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Tornadoes are vertical funnels of rapidly spinning air. Their winds may top 250 miles an hour and can clear a pathway a mile wide and 50 miles long.

Also known as twisters, tornadoes are born in thunderstorms and are often accompanied by hail. Giant, persistent thunderstorms called supercells spawn the most destructive tornadoes.

These violent storms occur around the world, but the United States is a major hotspot with about a thousand tornadoes every year.

" Tornado Alley," a region that includes the area in the eastern state of South Dakota, Nebraska, Kansas, Oklahoma, northern Texas, and eastern Colorado, is often home to the most powerful and destructive of these storms. U.S. tornadoes cause 80 deaths and more than 1,500 injuries per year.

What is a tornado?

A tornado is a violently rotating column of air that extends from a thunderstorm to the ground. It's often portended by a dark, greenish sky. Black storm clouds gather. Baseball-size hail may fall. A funnel suddenly appears, as though descending from a cloud. The funnel hits the ground and roars forward with a sound like that of a freight train approaching. The tornado tears up everything in its path.

Every U.S. state has experienced twisters, but Texas holds the record: an annual average of 120. Tornadoes have been reported in Great Britain, India, Argentina, and other countries, but they are most often seen in the United States.

Related to tornadoes, waterspouts are weak twisters that form over warm water. They sometimes move inland and become tornadoes.

Dust devils are small, rapidly rotating columns of air that are made visible by the dust and dirt they pick up. Dust devils are not associated with thunderstorms. Either are fire tornadoes, which can spawn from wildfires.

What causes tornadoes?

The most violent tornadoes come from supercells, large thunderstorms that have winds already in rotation. About one in a thousand storms becomes a supercell, and one in five or six supercells spawns off a tornado.

Tornadoes can occur at any time of year, but they are more common during a distinct season that begins in early spring for the states along the Gulf of Mexico. The season follows the jet stream -as it swings farther north, so does tornado activity. May generally has more tornadoes than any other month, but April's twisters are sometimes more violent. Farther north, tornadoes tend to be more common later in summer.

Although they can occur at any time of the day or night, most tornadoes form in the late afternoon. By this time the sun has heated the ground and the atmosphere enough to produce thunderstorms.

Tornadoes form when warm, humid air collides with cold, dry air.

The denser cold air is pushed over the warm air, usually producing thunderstorms. The warm air rises through the colder air, causing an updraft. The updraft will begin to rotate if winds vary sharply in speed or direction.

As the rotating updraft, called a mesocycle, draws in more warm air from the moving thunderstorm, its rotation speed increases. Cool air fed by the jet stream, a strong band of wind in the atmosphere, provides even more energy.

Water droplets from the mesocyclone's moist air form a funnel cloud. The funnel continues to grow and eventually it descends from the cloud. When it touches the ground, it becomes a tornado.

Characteristics of tornadoes

Twisters are usually accompanied or preceded by severe thunderstorms and high wlnds. Hail is also common.

Once a tornado hits the ground, it may live for as little as a few seconds or as long as three hours.

The average twister is about 660 feet wide and moves about 30 miles an hour. Most don't travel more than six miles before dying out.

Massive tornadoes, however-the ones capable of widespread destruction and many deaths-can roar along as fast as 300 miles an hour.

These measurements are scientists' best estimations. Anemometers, which measure wind speed, cannot withstand the enormous force of tornadoes to record them.

Using units F0 to F5, the Fujita scale measures a tornado's intensity by analyzing the damage the twister has done and then matching that to the wind speeds estimated to produce comparable damage. The United States now uses the EF (Enhanced Fujita) scale, which takes more variables into account when assigning wind speeds to a tornado.

Tornado destruction

Every year in the United States, tornadoes do about 400 million dollars in damage and kill about 70 people on average.

Extremely high winds tear homes and businesses apart. Winds can also destroy bridges, flip trains, send cars and trucks flying, tear the bark off trees, and suck all the water from a riverbed.

High winds sometimes kill or injure people by rolling them along the ground or dropping them from dangerous heights. But most tornado victims are struck by flying debris-roofing shingles, broken glass, doors, metal rods.

The number of average deaths per year in the United States used to be higher before improved forecasting and warning systems were put into place.

How tornadoes are forecasted

Meteorologists at the U.S. National Weather Service use Doppler radar, satellites, weather balloons, and computer modeling to watch the skies for severe storms and tornadic activity.

Doppler radars record wind speeds and identify areas of rotation within thunderstorms. Since Doppler radar has been in use, the warning time for tornadoes has grown from fewer than five minutes in the 1980s to an average of 13 minutes by the late 2000s.

When weather conditions are conducive for tornado formation, the National Weather Service issues a tornado watch. When a tornado has been sighted or indicated on radar, a tornado warning is issued.

Some scientists, meteorology buffs, and adrenaline junkies hit the road during tornado season to chase storms. Researchers race to place sensors in tornadoes' paths. The sensors measure data such as wind speed, barometric pressure, humidity, and temperature.

The challenge for researchers is being in the right place at the right time. Every morning they study weather conditions and head for the area that seems most likely to spawn a twister. They drive through severe storms, dodge lightning, face flash floods, and get pounded by hail-sometimes for years-before ever spotting a tornado.

All at considerable risk. In 2013, National Geographic Explorer Tim Samaras and his team were killed while trying to study a tornado in Oklahoma. ( See photos of Samaras's work.)

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Learn how these deadly storms form and wreak havoc, and how you can reduce your risk.

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1. Cold air (below freezing) is needed to make snow.
For snow to fall to the ground, the temperature must be cold both up in the clouds where snowflakes form, and down at ground level. If the air near ground level is too warm, the snow will melt on its way down, changing to rain or freezing rain.

2. Moisture is needed to form clouds and precipitation.
Moisture in the air is called water vapor. Air blowing across a body of water, such as a large lake or the ocean, is an excellent source of water vapor. As wind moves air over the water, some water evaporates from the surface, putting vapor into the air. This is how "lake effect snowstorms" and "Nor'easters" pick up so much moisture. However, cold air is not able to hold much water vapor. In fact, very cold air does not make very much snow.

