stone that is made when sand grains cement together. Sometimes the sandstone is
    deposited in layers of different colored sand.
  • Shale is clay that has been hardened and turned into rock. It often breaks apart in large flat sections.
  • Limestone is a rock that contains many fossils and is made of calcium carbonate &/or microscopic shells.
  • Gypsum, common salt or Epsom salt is found where sea water precipitates the salt as the water evaporates.
  • Breccia has jagged bits of rock cemented together in a matrix.

Understanding Erosion & Sedimentary Rocks by Looking at Lint!

You may have a difficult time imagining something solid like rocks wearing down over time - but everything does. If you take a look in the lint trap of your dryer, you will see that your clothes are being worn away as they tumble in the dryer. In fact if there is enough lint - you will see how these bits have been laid down into layers - just like sediments at the bottom of the lake. You will see layers of different colors because the clothes you dried were different - just like you will see different layers of rocks in sedimentary rocks. What is even more interesting is that if you scrunch up the lint a bit like in the picture here, you can see the layers of lint bending - just like the layers of rock are bent. Look carefully at the rocks in road cuts and you sill see layers of rocks that have been folded just like the lint in your dryer. Neat eh?!

METAMORPHIC ROCKS

Metamorphic rocks are rocks that have changed.
The word comes from the Greek "meta" and "morph" which means to change form.
Metamorphic rocks were originally igneous or sedimentary, but due to movement of the earth's crust, were changed.

If you squeeze your hands together very hard, you will feel heat and pressure.
When the earth's crust moves, it causes rocks to get squeezed so hard that the heat causes the rock to change. 
Marble is an example of a sedimentary rock that has been changed into a metamorphic rock.
  • Metamorphic rocks are the least common of the 3 kinds of rocks.
    Metamorphic rocks are igneous or sedimentary rocks that have been transformed by great heat or pressure.
  • Foliated metamorphic rocks have layers, or banding.
    • Slate is transformed shale. It splits into smooth slabs.
    • Schist is the most common metamorphic rock. Mica is the most common mineral.
    • Gneiss has a streaky look because of alternating layers of minerals.
  • Non-foliated metamorphic rocks are not layered.
    • Marble is transformed limestone.
    • Quartzite is very hard.

EROSION

Erosion is a key part of the Rock Cycle.
It is responsible for forming much of the interesting landscape that is around us.
It is also a major problem as people live in areas in large numbers and get used to the environment being in a certain way. People can do things to increase erosion or slow it down.
Erosion happens mainly as a result of weathering – the effect of water, temperature and wind on the landscape. 
Water causes much erosion. When it falls as acid rain, it can dissolve rocks that are sensitive to acid.
Marble & limestone weather when exposed to the rain.
When the rain falls very heavily, as in monsoons, then flooding can happen.
Rivers with a lot or rushing water can cause mud slides and erode river banks. 
The action of waves on a beach causes much erosion.
The waves pound on the rocks & over time, cliffs crumble.
That is why you will often find sand & little pebbles on beaches.
Rushing water, like what you find in rivers that move quickly in the mountains or strong waves
on the shores of oceans, roll rocks around.
This causes the sharp edges of the rocks to get knocked off & that is why river rocks are so smooth & beach pebbles look polished.
  • Acid Rain: chemicals in the air combine with precipitation
    When it rains it dissolves certain minerals sensitive to acid.
  • Leaching by ground water: water soaks into the soil, picks up chemicals
    This allows the water to leach or dissolve rocks it comes in contact with at bedrock.
  • Wave action at the beach: the waves tumble rocks
    Rocks get ground down by the sand particles already on the beach, rocks smash against each other & break.
  • Fast moving water: rocks get picked up & carried when water runs swiftly
    By bouncing along a river & smashing into other rocks, the sharp edges get knocked off.
  • Glaciers: large sheets of ice pick up large rocks, scrape bedrock
    Rocks tumble in under-glacier rivers when glaciers melt.
  • Precipitation / Floods: heavy rain can cause floods which move & break rocks

Broken glass is tumbled on the beach and worn smooth by the action of the waves.

