2015年5月31日星期日

What Colors to Wear with Orange Clothes

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Oh, so you finally got a very pretty orange blouse, but aren't sure what color to pair it with? We tell you about all things orange, and help you make the right clothing choices in this post. Read on.
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Orange color outift for women
Orange is a color of liberation from the pains of hurtful love and inner insecurities. To "Channel orange" is to be truly free. To be you.
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—Frank Ocean

Add a pop of color, some brightness, and lots of happiness with the most exciting color - orange! Fresh and funky orange is a very versatile color, and will give your wardrobe that much-needed color boost. Are you apprehensive about wearing orange? Yeah, most people are! But that could be b'coz you don't know what colors to pair with orange.

This fierce color symbolizes warmth, energy, happiness, and so much more. But the most important thing is... it looks so good! It's time to make heads turn and unleash the diva or the dude in you... with some ORANGE!

White And Bright!

orange and white

Looks awesome, isn't it? White is the color when you gotta balance a bright shade. Whether it's a dress, skirt, pants, or anything else, the orange and white pairing works, period.

A Little Subdued...

orange gray beige

So you don't like too much attention, and flashy is not really your style. Let's tone it down a little, with some neutral colors. Pair orange with beige or gray, and so you will love the effect.

No... We Like It Bright!

orange with bright colors

orange with other colors collage

Colors, and more colors! You don't wanna look like a rainbow, so do pair them right. Blue or green complements orange really well. A great shade of yellow (not too bright please) works really well as well. And, the pink and orange combination is so fresh and different!

Formal Or Casual... Orange Rocks

Orange clothes collage of Men

Orange looks equally alluring on men, the image is a proof! A formal orange shirt looks very smart. Pairing a casual tee with orange pants will work wonders as well. So don't shy away from orange guys!

Orange Fervor

orange dress collage

Why pair orange with other colors when you can go totally orange! A printed orange dress looks totally awesome, and you can also pair different shades of orange for an ethereal effect!

Get Sassy With Black

orange with black pants

orange and black clothes collage

How can you not pair any color with black? Black is the best thing when it comes to fashion! This combination will work wonders if you choose matte orange shades rather than bright ones. And yes, it will also remind people of Halloween! :P

Orange Blast Or Just a Pop!

full and partial orange

Gold and orange looks very stylish. Your simple orange dress will instantly turn glamorous with the perfect golden belt. If you don't like orange much, and yet wanna flaunt it, go for a bright orange belt!

The Orange Quotient!

orange jacket or scarf

Yes, you can go for orange accessories as well. Look how smart the burnt orange jacket looks. A bright scarf will instantly take your outfit a few notches high.

Divine Denim!


orange and denim skirts

orange and denim for women

orange and denim for men

We love the whole orange and denim combo. It's casual, fresh, and even men can carry orange with elan! Yes guys, it's fine to wear orange sometimes, we are not asking you to wear pink! It's time to get out of the stereotypical cliches and embrace colors!

Complement It Right


shoes with orange

You need perfect shoes to make your orange dress look all the more awesome. Go for bright blue heels on a plain solid orange dress or blouse. Gold is another color that instantly lifts up orange. If your clothes just have a hint of orange, then wear bold orange shoes, and white is always on the list!

accessories with orange

You can match your earrings to your shoes. Gold and orange or blue and orange themes work really well. Feel free to experiment with jewelry and other accessories, but don't go for a solid or bright color with orange.
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So, now that you know how to flaunt orange, go and paint the town pink, err... orange!

2015年5月28日星期四

26 Famous Quotes by Rabindranath Tagore

Rabindranath Tagore, a great poet, writer, artist, and a Nobel laureate from India, has contributed greatly to the field of literature. A visionary, and torch-bearing personality with deep profound thoughts, his quotes will certainly chant a hymn that our hearts will truly understand. Be it nature, religion, god, country, love, life or freedom, Tagore's words are real jewels.
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Rabindranath Tagore quote
Did You Know?
The National Anthem of India, Jana Gana Mana, was penned by Rabindranath Tagore.
Nobel laureate Rabindranath Tagore was a great connoisseur of art and literature. Famous for his collection of poems, 'Gitanjali', in Bengali, he was one of the most famous and profound writers of his time who played a pivotal role in India's struggle for independence against the British.