3. Warm, rising air is needed to form clouds and cause precipitation.
For a blizzard to form, warm air must rise over cold air. There are two ways that this may happen. Winds pull cold air toward the equator from the poles and bring warm air toward the poles from the equator. When warm air and cold air are brought together, a front is formed and precipitation occurs. Warm air can also rise to form clouds and blizzard snows as it flows up a mountainside.

What Are Snowflakes?

Snowflakes are made of ice crystals. Each snowflake is made of as many as 200 ice crystals.

Some snow crystals are symmetrical, like the type that you cut from paper. They form a hexagonal shape because that is how water molecules organize themselves as they freeze. Others are small and irregularly shaped. If they spin like tops as they fall to the ground, they may be perfectly symmetrical when they hit the Earth. But if they fall sideways, they will end up lopsided.

Even though most have a hexagonal structure, there are so many ways that water molecules can arrange themselves as the water freezes, that some people say that there are no two snowflakes alike. Probably no two snowflakes have exactly the same arrangement of molecules. But they can look alike. Many snow crystals are like the two in the photograph below. They are simple in shape and look alike.

How Snowflakes Form

Snowflakes form in clouds where the temperature is below freezing (0ºC, or 32ºF). The ice crystals form around tiny bits of dirt that have been carried up into the atmosphere by the wind. As the snow crystals grow, they become heavier and fall toward Earth. Different types of snowflakes form in different conditions. Temperature determines if the crystals become a flat plate, a long column, or a prism shape.

On average, 10 inches of snow melt down to about an inch of water; however, not all snow is the same. Some places receive very heavy snow. For instance, only five and a half inches of January snow on Mount Washington, New Hampshire, melt down to an inch of water. In contrast, over 15 inches of January snow at Crested Butte, Colorado, melt down to an inch of water.

Other Icy Precipitation
Snow is not the only type of ice that falls from the sky! Other types are described below.
Graupel: Snowflakes that have become encrusted with ice. This happens when snowflakes pass through a chilly cloud on their way down and water droplets freeze on them.

Ice pellets: Frozen raindrops, also known as sleet. They are usually quite small in size and unlike snowflakes, do not have a crystal shape.

Hail: A frozen raindrop or graupel that is kept from falling to the ground by the upward flowing air of a thunderstorm. The more droplets that freeze onto the hailstone, the longer the hailstone spends in the sky. When it finally grows too heavy to be held up by the flowing air, it falls to the ground like those in the picture to the right.

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1. Cold air (below freezing) is needed to make snow. For snow to fall to the ground, the temperature must be cold both up in the clouds where snowflakes form, and down at ground level. If the air near ground level is too warm, the snow will melt on its way down, changing to rain or freezing rain.

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Tornadoes, Hurricanes, Cyclones, Thunderstorms, Hailstorms, Snowstorms, and Sandstorms: Epic

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Tornadoes, Hurricanes, Cyclones, Thunderstorms, Hailstorms, Snowstorms, and Sandstorms: Epic

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They can speed across the ocean as fast as a jet plane, swallow up islands and wipe out villages.

But what causes tsuamis...? Join National Geographic Kids and dive into our tsunami facts to find out!

What causes a tsunami?

Meaning " great harbour wave" in Japanese, tsunamis are sometimes called "tidal waves" but their strength has nothing to do with the tides. About four out of five tsunamis happen within the Ring Of Fire, a zone in the Pacific Ocean where earthquakes and volcanic eruptions frequently take place.

Giant slabs of the Earth's crust, called tectonic plates, grind together. Sometimes, though, the plates get stuck, the pressure builds up and they suddenly slam into a new position. This causes an earthquake. If an earthquake lifts or drops part of the ocean floor, the water above rises and starts spreading across the ocean, causing a tsunami. Underwater landslides or volcanic eruptions can also displace water (cause water to spread across the ocean) and may lead to a tsunami.

How big is a tsunami?

Out in the open ocean, tsunami waves are only about one-metre high because the water is deep. However, as the water becomes shallow, the waves slow down and begin to grow. They can rise 35m or higher - that's the same as a 10-floor block of flats! However, the scariest thing about a tsunami is its wavelength, as this determines how far inland it can travel. Whereas a large wave caused by a storm might have a wavelength of up to 150m, a tsunami could reach up to a fearsome 1,000km!

How fast is a tsunami?

A normal wind wave travels at about 90kmh, but a tsunami can race across the ocean at an incredible 970kmh! Sometimes, before a tsunami hits, there is a huge vacuum effect, sucking water from harbours and beaches. People can see the ocean floor littered with flopping fish and other sea animals. Then a wave blasts onto the shore minutes later, then another and another for two hours or more. There may also be up to one hour between each wave.

Can you predict when a tsunami is coming?

To save lives, scientists established the Pacific Tsunami Warning System, based in Hawaii, in the USA. Its network of detectors can track quakes that may cause a tsunami. These waves can race from one side of the Pacific Ocean to the other in less than a day, so people need to be warned in time to head for higher ground!

What do you think of these tsunami facts? Let us know by leaving a comment, below!

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Tsunami facts: check out the mighty wave! - National Geographic Kids

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Check out these epic tsunami facts from National Geographic Kids! How do tsunamis form? And how big are they? Find out all about them in our tsunami facts...

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Enjoy our awesome range of Earth facts for kids. Check out the cool trivia and have fun learning about some of our planet's most amazing features.

Tsunami Facts

Check out our tsunami facts for kids and learn some interesting information related to these great walls of water that can cause so much destruction. Find out what causes tsunamis and read about some notable recent examples of tsunamis that have occurred around the globe.

Tsunamis are huge waves of water that are usually caused by earthquakes or volcanic eruptions.

As a tsunami approaches the shore, water may recede from the coast, if it is shallow enough the water may be pulled back hundreds of metres. If you are in the area, observing this is a good indication that a tsunami is on the way.

Regions in tsunami danger zones often have warning systems in place to give people as much time to evacuate as possible.

When tsunamis hit shallow water (often near the coast) they slow down but increase in height.

An earthquake in the Indian Ocean off Indonesia in December 2004 caused a tsunami that killed over 200000 people in 14 countries. More earthquake facts.

In March 2011, the Tohoku earthquake off the eastern coast of Japan caused a tsunami that was a major factor in the death of over 15000 people.

The tsunami waves created by the Tohoku earthquake reached heights of over 40 metres (131 feet) in some areas, wiping out coastal towns and causing a number of nuclear accidents.