Broken bits of shale tumble to the bottom of hills and river banks. Then they are washed away and tumbled by waves and water. When they are deposited at the side of rivers and on the beach, they are smooth. This is caused by erosion.
The freeze / thaw cycle causes mountains to crumble over time and large rocks to break
down into little rocks.
When water gets into cracks in the rocks, this water expands during the freeze cycle,
making the cracks bigger.
Then when the cracks fill up with water in the thaw period.
This allows more water to go deeper into the rock which will make the rocks split apart
when they freeze again. The power of frozen water expanding can be seen when you leave
a glass bottle filled with liquid in the freezer.
  • Wind, when it carries bits of sand and grit, can blast away layers of rocks.
    The wind can easily pick up little bits of sand and then sandblast the rocks that are in the wind's way.
    Sometimes only the soft layers of the rock are eroded, leaving interesting shapes.
    This kind of erosion usually only happens in very dry, desert like areas.
  • Other causes for rocks to break down & erode:
    • How hard / tough mineral is: softer, more friable rocks and minerals break up easily
    • Plant roots growing: plants get nutrients from the soil, seek out certain minerals like potash,
      apatite for fertilizer, small roots go in cracks & break up mineral or rock when the root grows bigger
    • Rock Falls: rocks tumbling down from a cliff or steep mountainside cause rocks to break up
    • Contact with soil: certain soils have chemicals in them that react with the chemical make up of rocks
  • Photo of what damage erosion does  http://www.erosionseed.com/
  • Erosion also makes caves. Visit The Virtual Cave 

GEMSTONES

Gemstones are often what people mean when they talk about "crystals".
There are many gemstones and most are used for jewelry or decoration.
The are minerals that are usually transparent and have been cut and polished.
Some gemstones look similar to what the mineral looks like when found in nature and others are very different.
Few minerals found in nature are suitable to use unaltered in jewelry.
One exception is the "Herkimer Diamond" which forms in vugs of gray rock and are found near Herkimer, New York.
These are not real diamonds - they are quartz crystals that look like they have been cut & polished like a diamond.

To see some gems, look at

BIRTHSTONES

Most people are familiar with precious & semi-precious gemstones because of the popularity of birthstones.
They are as follows:
MonthModern (as of 1912 USA)Traditional
JanuaryGarnetGarnet
FebruaryAmethystAmethyst
MarchAquamarineBloodstone
AprilDiamondDiamond
MayEmeraldEmerald
JunePearl, MoonstoneAlexandrite
JulyRubyRuby
AugustPeridotSardonyx
SeptemberSapphireSapphire
OctoberOpal, TourmalineTourmaline
NovemberYellow Topaz, CitrineCitrine
DecemberBlue Topaz, TurquoiseZircon, Turquoise, Lapis Lazuli

Date of Download: Sept. 10, 2013

Eclipse facts


Lunar eclipses can only occur during a full moon.

Solar eclipses can only occur during a new moon.

A Solar eclipse always occurs two weeks before or after a lunar eclipse.

Eclipses very often occur in threes, alternating lunar, solar and lunar.

The maximum time a lunar eclipse can last is 3 hours and 40 minutes.

The longest time the Moon can stay in totality is 1 hour 40 minutes.

The maximum time for a total solar eclipse is 7 minutes and 40 seconds.

The maximum time for an annular solar eclipse is 12 minutes 24 seconds.

Lunar eclipses can occur up to 3 times a year.

Solar eclipses can occur at least 2 and no more than 5 times a year.

Lunar eclipses are visible over an entire hemisphere.

Solar eclipses are visible in a narrow path a maximum of 167 miles wide (269km.)

At any geographic position on the Earth, a total solar eclipse occur an average of once every 360 years.

The cycle of eclipses repeats every 18.6 years called the saros.

The eclipse shadow moves at 2,000 mph at the Earth's poles and 1,000 mph at the Earth's equator.

The StarrySkies Lunar Eclipse Pages
Total Lunar Eclipse: Second Moon Show of the Year takes place November 8
What is a Lunar Eclipse
Why we don't have a Lunar Eclipse every month
Eclipse Facts
Rating a lunar eclipse - the Danjon Scale
Photographing a Lunar Eclipse
Myths and Lore about Lunar Eclipses
The Lunar Eclipse that Saved Christopher Columbus
Moon Facts
Moonstats - Lunar Vital Statistics
Moonwatching
Why we see only one side of the Moon - librations
Lunar Phases
Moon Tales: The Night the Moon fell - 1939 Springfield, Missouri
Moon Tales: When the Moon saved the Sun - New York 1835
Moon Trees - Have you got one in Your Town? 
Multimedia Moon - Images and Video clips of the Moon
3D Moon - Catch the Moon in 3D (note: you will need 3D glasses)

Copyright © 1995 - 2008
Kathy Miles, Author, and Chuck Peters, Systems Administrator
cont...@starryskies.com
URL reveals our email address after you solve a reCAPTCHA (image containing two words).