Tagore was born in Calcutta (now, Kolkata), India, in 1861, in a wealthy family. Besides authoring many stories and poems of immense literary value, he also started the experimental school Shantiniketan, which broke away from traditional methods of learning and teaching school curriculum. Till date, the school has produced many eminent personalities including Nobel Prize winner for economics, Amartya Sen. His poems and literary work became very popular in the West too, and he was conferred with the Nobel Prize in Literature in 1913. Tagore was not only a writer, but also a true artist in all forms, and his works included drawings, paintings, and music compositions.

Apart from this, Rabindranath Tagore's literary works espoused freedom of mind and spirit. This proved highly inspirational for the general public who were struggling to gain independence from British rule. However, he also prompted readers, through his works, to free themselves from blind faith, caste discrimination, oppression against women, etc. Here are some quotes by Tagore that are certainly thought-provoking.

Quotes On Love

"Love is an endless mystery, for it has nothing else to explain it."

"Only in love are unity and duality not in conflict."

"Beauty is simply reality seen with the eyes of love."

rabindranath tagore quote on love

"I will sit in the pupil of your eyes and that will carry your sight into the heart of the things."

Quotes On Nature

"Let your life lightly dance on the edges of
Time like dew on the tip of a leaf."

"The butterfly counts not months but moments, and has time enough."

"The roots below the earth claim no rewards for making the branches fruitful."
― Stray Birds

"By plucking her petals you do not gather the beauty of the flower."
― Stray Birds

rabindranath tagore quote on butterfly

"The flower which is single need not envy the thorns that are numerous."

"Clouds come floating into my life, no longer to carry rain or usher storm, but to add color to my sunset sky."
― Stray Birds

"The world speaks to me in colours, my soul answers in music."

"Trees are the earth's endless effort to speak to the listening heaven."

rabindranath tagore quote on nature

Quotes On Death

"Death is not extinguishing the light; it is only putting out the lamp because the dawn has come."

"And because I love this life
I know I shall love death as well.
The child cries out when
From the right breast the mother
Takes it away, in the very next moment
To Find in the left one
Its consolation."

Quotes On God and Religion

"Men can only think. Women have a way of understanding without thinking. Woman was created out of God's own fancy. Man, He had to hammer into shape."
- The Home and the World

"Every child comes with the message that God is not yet discouraged of man."

"When I stand before thee at the day's end, thou shalt see my scars and know that I had my wounds and also my healing."

rabindranath tagore quote on woman

Quotes On Education

"Children are living beings - more living than grown-up people who have built shells of habit around themselves. Therefore it is absolutely necessary for their mental health and development that they should not have mere schools for their lessons, but a world whose guiding spirit is personal love."

"The highest education is that which does not merely give us information but makes our life in harmony with all existence."

"Don't limit a child to your own learning, for she was born in another time."

Quotes On Country and Freedom

"Deliverance is not for me in renunciation. I feel the embrace of freedom in a thousand bonds of delight."
― Gitanjali


"Where the mind is without fear and the head is held high; Where knowledge is free; Where the world has not been broken up into fragments by narrow domestic walls; Where words come out from the depth of truth; Where tireless striving stretches its arms towards perfection; Where the clear stream of reason has not lost its way into the dreary desert sand of dead habit; Where the mind is led forward by thee into ever-widening thought and action - Into that heaven of freedom, my Father, let my country awake."
― Gitanjali

Other Quotes

"Facts are many, but the truth is one."

"If no one responds to your call, be not afraid to walk alone."
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"Dreams can never be made captive."
― The Gardener

"It is very simple to be happy, but it is very difficult to be simple."