The Japanese word tsunami literally means 'harbor wave'.

Tsunamis are sometimes referred to as tidal waves but this term has fallen out of favour because tsunamis are not related to tides.

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Tsunami Facts for Kids - Interesting Information about Tsunamis

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Enjoy our awesome range of Earth facts for kids. Check out the cool trivia and have fun learning about some of our planet's most amazing features. Tsunami Facts Check out our tsunami facts for kids and learn some interesting information related to these great walls of water that can cause so much destruction.

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Disasters don’t plan ahead. You can. Know what disasters and hazards could affect your area and learn what to do before, during, and after each type of emergency.

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Wherever there is a shortage of rain over a long period of time, there is drought. Drought affects plants, animals, and people. It is a serious problem for farmers and for the people who depend on the crops they produce.

Drought may occur almost anywhere in the world. Deserts receive very little rain all year. They are sometimes said to be in a permanent drought. Places that have a rainy season and a dry season have seasonal drought during the dry season. Other places can experience drought at any time.

Drought results from changes in Earth's atmosphere. Some droughts are caused by shifts in the winds that normally bring rain to an area. Others are caused by changing ocean currents, which affect the temperature and moisture of the air.

Severe droughts can last for months or years. When this happens no crops will grow. As a result many people and animals may die of famine, or lack of food. Severe droughts often force people and animals to move to find water. Some farmers go to places where they think conditions will be better for their crops and animals. Some people give up farming altogether. They move to cities to find other types of work.

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Wherever there is a shortage of rain over a long period of time, there is drought. Drought affects plants, animals, and people. It is a serious problem for farmers and for...

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What is a drought?
A drought is when there is a lack of precipitation over an extended period of time, usually a season or more, resulting in a water shortage for some activity, group, or environmental sector. Its impacts result from the interplay between the natural event (less precipitation than expected) and the demand people place on water supply, and human activities can exacerbate the impacts of drought.

What causes a drought?
Drought has many causes. It can be caused by not receiving rain or snow over a period of time. If you live in a place where most of the water you use comes from a river, a drought in your area can be caused by places upstream from you not receiving enough moisture. There would be less water in the river for you and other people who live along the river to use. People can also play a big role in drought. If we use too much water during times of normal rainfall, we might not have enough water when a drought happens.

Can scientists predict if a drought is going to happen?
No! Studies conducted over the past century have shown that meteorological drought is never the result of a single cause. It is the result of many causes including, global weather patterns, high pressure, the tropical outlook and other global-scale variables.

Are there places in the United States that experience drought?
Yes! The Western United States is experiencing an exceptional and extreme drought at this time. To see the map, Click Here to see the current U.S. Drought Monitor.

What was the Dust Bowl?
Of all the droughts that have occurred in the United States, the drought events of the 1930s are widely considered to be the "drought of record" for the nation. The 1930s drought is often referred to as if it were one episode, but it was actually several distinct events occurring in such rapid succession that affected regions were not able to recover adequately before another drought began. The term Dust Bowl was coined in 1935 to describe the drought-affected south central United States in the aftermath of horrific dust storms. Although it technically refers to the western third of Kansas, southeastern Colorado, the Oklahoma Panhandle, the northern two-thirds of the Texas Panhandle, and northeastern New Mexico, the Dust Bowl has come to symbolize the hardships of the entire nation during the 1930s.

How bad was the drought in the Dust Bowl years?
In the 1930s, drought covered virtually the entire Plains for almost a decade. The drought's direct effect is most often remembered as agricultural. Many crops were damaged by deficient rainfall, high temperatures, and high winds, as well as insect infestations and dust storms that accompanied these conditions. The resulting agricultural depression contributed to the Great Depression's bank closures, business losses, increased unemployment, and other physical and emotional hardships. Although records focus on other problems, the lack of precipitation would also have affected wildlife and plant life, and would have created water shortages for domestic needs.

What was the Black Sunday Dust Storm?
The 1930s were times of tremendous hardship on the Great Plains. Settlers dealt not only with the Great Depression, but also with years of drought that plunged an already-suffering society into an onslaught of relentless dust storms for days and months on end. They were known as dirt storms, sand storms, black blizzards, and "dusters." It seemed as if it could get no worse, but on Sunday, the 14th of April 1935, it got worse. The day is known in history as "Black Sunday," when a mountain of blackness swept across the High Plains and instantly turned a warm, sunny afternoon into a horrible blackness that was darker than the darkest night. Famous songs were written about it, and on the following day, the world would hear the region referred to for the first time as "The Dust Bowl."

How does a drought affect our lives?
Drought affects our lives in many different ways because water is such an important part of so many of our activities. We need water to live, and animals and plants do too. We need water to grow the food we eat. We also use water for many different things in our lives, like washing dishes, cooking, bathing, and swimming or river rafting. Water is also used to help make the electricity we use to run the lights in our houses and the video games you may like to play. When we don't have enough water for these activities because of a drought, many people and many different things will be affected in many different ways.

How can we help if we're in a drought?
One of the easiest steps we can take to help mitigate the impacts of drought is conserving water. If we use water wisely at all times, more water will be available to us and to plants and wildlife when a drought happens. We can lose a lot of water doing simple everyday tasks. Did you know that turning off the water while you brush your teeth can save more than 100 gallons of water a month? If you have a leaky faucet, the drips can add up to 300 gallons of wasted water a month.

What are the different types of drought?
There are four basic approaches to measuring drought: meteorological, hydrological, agricultural, and socioeconomic. The first three approaches deal with ways to measure drought as a physical phenomenon. The last deals with drought in terms of supply and demand, tracking the effects of water shortfall as it ripples through socioeconomic systems.

Meteorological drought is defined usually on the basis of the degree of dryness (in comparison to some "normal" or average amount) and the duration of the dry period. Definitions of meteorological drought must be considered as region specific since the atmospheric conditions that result in deficiencies of precipitation are highly variable from region to region. For example, some definitions of meteorological drought identify periods of drought on the basis of the number of days with precipitation less than some specified threshold. This measure is only appropriate for regions characterized by a year-round precipitation regime such as a tropical rainforest, humid subtropical climate, or humid mid-latitude climate.