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THE HOROLOGICAL CYCLE (WATER CYCLE)


The Water Cycle
Introduction
Precipitation, evaporation, and transpiration are all terms that sound familiar, yet may not mean much to you. They are all part of the water cycle, a complex process that not only gives us water to drink, fish to eat, but also weather patterns that help grow our crops.


Water is an integral part of life on this planet. It is an odorless, tasteless, substance that covers more than three-fourths of the Earth's surface. Most of the water on Earth, 97% to be exact, is salt water found in the oceans. We can not drink salt water or use it for crops because of the salt content. We can remove salt from ocean water, but the process is very expensive.  

Water is an integral part of life on this planet. It is an odorless, tasteless, substance that covers more than three-fourths of the Earth's surface. Most of the water on Earth, 97% to be exact, is salt water found in the oceans. We can not drink salt water or use it for crops because of the salt content. We can remove salt from ocean water, but the process is very expensive.
The amount of fresh water on earth is only 3%. Two percent is in solid form, found in ice caps and glaciers. Because it is frozen and so far away, the fresh water in ice caps is not available for use by people or plants. That leaves about 1% of all the Earth's water in a form useable to humans. This fresh water is found in lakes, rivers, streams, ponds, and in the ground. (A small amount of water is found as vapor in the atmosphere.)

Scientific Concepts

There are six important processes that make up the water cycle. These are:
Evaporation
Evaporation is the process where a liquid, in this case water, changes from its liquid state to a gaseous state. Liquid water becomes water vapor. Although lower air pressure helps promote evaporation, temperature is the primary factor. For example, all of the water in a pot left on a table will eventually evaporate. It may take several weeks. But, if that same pot of water is put on a stove and brought to a boiling temperature, the water will evaporate more quickly.


During the water cycle some of the water in the oceans and freshwater bodies, such as lakes and rivers, is warmed by the sun and evaporates. During the process of evaporation, impurities in the water are left behind. As a result, the water that goes into the atmosphere is cleaner than it was on Earth.

Condensation
Condensation is the opposite of evaporation. Condensation occurs when a gas is changed into a liquid. Condensation occurs when the temperature of the vapor decreases.
When the water droplets formed from condensation are very small, they remain suspended in the atmosphere. These millions of droplets of suspended water form clouds in the sky or fog at ground level. Water condenses into droplets only when there are small dust particles present around which the droplet can form.

Precipitation
When the temperature and atmospheric pressure are right, the small droplets of water in clouds form larger droplets and precipitation occurs. The raindrops fall to Earth.
As a result of evaporation, condensation and precipitation, water travels from the surface of the Earth goes into the atmosphere, and returns to Earth again.
Surface Runoff
Much of the water that returns to Earth as precipitation runs off the surface of the land, and flows down hill into streams, rivers, ponds and lakes. Small streams flow into larger streams, then into rivers, and eventually the water flows into the ocean.
Surface runoff is an important part of the water cycle because, through surface runoff, much of the water returns again to the oceans, where a great deal of evaporation occurs.

Infiltration
Infiltration is an important process where rain water soaks into the ground, through the soil and underlying rock layers. Some of this water ultimately returns to the surface at springs or in low spots downhill. Some of the water remains underground and is called groundwater.
As the water infiltrates through the soil and rock layers, many of the impurities in the water are filtered out. This filtering process helps clean the water.

Transpiration:
One final process is important in the water cycle. As plants absorb water from the soil, the water moves from the roots through the stems to the leaves. Once the water reaches the leaves, some of it evaporates from the leaves, adding to the amount of water vapor in the air. This process of evaporation through plant leaves is called transpiration. In large forests, an enormous amount of water will transpire through leaves.

The Cycle

Each part of the cycle drives the other parts. Water is constantly being cycled between the atmosphere, the ocean and land. This cycling is a very important process that helps sustain life on Earth. 
As the water evaporates, vapors rise and condense into clouds. The clouds move over the land, and precipitation falls in the form of rain, ice or snow. The water fills streams and rivers, and eventually flows back into the oceans where evaporation starts the process anew.  Learn a lot more about this complicated process in concepts.