2015年5月27日星期三

How Does the Foucault Pendulum Prove Earth's Rotation?

Can a pendulum that swings back and forth right here on the surface of Earth demonstrate and prove conclusively that the Earth rotates about its axis? Read this  post to find the answer.
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Foucault pendulum proves Earth's rotation
Did You Know?
The Principia housed at the Oregon Convention Center is the world's largest Foucault pendulum. It comprises a 900-pound ball which is suspended using a 70-foot long cable. It swings continuously at a height of 20 feet over the heads of the visitors.
Without ogling at the heavens through a giant telescope, or making a quick trip to the International Space Station, will you be able to prove conclusively that the Earth rotates around its axis? Seems to be a near impossible task, doesn't it? However, as was demonstrated by the French physicist Jean Bernard Leon Foucault back in the 1800s, it is possible to do that, right here on Earth itself.

Born in 1819, Foucault was the son of a French publisher. From an early age he showed exceptional skill at making mechanical toys. He studied medicine, but later moved on to the study of physical sciences at the Paris Observatory. Foucault is widely regarded as one of the most gifted and versatile experimentalists of all time. He is credited with the invention of the gyroscope, which is an important instrument used to indicate a fixed direction during rapid motions. It forms an important part in many navigational systems used today.

In 1851, Foucault devised an innovative experiment to verify the Earth's rotation. His main apparatus was a large pendulum, which later came to be known as the Foucault pendulum in his honor. Here, we shall find out how the Foucault pendulum proves that the earth rotates. However, before that, let's examine a few important concepts in physics, that form the basis of this experiment.

Pendulums and the Concept of Inertia

Sir Isaac Newton explained that if an external force is applied to a body, it will begin moving in a straight line. This body will then continue its linear motion until another external force is applied to interrupt/redirect it. Newton termed this ability of a body to resist any changes in its state of motion, including both speed as well as direction of motion, as Inertia.

A good example of the effect of inertia is when the brakes in the vehicle you are sitting are applied suddenly. While the vehicle comes to a stop due to friction, inertia causes your body to continue moving forward until you stop yourself using your hands or with the help of seat belts. This is experienced as a sudden jerk.

Pendulums are devices that work on the concept of inertia. They typically comprise a bob which is usually a weighted sphere that is suspended from one end of a taut wire or string, while the other end is held in one's hand or tied to a fixed point at some height.

When the bob is pulled back and released, it descends down and moves forward under the influence of gravity and inertia receptively, until the length of the string limits its travel. After that, it swings back out and up again due to the same forces.

Thus, the pendulum continues to swing freely under the influence of gravity and inertia opposed only by the air surrounding it. The amount of inertia developed depends on the weight of the bob, which also determines the time it takes for air resistance to stop the pendulum from swinging.

The more the weight of the bob and longer the length of its swing, the more will be the time for which it will continue swinging. Air resistance will continue to counter its motion and decrease its speed, finally bringing it to a stop.

Demonstration of the Foucault's Pendulum Experiment

To understand the working of the Foucault's pendulum, lets carry out a simpler version of his original experiment. The following image displays the setup.

Foucault Pendulum Two Pegs
Foucault Pendulum With Two Fallen Pegs

As seen in the figure above, a pendulum is constructed by suspending a sufficiently heavy ball on a long wire/string which is attached to a fixed point on the roof of a high ceiling, wide hall or room. The ball needs to be heavy and the wire long enough so that the pendulum is able to overcome the air resistance and continue swinging for a long duration.

A number of light wooden pegs are arranged circularly and equidistant from each other on the floor below the pendulum. These pegs are chosen such that they fall easily on coming in contact with the heavy ball, without affecting the velocity or altering the direction of its swing. The ball is then pulled up and tied to a stable stationary point in the room with the help of a small piece of string.

To begin the experiment, this string is burnt which frees the pendulum and sets it swinging. The reason why this method of burning a string is used, is that prevents the accidental introduction of any angular momentum, because for our experiment to work properly, we need the ball to swing back and forth in a nearly straight line.