Agricultural drought links various characteristics of meteorological (or hydrological) drought to agricultural impacts, focusing on precipitation shortages, differences between actual and potential evapotranspiration, soil water deficits, reduced groundwater or reservoir levels, and so forth. Plant water demand depends on prevailing weather conditions, biological characteristics of the specific plant, its stage of growth, and the physical and biological properties of the soil. A good definition of agricultural drought should be able to account for the variable susceptibility of crops during different stages of crop development, from emergence to maturity.

Hydrological drought is associated with the effects of periods of precipitation (including snowfall) shortfalls on surface or subsurface water supply (i.e., streamflow, reservoir and lake levels, groundwater). The frequency and severity of hydrological drought is often defined on a watershed or river basin scale. Although all droughts originate with a deficiency of precipitation, hydrologists are more concerned with how this deficiency plays out through the hydrologic system. Hydrological droughts are usually out of phase with or lag the occurrence of meteorological and agricultural droughts. It takes longer for precipitation deficiencies to show up in components of the hydrological system such as soil moisture, streamflow, and groundwater and reservoir levels. As a result, these impacts are out of phase with impacts in other economic sectors.

Socioeconomic definitions of drought associate the supply and demand of some economic good with elements of meteorological, hydrological, and agricultural drought. It differs from the aforementioned types of drought because its occurrence depends on the time and space processes of supply and demand to identify or classify droughts. The supply of many economic goods, such as water, forage, food grains, fish, and hydroelectric power, depends on weather. Because of the natural variability of climate, water supply is ample in some years but unable to meet human and environmental needs in other years. Socioeconomic drought occurs when the demand for an economic good exceeds supply as a result of a weather-related shortfall in water supply.

Aquifer - an area that contains large amounts of water under the surface of the earth.

Climate - day-to-day weather over a longer period of time. Climatology is the study of climate.

Climograph - a graph that shows monthly average temperature and precipitation for some location.

Dam - a structure built across a river to hold back water for a variety of reasons, including protecting areas from floods, storing water, and generating power.

Desalination - the process of removing salts and other minerals from seawater so that it can be used for drinking water.

Drought - less rainfall than is expected over an extended period of time, usually several months or longer. Or, more formally, it is a deficiency of rainfall over a period of time, resulting in a water shortage for some activity, group, or environmental sector.

Drought Index - a numerical scale that scientists use to describe the severity of a drought. Scientists take many kinds of data (like streamflow, rainfall, temperature, and snowpack) and "blend" it into a single number, called a drought index value, to make it easier to understand the drought conditions of a particular area. Drought indices are one type of drought indicator.

Drought I ndicator - a way to look at one or more variables, such as precipitation, to describe available water in soil or hydrologic systems. It may be a record of a single measurement, such as rainfall at a particular rain gauge. It may also be a complex index. Drought indices (indexes) are a subset of drought indicators.

Dust Bowl - an area of the U.S. Plains that included parts of Kansas, Colorado, Oklahoma, Texas, and New Mexico. The term was coined in the 1930s, when dry weather and high winds caused many dust storms throughout the United States, but particularly in this area.

Erosion - a process that wears the earth's surface away, causing soil to move from one place to another. It's a natural process, but human activities can make it worse.

Groundwater - water that is found underground in spaces in soil, sand, or rocks.

Hydroelectricity - electricity created by channeling water through turbines in power stations located below dams.

Irrigation - an agricultural practice that involves providing water to crops through pipes, ditches, or streams.

Mitigation - actions that we can take before, or at the beginning of, drought to help reduce the impacts of drought. Mitigation includes actions as diverse as drought planning, implementing land use practices that increase the organic content and water-holding capacity of soil, and designing agricultural policy that doesn't encourage short-term economic gains at the expense of long-term productive capacity. The Intergovernmental Panel on Climate Change uses mitigation to mean reducing emissions of greenhouse gasses.

Reservoirs - water that's collected and stored in natural or manmade lakes.

Submarginal Farmland - lands with nutrient-poor soils and/or soils that have been damaged by poor cultivation practices.

Water Banking - a water management strategy that temporarily transfers water from those who are willing to lease it to those who are willing to pay to use it.

Water Recycling - reusing treated wastewater for purposes like agricultural and landscape irrigation. It's also referred to as water reclamation or water reuse.

Xeriscaping - a type of landscaping around homes and businesses that uses a limited amount of water.

Click on the chart to make larger!

Click Here to see the current U.S. Drought Monitor!

Lesson Plan: Here is a lesson plan on water conservation.

Lesson Plan: Here is a lesson plan on how drought affect agriculture.

Science Fair Project Ideas: Here is a complete list of science fair project ideas. Discover the science behind the weather that impacts us every day.

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What is a drought? A drought is when there is a lack of precipitation over an extended period of time, usually a season or more, resulting in a water shortage for some activity, group, or environmental sector.

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Interested in learning more about tornadoes? Are you a student looking up information for a class project? Then you've come to the right place! We've put together these tornado facts for kids to help you with the learning and research process. You can learn more about tornadoes by visiting our Tornado Facts homepage.

If you're doing a school project you can freely use the information on this web page if you give properly reference this website. If you want to report any inaccurate information please contact us.

Tornadoes are also referred to as cyclones or twisters.

A tornado is a violent weather event.

A tornado generally has a grey color tint and looks like an elephant's trunk.

The majority of tornadoes have a wind speed than is less than 100 miles per hour.

The majority of tornadoes only travel a few miles before they dissipate.

The majority of tornadoes only last for a few minutes.

Extreme tornadoes can have wind speeds that reach 300+ miles per hour.

Extreme tornadoes can travel 100+ miles before they dissipate.

Extreme tornadoes can last on the ground for over an hour before they dissipate.

There are about 1,000 to 1,200 tornadoes annually in the United States.

The Fujita Scale andEnhanced Fujita Scale are used to measure the strength of tornadoes.

Areas in the U.S. with the most tornadoes are Texas, Oklahoma, Kansas and Florida.

The region(s) that have a frequent occurrence of tornadoes are called tornado alley.

The 1925 Tri-State Tornado was the deadliest tornado in U.S. history, it killed 695 people.

A tornado hit Bangladesh in 1989 and killed 1,300+ people making it the deadliest tornado ever.

Doppler radar is used to detect tornadoes by looking for large rotating updrafts in supercells.

A tornado that forms or travels over water is called a waterspout.

Tornadoes in the southern hemisphere usually rotate clockwise.