Water's state (solid, liquid or gas) is determined mostly by temperature. Although water continuously changes states from solid to liquid to gas, the amount of water on Earth remains constant. There is as much water now as there was hundreds of millions of years ago.


Cloud Formation
Precipitation is one key to the water cycle.
Rain comes from clouds, but where do clouds come from?
Through the process of evaporation and transpiration, water moves into the atmosphere. Water vapors then join with dust particles to create clouds. Eventually, water returns to Earth as precipitation in the form of rain, snow, sleet, and hail.
All clouds contain water vapors. You rarely ever see clouds in the desert because there is very little water to evaporate and form clouds. Coastal regions can receive a lot of rain because they pull up moisture from surrounding waters.
Cloud size is influenced by many complex factors, some of which we still do not understand very well. These include: heat, seasons, mountain ranges, bodies of water, volcanic eruptions, and even global warming.

There are many funny names for clouds.
Have you ever wondered why clouds have such weird names?
In 1802 an Englishman by the name of Luke Howard invented the cloud naming system that is still in use today.  Howard used Latin names to describe clouds. (The first part of a cloud's name describes height, the second part shape.)
The prefixes denoting heights are:
cirro, high clouds above 20,000 feet,
alto and mid level clouds between 6,000 - 20,000 feet.
There is no prefix for low level clouds.
The names denoting shapes are:
cirrus means curly or fibrous,
stratus means layered
cumulus means lumpy or piled.
Nimbo or nimbus is added to indicate that a cloud can produce precipitation.
Given that information, describe what each of the following clouds would look and act like?
•Cumulonimbus
•Nimbostratus
•Cirrocumulus
•Altostratus


Citation: 

Date of Download: Sept. 9, 2013
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Tuesday, July 30, 2013

Philippine Environment Laws


P.D. 984 – Pollution Control Law

P.D. 1151 – Philippine Environmental Policy

- defines the general policies on he pursuit of a better quality of life for the present and future generations and mandates the undertaking the environmental impact assessments for all projects, which may significantly affect the environment.

P.D. 1152 – Philippine Environmental Policy

- defines the policy objectives and the strategies for the various aspects of environmental management, such as air and water quality management, natural source development, land management, and waste management. It launches a comprehensive national program of environmental protection and management, with reference to policies and standards of noise, air quality, water quality, classification of water and waste management.

P.D. 1586 – defines the framework for the implementation of the environmental impact assessment as the mechanism to reconcile the impacts of development projects on society and the physical environment.

P.D. 389 (P.D. 705) – The Forestry Reform Code

- codifies, updates and raises forestry laws in the country. It emphasizes the sustainable utilization of forest resources.

P.D. 330 & P.D. 953 – laws on penalizing illegal cutting of trees

P.D. 953 & 1153 – laws on tree planting

P.D. 331- laws requiring all public forests be developed on a sustained yield basis.

P.D. 704 – preservation of optimum productivity of fishery resources through conservation and protection.

P.D. 1015 – banning the operation of commercial fishing within a distance of 7 kilometers from the shoreline.

P.D. 1058 – increasing the penalties for illegal forms of fishing.

P.D. 1219 – providing for the protection of coral ecosystems.

P.D. 1067 – Water Code of the Philippines

- adopts adequate measures to conserve and regulate the use of water in commercial, industrial and residential areas. It also provides other policy guidelines in water quality and management of water resources.

P.D. 463 – amended the Mining Act of 1936, requires all mining leaseholders to comply with Pollution Control Laws and regulations and provide for penalties for noncompliance.

P.D. 1198 – reinforces this provision for restoration of mined-out areas to this original condition to the extent possible.

P.D. 1251 – imposes fines on tailings and mine wastes and the fund generated is used to pay for the damages to land, agricultural crops, forests products, aquatic resources and infrastructures caused by pollution for mining operations.

P.D. 984 – The Pollution Control Law

P.D. 1181 (supplements the provision of P.D. 984) – providing for the abatement, control and prevention of vehicular pollution & establishing the maximum allowance emissions of specific air pollutants from all types of vehicle.

P.D. 600 ( amended by P.D. 979) – Water Pollution Control

- prohibits the discharge of oil, noxious liquid substances, and other harmful substances into the country’s inland and territorial waters.

P.D. 825 – prohibits the improper disposal of garbage

P.D. 856 – Sanitation Code

- places the responsibility in the local government units for he solid waste management in his area of production.