Arranged correctly, on the very first swing of the ball, it knocks down two diagonally opposite pegs (as shown), that lay in the path of its swing. The ball then continues to oscillate without disturbing any of the other standing pegs. This is allowed to happen for a while, ensuring that the pendulum's swing and the rest of the experimental setup remains undisturbed.

Foucault Pendulum Four Pegs
Foucault Pendulum With Four Fallen Pegs

After a sufficiently long period of time (typically about an hour or more), the pendulum knocks down another two diagonally opposite pair of pegs as shown in the image above. As more and more time elapses, the pendulum periodically keeps knocking down the standing pegs, until the air resistance finally slows it down, finally bringing it to a halt, thus ending the experiment.

Observation and Explanation

In the above demonstration, we observed that the pendulum continued to swing along the same line, under the influence of gravity and its own inertia alone. There was no external force acting on it which could have altered its trajectory. Despite that, it seemingly rotated in the plane of its swing, and was able to knock down more sets of diagonally opposite pegs.

The only explanation for this phenomenon is that while the pendulum swung back and forth, undisturbed, along a straight line, the Earth and therefore the floor beneath the pendulum moved, thus rotating the circle of pegs along with it. This caused more of the standing pegs to come in the line of the pendulum's swing, and so they too were knocked down. Essentially, the plane of oscillation of the pendulum remained constant, while the Earth beneath it moved, changing the orientation of the floor with respect to it.

Now, the way the floor below moves with respect the constant swing-plane of the pendulum, is dependent on the location on Earth's surface where this experiment is carried out. This is shown in the image below.

Foucault Pendulum Earth Rotation
Respective Motion of the Floor at Different Locations

If the experiment is carried out exactly at either the North or the South pole, the Earth and building floor will rotate beneath the pendulum's plane taking one sidereal day (23.93 hours) to complete the rotation and make all the pegs fall.

If the experiment is conducted somewhere along the Equator, the building will co-rotate along with the Earth, traveling eastward along the Earth's axis. As there will be no twisting of the floor, after the initial pair of pegs fall, none of the other pegs will be knocked off.

If the experiment is conducted at some place between the pole and the Equator, the motion of the building floor, viewed with respect to the constant swing-plane of the pendulum, will be a combination of rotation and traveling. This will result in it being twisted beneath the pendulum, albeit at a slower rate than the rotation of the Earth. The pendulum doesn't share this twisting motion, and hence, its plane of swing remains constant while the floor changes orientation so that the pegs are knocked out sequentially.

The degree of twist per day (n) is given by the following formula:

N = 360º sin φ

If the Foucault's pendulum is used at 30º south latitude, it will twist by 180º per day and will complete a full rotation in two days.

Thus, with the help of a Foucault pendulum, we can conclusively prove that the Earth rotates about its axis.

The Original Foucault's Pendulum Experiment

To prove that the Earth rotates, Léon Foucault carried out the pendulum experiment at the Meridian of the Paris Observatory in February 1851. Some weeks later, he carried out the demonstration once more with the help of a 28 kg, brass-coated lead bob which was suspended from the dome of the Panthéon in Paris, with the help of a 67-meter long metal wire.

Once this pendulum began oscillating, it was observed that the pendulum swings regularly changed directions in the clockwise direction at the rate of approximately 11 degrees per hour completing a full circular rotation in 32.7 hours, thus proving that the Earth rotates.
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In conclusion, the Foucault pendulum is one the simplest and most elegant ways to prove Earth's rotation. Since its initial demonstration, it has garnered a lot of interest in the general as well as the scientific communities. Today, there are several Foucault pendulums around the world, found mainly at universities, science museums, and planetariums. To prevent air resistance from slowing down and stopping the pendulums, many of these places utilize electromagnetic drives, motors, etc., to keep the bob oscillating continuously for the audience to see. Thus, the Foucault pendulum experiment still finds a lot of appeal among the young and old alike.