Tornadoes in the northern hemisphere usually rotate counterclockwise.

A tornado watch is issued when the conditions are right for the formation of a tornado.

A tornado warning is issued when a funnel cloud has been sighted or a meteorologist has detected a tornado using Doppler radar.

A basement, storm cellar or underground area is the safest place to be during a tornado.

You might also want to check out our web page with general tornado facts. If you live in an area with a high occurrence of tornadoes we recommend you read our web page with tornado safety facts. Head on over to our tornado myths archive to learn about all the misinformation surrounding torandoes.

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Interested in learning more about tornadoes? Are you a student looking up information for a class project? Then you've come to the right place! We've put together these tornado facts for kids to help you with the learning and research process. You can learn more about tornadoes by visiting our Tornado Facts homepage.

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Kid's learn about the science of earthquakes. What causes them and where they happen.

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The ground shakes, buildings tumble and the earth heaves and cracks. Serious earthquakes are terrifying and dangerous, but are rare in the U.S. But why do earthquakes happen? The earth is made up of four layers - the inner core, outer core, mantle and crust. The mantle and crust are a thin skin compared to the other layers.

The mantle is about 1,750 miles thick, while the crust is only about 8 miles thick. This thin skin is broken into pieces called tectonic plates. The plates are like puzzle pieces, floating on top of the Earth's inner core. Sometimes the pieces slide under or against each other and become stuck.

When the pieces slide apart, they create tremendous force. This force causes the earth to shake and ripple. Over 80 percent of the earth's earthquakes happen in the Pacific Ocean, in a place known as the "Ring of Fire." Annually, around 10,000 people die in earthquakes every year. Most of the deaths happen when people are trapped in falling buildings. After an earthquake, mudslides, fires and tsunamis can also hurt people.

Fun Facts All About Earthquakes for Kids

Alaska, California and Hawaii have the most earthquakes in the U.S. Other western states, like Nevada, Idaho, Washington and Oregon are prone to earthquakes or can be damaged by earthquakes that happen in Alaska and California.

Alaska has more earthquakes than any other U.S. state. It has experienced over 12,000 earthquakes in the last 30 years. Alaska is followed by California, Hawaii, Nevada, Washington, Idaho, Wyoming, Montana and Utah.

Underneath the Earth's surface lie tectonic plates. These plates move and shift over time. Sometimes they slide under one another or push up against each other, creating enormous stress. When they move again, they cause an earthquake.

Scientists who study earthquakes are called seismologists.

Seismologists can tell how serious an earthquake is by a machine called a seismogram, which rates the intensity of the quake's shaking.

Scientists can use special instruments to record an earthquake's strength. An earthquake rated 3 to 5 is minor; an earthquake rated 5 to 7 is moderate to strong; an earthquake rated 7 to 8 is major; an earthquake rated 8 or above is great.

On average, one earthquake measuring 8 or above happens every year.

The area near Japan in the Pacific Ocean has the most earthquakes in the world. This area also has a lot of volcanoes. It is called the Ring of Fire.

Most people who die in earthquakes die when buildings collapse on them. Others die in floods, fires or mudslides that happen after the earthquake.

May 22nd 1960 in Valdivia Chile the largest ever recorded Earthquake measuring a whopping 9.5 magnitude struck.

December 26th 2004 an Earthquake in the Indian Ocean measuring a magnitude of 9.1 on the Richter Scale resulted in a massive Tsunami hitting the region which resulted in the deaths of over 230,000 people.

March 11th 2011 off the coast of Honshu Japan a magnitude 9.0 earthquake caused a massive Tsunami to hit the coast. The Tsunami caused over 18,000.

On our planet earth we have four different types of dip-slip-faults and they are Normal - Reverse - Thrust - Strike Up.

Earthquake Vocabulary

Learn More All About Earthquakes and Why They Happen

Imagine that you're sitting in school when the ground begins to shake. Books fall off the shelves and you might even be thrown from your chair. That's what happens when an earthquake occurs. Earthquakes are the most deadly of all natural disasters. Over 10,000 people die every year in earthquakes.

Easy Science All About Earthquakes for Kids Video

Watch this interesting video all about earthquakes:

Earthquake Q&A

Question: Do all earthquakes cause damage?

Answer: Most earthquakes cause only minor shaking. Southern California has about 10,000 earthquakes every year. Some of them are so mild people don't even feel them.

------------

Question: What can I do to be safe in an earthquake?

Answer: If you're in a building in an earthquake, get under a table or desk and hold onto it. If you're outside, move to an open area away from trees, buildings or power lines.

------------

Question: What should I do to keep safe in an earthquake?

Answer: The best way to survive an earthquake is to take cover under a sturdy table. Get down low and place your hands over your head. You can even duck down in a door frame or curl up next to a couch or bed. Don't go outside, though. Many people die from falling debris.

Enjoyed the Natural Science for Kids website all about Earthquakes info? Take the FREE & fun all about Earthquakes quiz and download FREE all about Earthquakes worksheet for kids. For lengthy info click here.

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All About Earthquakes and Why They Happen Fun Science Facts for Kids. Learn more all about Earthquakes through our Easy Earth Science for Kids website.

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Learn the science behind how earthquakes happen—and how you can stay safe if one hits.

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Nor'easters can occur in the eastern United States any time between October and April, when moisture and cold air are plentiful. A Nor'easter is named for the winds that blow in from the northeast and drive the storm up the east coast along the Gulf Stream, a band of warm water that lies off the Atlantic coast. They are known for dumping heavy amounts of rain and snow, producing hurricane-force winds, and creating high surfs that cause severe beach erosion and coastal flooding. Winter Storms

How do winter storms form?
Winter storms derive their energy from the clash of two air masses of different temperatures and moisture levels. Winter storms usually form when an air mass of cold, dry, Canadian air moves south and interacts with a warm, moist air mass moving north from the Gulf of Mexico. The point where these two air masses meet is called a front. If cold air advances and pushes away the warm air, it forms a cold front. When warm air advances, it rides up over the denser, cold air mass to form a warm front. If neither air mass advances, it forms a stationary front.