P.D. 1144 – Control of Pesticides

R.A. 8749 – Philippine Clean Air Act of 1999

- provides for a comprehensive air pollution control policy

R.A – 3720 – Food Additives

R.A. 6425 – Drugs

R.A 280 – Cosmetics

R.A. 7160 – Local Government Code of 1991

-provides that local government should share with the national government the responsibility in the management and maintenance of ecological balance within their territorial jurisdiction subject to national policies and other pertinent provisions of the code.

R.A. 6969 – Toxic Substances and Hazardous and Nuclear Wastes Control Act

- authorizes the DENR to establish a program to regulate, restrict or prohibit the importation, manufacture, processing, sale, destruction, use and disposal of chemical substances, and mixture that present unreasonable risk and/or injury to health or the environment.

R.A. 8550 – The Fisheries Code of the Philippines

- defines the policies of the state in the protection, conservation and effective management of fisheries stock as well as identifying allowable fishing methods in Philippine coastal waters.

R.A. 9003 – The Solid Waste Management Act of 2001- an act providing for an ecological solid waste management program, creating the necessary institutional mechanisms and incentives, declaring certain acts prohibited and providing penalties, appropriating funds therefor, and for other purposes.

R.A. 9275- also known as the Philippine Clean Water Act of 2004 – an act providing a comprehensive water quality management and for other purposes.
R.A. 9729 – also known as the Climate Change Act of 2009. - an act mainstreaming climate change into government policy formulations, establishing the framework strategy and program on climate change, creating for this purpose the climate change commission, and for other purposes.

Tuesday, January 22, 2013

Weather Forecast and Advisory Terms


DEFINITION OF TERMS



Following are definitions of some common terms used in various issuances such as forecasts and advisories. 

Weather
_ 
the specific conditions of the atmosphere at a particular place and time. It is measured in terms of such parameters as wind, temperature, humidity, atmospheric pressure, cloudiness and precipitation. In most places, weather can change from hour to hour and season to season.
Climate
_
the average weather and its long term variability over a particular place and time (say a month, a season, a year or several years).
Climate Variability
_
refers to the fluctuations / variations of climate observed since the instrumental period (i.e., 1860 to present). These fluctuations are due to natural causes and to human activities. 
Season
_
a division of the year according to some regularly recurent phenomena, usually astronomical or climatic. In the tropics, precipitation is the primary factor; thus, nearly all regions have their rainy season and dry season. 
Normal 
(climatological normal)
_
the average value of a meteorological element over any fixed period of years that is recognized as standard for a country and element concerned; usually a 30-year period as recommended by the World Meteorological Organization (WMO). 
Anomaly 
(departure from normal)
_
the deviation of (usually) temperature or precipitation from the normal values in a given region over a specified period. 
NE Monsoon
_
locally known as "Amihan". It affects the eastern portions of the country from October up to late March, starts over Siberia as a cold, dry air mass but gathers moisture as it travels across the Pacific Ocean before reaching the eastern sections of the Philippines is characterized by widespread cloudiness with rains and showers. The North Pacific Trades gradually replaces the NE Monsoon in March, appears in all seasons and blows dominantly from March to April, giving strong convective activity. 
SW Monsoon
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locally known as "Habagat", it affects the country from July to September, is very warm and humid, occurs when warm moist air flows over the country from the southwest direction, is characterized by heavy rainfall that may last for a week. It brings the rainy season to the western portion of the country. 

  
Linear Systems 
Description
Associated Weather
Period
Intertropical Convergence Zone (ITCZ)
Result of the northern hemisphere and southern hemisphere tradewind convergence
Widespread cloudiness, occasional thunder-storms, precipitation, moderate to strong surface winds
Migratory, depending on the time of the year
Tail-end of Cold Front
Front boundary of 2 air masses, found in mid-latitudes
Rainfall and cloudiness over affected areas
Northern portion of the country during the Northern Hemisphere winter season
Easterly Waves
Wavelike perturbations embedded in the easterly current
cloudiness and precipitation in eastern coastal portions
More frequent during the transition period

Tropical Cyclone Intensity / Category

  Intensity / Category
  Maximum Winds
  Tropical Depression
  Between 35 KPH and 64 KPH near the center
  Tropical Storm
  Between 65 KPH and 118 KPH near the center
  Typhoon
  119 to 200 KPH near the center
  Super Typhoon
  Maximum winds greater that 200KPH

Date of Download: Jan. 22, 2013