What are snowflakes?
Snowflakes are made of ice crystals. Each snowflake is six-sided and made of as many as 200 ice crystals. Snowflakes form in clouds where the temperature is below freezing. The ice crystals form around tiny bits of dirt that has been carried up into the atmosphere by the wind. As the snow crystals grow, they become heavier and fall toward the ground. Why is snow white?
Bright snow blinds us with its gleaming white color because it reflects beams of white light. Instead of absorbing light, snow's complex structure prevents the light from shining through its lattice formation. A beam of white sunlight entering a snow bank is so quickly scattered by a zillion ice crystals and air pockets that most of the light comes bouncing right back out of the snow bank. What little sunlight is absorbed by snow is absorbed equally over the wavelengths of visible light thus giving snow its white appearance. So while many natural objects get their blue, red, and yellow colors from absorbing light, snow is stuck with its white color because it reflects light.

What is thundersnow? How is snow formed?
Snow is commonly formed when water vapor undergoes deposition, which is when water vapor changes directly to ice without first becoming a liquid, high in the atmosphere at a temperature of less than 32°F and then falls to the ground. What is sleet?
Sleet is just rain drops that freeze into ice pellets before reaching the ground. Sleet usually bounces when hitting a surface and does not stick to objects. However, it can accumulate like snow and cause a hazard to motorists.
What is an ice storm?
An ice storm is a type of winter storm caused by freezing rain. The U.S. National Weather Service defines an ice storm as a storm which results in the accumulation of at least 0.25-inch of ice on exposed surfaces.
What is freezing rain?
Freezing rain is just rain that falls onto a surface with a temperature below freezing. This causes it to freeze to surfaces, such as trees, cars, and roads, forming a coating or glaze of ice. Even small accumulations of ice can cause a significant hazard. How do ice storms form?
Ice storms form when a layer of warm air is between two layers of cold air. Frozen precipitation melts while falling into the warm air layer, and then proceeds to refreeze in the cold layer above the ground. This creates freezing rain or a glaze of ice.

What is frost? What is a frost quake?
Frost is white ice crystals that form on a surface, like the ground or leaves of a plant. Frost is created when the air temperature drops below freezing and the water vapor in the air freezes into ice crystals.

How is lake-effect snow formed?
As the cold air flows over the warm lake water, the relatively warm water heats the air's bottom layer as lake moisture evaporates into the cold air. Since warm air is lighter or less dense than cold air, the heated air rises and begins to cool. As the air cools, the moisture that evaporated into it condenses and forms clouds and snow begins falling from the cloud if the air is humid enough. (Graphic Credit: USA TODAY.) What is a Nor'easter?

What is Wind Chill? What is an Alberta Clipper? Click Here to calculate the Wind Chill.
An Alberta clipper is an area of low pressure that generally forms over Alberta, Canada, east of the Rocky Mountains. They develop east of the Rockies because air flowing eastward over the mountains creates favorable conditions. Once an Alberta Clipper forms it usually moves very rapidly to the southeast across the USA's northern Plains and then to the east off the mid-Atlantic Coast. Clippers usually cause only light precipitation with very few producing major snowstorms. However, if conditions are favorable, some Alberta clippers can rapidly intensify off the East Coast once the storm taps the relatively warm moist air over the Atlantic Ocean. The storms that rapidly intensify sometimes spread heavy snow over New England and southeastern Canada. Generally, the main weather features associated with Alberta clippers are some light snow and a reinforcement of cold air over the USA.
What is frostbite? How do blizzards form?

A blizzard is a long-lasting snowstorm with very strong winds and intense snowfall. You need three things to have a blizzard; cold air at the surface, lots of moisture, and lift. Warm air must rise over cold air.
What is an avalanche?
An avalanche is a moving mass of snow that may contain ice, soil, rocks, and uprooted trees. The height of a mountain, the steepness of its slope, and the type of snow lying on it all help determine the likelihood of an avalanche. Avalanches begin when an unstable mass of snow breaks away from a mountainside and moves downhill. The growing river of snow picks up speed as it rushes down the mountain. Avalanches have been known to reach speeds of 245 miles an hour (394 kilometers per hour)—about four times as fast as the speediest downhill skier.
Click Here to learn more about Avalanche Saftey.
Know the Lingo
WINTER WEATHER ADVISORIES - Issued for accumulations of snow, freezing rain, freezing drizzle, and sleet which will cause significant inconveniences and, if caution is not exercised, could lead to life-threatening situations.

Thundersnow is when thunder and lighting occur during a snowstorm. This occurs most often in late winter or early spring. To get thundersnow, you need a mass of cold air on top of warm air, plus moist air closer to the ground. Thundersnow starts out like a summer thunderstorm. The sun heats the ground and pushes masses of warm, moist air upward, creating unstable air columns. As it rises, the moisture condenses to form clouds, which are jostled by internal turbulence. The "tricky part" for making thundersnow is creating that atmospheric instability in the wintertime. For thundersnow to occur, the air layer closer to the ground has to be warmer than the layers above, but still cold enough to create snow. During thundersnow events, heavy snowfall is to be expected. In some cases, two inches per hour is possible.

Click Here to see if there are any active warnings in your area.

Winter Storm Safety Tips
BEFORE A WINTER STORM: Have a disaster plan and prepare a disaster supplies kit for your home and car. Include a first aid kit, emergency food supply, bottled water, battery-operated radio, flashlight, protective clothing, and blankets. Don't forget, be aware of changing weather. DURING A WINTER STORM: Stay indoors and dress warmly. Eat regularly, because food provides the body with energy for producing its own heat. Also, drink lots of water. If you must go outside, wear layered clothing, mittens and a hat. Watch for signs of hypothermia and frostbite. Remember to keep dry. Always change wet clothing to prevent the loss of body heat. If you must drive, carry a cell phone. Always, keep the gas tank full. Don't forget, let someone know where you're going, just in case your car gets stuck. If you're car gets stuck, stay with it and wait for help unless help is visible within 100 yards. Use maps and car mats to stay warm.

AFTER A WINTER STORM: Avoid driving until conditions have improved. Avoid overexertion! Heart attacks from shoveling snow are the leading cause of deaths during the winter. Also, check on neighbors to make sure they're okay.

Frost quakes are non-tectonic seismic events, meaning they are not caused by the shifting of the Earth's tectonic plates. Also known as cryoseisms, frost quakes are caused by a sudden rapid freezing of ground and bedrock, usually when temperatures go from above freezing to below zero. As moisture absorbed in the rock and soil freezes, it expands. This puts a great amount of stress on the areas around it. Eventually, the stress is too much and the soil and rock will crack in an "explosive" manner, creating a loud sound and even shaking the ground surface. Since temperatures are coldest in the overnight hours, most people experience frost quakes in the middle of the night. Winter Storm Activities
Lesson Plan: Here is a great lesson plan on learning about winter weather. In this activity, kids investigate aspects of winter weather, such as temperature and wind. They familiarize themselves with weather-related words. It's a great activity for K-2nd graders.

Cold air moves over warm water and is warmed from below. Moisture evaporates in the air.

Warm moist air rises downwind of lakes and forms heavy snow.

Lesson Plan: Here is a great lesson plan on learning about winter weather. In this activity, kids learn how winter storms form and about the different types of fronts. It's a great activity for 3rd-5th graders. Note: This is a PDF file, so you need to have Adobe Acrobat Reader.
Measuring Snow Experiment: Here is a great experiment that lets kids measure snow. They let the snow melt and then measure it again. It teaches kids that snow is very dense and is why it holds more space than water.

The wind chill is the temperature your body feels when the air temperature is combined with the wind speed. The higher the wind speed the faster exposed areas of your body lose heat and the colder you feel.Melting Snow Experiment: Here is another experiment that teaches kids the difference between the freezing and melting process. It allows kids to take the temperature of a glass of snow. Then, watch the snow melt and observe how the temperature changed.

Frost Experiment: Here is a great experiment that lets kids make frost. They can see how dew turns into frost in a matter of minutes.Examining Snowflakes Experiment: Here is a great experiment that lets kids see snowflakes up close. They can examine the snowflake's six sides.
Pressure Experiment: Here is an experiment that shows how pressure is created in our atmosphere by sucking an egg in a bottle. This is a very cool experiment!
Science Fair Project Ideas: Here is a complete list of science fair project ideas. Discover the science behind the weather that impacts us every day.
Make A Barometer Experiment: Here is an experiment that allows the kids to make a barometer.

Evaporation Experiment: Here is an experiment that shows kids how evaporation takes place.

Frostbite is damage to the skin due to prolonged exposure to cold temperatures, usually below 32° F.

WINTER STORM WATCH - Alerts the public to the possibility of a blizzard, heavy snow, heavy freezing rain, or heavy sleet. Winter Storm Watches are usually issued 12 to 48 hours before the beginning of a winter storm.

WINTER STORM WARNING - Issued when hazardous winter weather in the form of heavy snow, heavy freezing rain, or heavy sleet is occurring. Winter Storm Warnings are usually issued 12 to 24 hours before the event is expected.

BLIZZARD WARNING - Issued for sustained or gusty winds of 35 mph or more, and falling or blowing snow creating visibilities at or below 1/4 mile. These conditions should persist for 3 hours.

FROST/FREEZE WARNING - Issued when below freezing temperatures are expected.

LAKE EFFECT SNOW ADVISORY - Issued when accumulation of lake effect snow will cause significant inconvenience.

LAKE EFFECT SNOW WARNING - Issued when heavy lake effect snow is occurring.

WIND CHILL ADVISORY - Issued when the wind chill temperature is forecast to be between -15°F to -24°F.

WIND CHILL WARNING - Issued when the wind chill temperature is forecast to be -25°F or lower.

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Weather Wiz Kids weather information for kids

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Weather Wiz Kids is a fun and safe website for kids about all the weather info they need to know. It contains tools for weather education, including weather games, activities, experiments, photos, a glossary and educational teaching materials for the classroom.

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What is a blizzard? How does a blizzard form?

According to The Weather Channel a blizzard is a storm with "winds of at least 35 mph, and visibility reduced by falling and/or blowing snow to less than 1/4 mile." These conditions must last for at least 3 hours. Snow forms when two air masses collide one with warm air and one with cold air they collide and make a front if there is more cold air it creates a snow if there is more warm air it will just rain. When this snow is combined with the wind, and decreased visibility, it forms a blizzard.

How blizzards affect people....

- A blizzard can shut down a city, sometimes for days. Transportation can be impossible. This means kids miss school and adults cannot get to work. People can be stuck in their homes for days.

- Electrical wires often go down because of the heavy wind and snow. This leaves people with no electricity. Without electricity, people can't use computers, TVs, appliances, and lights.

- If people are caught outside in a blizzard, they risk getting frost bite and hypothermia.

- A blizzard can cause lots of property damage, such as roof cave-ins and windows breaking. Trees can fall on houses, cars, etc.

- Blizzards can be the cause of lots of car accidents. Cars can be stranded on highways too.

-Blizzards are life threatening storms. People have died in blizzards.

- Blizzards can hurt the economy. People can't get to work. Jobs don't get done. Businesses and stores lose money.

How blizzards affect the land....

- Trees, plants, and crops can die in a blizzard, because of the extreme cold.

- Tree branches and limbs can break.

- Flooding can happen after a blizzard. This happens when there is a warm up after having large amount of snow. The snow starts melting faster than land can absorb it.

How blizzards affect animals....

- Blizzards can be life threatening to pets, farm animals, etc. They can die if exposed to the cold. They can also get lost and not be able to find their way home during a blizzard.

- Pets should not be left outside during a snow storm or a blizzard.

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According to The Weather Channel a blizzard is a storm with "winds of at least 35 mph, and visibility reduced by falling and/or blowing snow to less than 1/4 mile." These conditions must last for...

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The word "hurricane" comes from 'Huracan', the god of big winds and evil spirits once worshiped by the Maya people of Central America. Here we take a look at some cool hurricane facts.

First - what is a hurricane? A hurricane is an intense tropical storm with powerful winds and heavy rain and can also create tornadoes, high waves and lots of flooding.

Where do hurricanes form?

They usually form in tropical parts of the world like the southern Atlantic Ocean, Caribbean Sea, Gulf of Mexico, and in the eastern Pacific Ocean. The Atlantic hurricane season lasts from June to November, with the peak season being from August to late October.

So, no visiting at those times then. Make sure your parents plan their holiday properly! The Eastern Pacific hurricane season begins on May 15 and ends November 30. Evaporation (when liquid changes to gas) from the seawater also increases their power.

The heat dissipates (reduces) as the hurricane moves toward the poles, sometimes causing extreme damage for people living along the coastlines where hurricanes take place.

Some Info about Hurricanes

Hurricanes range from about 100 miles (160 kilometers) to 1000 miles (1600 kilometers) wide. They can last from days to weeks and almost always form over the ocean.

They can have speeds over 200 miles per hour (322 kilometers per hour), with things flying all over and be can also have heavy rains with them, which can cause land/mud slides.

What needs to happen for a hurricane to form?

The ocean waters must be warm enough at the surface - about 80° Fahrenheit (26⁰ Celsius) or warmer to put enough heat and moisture into the atmosphere.

Atmospheric moisture from sea water evaporation must cool off very quickly and combine the heat and energy to form the powerful engine needed to propel the hurricane.

A wind must be blowing in the same direction and at the same speed to force air upward from the ocean surface. Bands of thunderstorms form, allowing the air to warm even more and rise higher into the atmosphere.

Winds flow outward above the storm and the air below rises. If the winds at the higher levels are not that strong, the structure can remain intact and grow stronger and this is the beginning of a hurricane.

When hurricanes come onto land, the heavy rain, strong winds and large waves can damage buildings, trees and cars.

The eye of the hurricane

The eye of a hurricane is the calmest spot. It is generally 20 (32 kilometers) to 30 miles (48 kilometers) wide. Amazingly the hurricane can be about 400 miles (644 kilometers) wide. The most violent activity takes place in the area immediately around the eye, called the "eyewall".

At the top of the eyewall, which is up to 50,000 feet (15,240 meters), most of the air is driven outward, which increases the upward motion of the air. Some of the air, however, moves inward and sinks into the eye. This actually creates a cloud-free area.

Hurricane winds in the northern hemisphere circulate in a counter-clockwise motion around the hurricane's centre or "eye," while hurricane winds in the southern hemisphere circulate clockwise. Wow, that's amazing!

Storm surges are usually the most devastating part of a hurricane. As a hurricane's winds spiral around and around the storm, they push water into a mound at the storm's centre. This mound of water becomes dangerous when the storm reaches land because it causes flooding along the coast.

The water piles up, unable to escape anywhere but on to land as the storm carries it forwards. A hurricane will cause more storm surge in areas where the ocean floor slopes gradually and this will cause major flooding.

The amount of surge that a hurricane can cause is measured on machines called Slosh Models. What a weird name.

From 1953 the United States Weather Bureau started naming hurricanes using women's names for North Atlantic hurricanes. The rest of the world eventually caught on, and now the World Meteorological Organization, is responsible for naming hurricanes.

It uses different types of names dependent on the part of the world the storm is in. Around the US only women's names were used. Then in 1979 they decided men's names should be used as well. If a hurricane creates huge damage, its name is retired and replaced with another.

Here are a few of the names from the 2015 list: Ana, Bill, Claudette, Danny, Erica, Fred. There are many more!

There are brave "hurricane hunters" who work for the National Oceanic and Atmospheric Administration (NOAA). Each mission lasts about ten hours, with the crews passing four to six times through the storm. Can you imagine? That just sounds crazy!

The planes carry radar, sophisticated computers and weather instruments that measure temperature, air pressure, wind speed, and wind direction inside the hurricane. The crews also release instruments that measure temperature, air pressure, and wind at different levels as the devices drop through the hurricane toward the ocean.

By mission's end, NOAA can warn everyone in the hurricane's path. At least it's a massive help to people.

Hurricanes can be tracked by weather satellites and weather radar closer to land.

What was one of the worst hurricanes in history?

One of the worst hurricanes in history was the Galveston hurricane in the 1900s, which devastated the city and killed between 6,000 and 12,000 people - mostly from drowning. That's frightening.

The 1970 Bhola Cyclone that struck Bangladesh killed over 300,000 people. Cyclones, hurricanes and typhoons are just different names for the same thing.
Earth Science

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Hurricane Facts For Kids The word "hurricane" comes from 'Huracan', the god of big winds and evil spirits once worshiped by the Maya people of Central America. Here we take a look at some cool hurricane facts. First - what is a hurricane?

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Hold on tight, gang - and we mean super tight! - because we're about to check out ten facts on one of nature's most powerful forces - hurricanes!

1. Hurricanes are giant tropical storms that produce heavy rainfall and super-strong winds.

2. Hurricanes form over warm ocean waters near the equator. The warm, moist air above the ocean surface rises, causing air from surrounding areas to be "sucked" in. This "new" air then becomes warm and moist, and rises, too, beginning a continuous cycle that forms clouds. The clouds then rotate with the spin of the Earth. If there is enough warm water to feed the storm, a hurricane forms!

3. Hurricanes rotate around a circular centre called the " eye ", where it is generally calm with no clouds. Surrounding the eye is the eye wall - the most dangerous part of the hurricane with the strongest winds, thickest clouds and heaviest rain!

4. Most hurricanes occur harmlessly out at sea. However, when they move towards land they can be incredibly dangerous and cause serious damage.

5. The strong spiraling winds of a hurricane can reach speeds of up to 320kmph - strong enough to rip up entire trees and destroy buildings!

6. In the southern hemisphere, hurricanes rotate in a clockwise direction, and in the northern hemisphere they rotate in an anti-clockwise direction. This is due to what's called the Coriolis Force, produced by the Earth's rotation.

7. When a hurricane reaches land it often produces a " storm surge". This is when the high winds drive the sea toward the shore, causing water levels to rise and creating large crashing waves. Storm surges can reach 6m high and extend to over 150km!

8. Hurricanes are also called cyclones and typhoons, depending on where they occur. In the Atlantic Ocean and Northwest Pacific they are hurricanes, in the Northwest Pacific they are typhoons and in the South Pacific and Indian Ocean they are cyclones.

9. The largest hurricane on record is Typhoon Tip, which occurred in 1979 in the northwest Pacific. With a diameter of around 2,220km, it was nearly half the size of the United States!

10. Hurricanes are given names by the World Meteorological Organisation (WMO) so that they can be distinguished. Each year, tropical storms are named in alphabetical order according to a list produced by the WMO. That name stays with the storm if it develops into a hurricane. The names can only be repeated after six years.

Photos: Getty Images UK

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10 Facts about Hurricanes! - National Geographic Kids

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Check out ten top facts about hurricanes here at National Geographic Kids! Learn how hurricanes form, what the world's biggest hurricane is and more!

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