2015年5月26日星期二

7 Good Photo Sharing Apps That Aren't Instagram

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7 Good Photo Sharing Apps That Aren't Instagram
Currently, there is a 'love it or leave it' dilemma being played out in people's minds about the tremendously popular app, Instagram. If your pointer is slightly tilted toward the 'leave it' part, consider the following picture-sharing apps that are similar to Instagram.
Good photo sharing apps
What led to the fall of Instagram?
The misinterpreted version of Terms of Services of Instagram says, it owns your photographs and the authority to use and sell them to advertising parties.
We don't think there's anybody out there who wouldn't be aware of this hilarious app. Even if you aren't into photography, you probably know this photo-sharing app. It has brought a revolution in the filter-editing and social networking world.
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But an unfortunate incident in the form of the 2012 Instagram controversy led to the loss of followers in large numbers. Though Instagram released a statement regarding the misinterpretation of its terms of services, there are users who no more feel secure.

Whether you're interested in enhancing your pictures, are a photography fancier, or just not sure about being on insta, we've got some great picture-sharing and editing apps for you. We don't promise to give you alternatives that are free, but these are definitely worth a download.

Flickr
Platform: iOS, Android | Price: Free

You may think Flickr is dead, but think again. Yahoo just gave it a makeover, and it's all set to amaze you with its sparkling new interface and of course, photo hosting service. It's got advanced photo-editing options, amazing live filters, an option for adding captions, and lets you share them on Facebook, Twitter, Tumblr, or email. You can shoot from the app itself, or put a new spin on a previously clicked image. It has expanded ways to connect with people and browse pictures around the world. And the best part, there are no issues with licensing on your photos―you own them all.

Download from Google Play
Download from iTunes

EyeEm
Platform: iOS, Android | Price: Free

This photo-sharing social network app is very similar to Instagram, and for some photography enthusiasts, much better than it. It boasts sharing of pictures that are similar in type. For instance, if you post a picture of hot chocolate, it will showcase your picture to all those who've posted about hot choc, and also show you pictures of the same beverage uploaded by others (spare the hot chocolate part). It provides an automatic tagging system that will give you relevant tags, location, and data on every picture taken. The sharing feature is the most robust of all, letting you share via email, on Facebook, Twitter, Flickr, Foursquare, and Tumblr.

Download from Google Play
Download from iTunes

Hipstamatic
Platform: iOS, Windows | Price: USD 1.99

Wanna swim back to the retro world? This insta alternative is all you need. It has an old-camera-style user interface that comes with innumerable vintage-styled filters. The feature that differentiates it from the crowd is that it lets you apply effects before clicking a snap and offers group albums. It turns your pictures into postcard-like snaps which you can share not just on Facebook and Twitter, but also on Instagram and Flickr. Hipstamatic promises to make your digital photography look analog, and well, we say they are pretty successful in doing it.

Download from iTunes

pixlr-o-matic
Platform: iOS, Android | Price: Free

This is your standard phone camera with a 20+ insta-like filters, overlays, frames and border options. If time is a constraint, or if you're too jumbled by the various options, you can go in for the 'randomizer' option given by it that would select an effect, overlay, and border/frame for you. You can share your edited pictures on Facebook, Flickr, DropBox, iTunes, or email. And the good news is, it has a desktop version too. If you've fallen in love with the effects it offers, try its plus version (can cost you up to $1.) with more exciting overlays and effects.

Download from Google Play
Download from iTunes

snapseed
Platform: iOS, Android, Windows | Price: USD 4.99

This is one of the priciest apps on the list, but trust me, it's worth the USD 4.99 tag. This image-enhancing app offers a number of features beyond mere filters. With just a simple swipe, you can fine-tune your photographs. Its photo correction capabilities are incomparable, making it one of the best iPhone camera apps. And last but not the least, it lets you complete control over your pictures.

Download from Google Play
Download from iTunes

Camera+
Platform: iOS, Android | Price: USD 0.99 - USD 1.99

This is probably the most well-loved iPhone photo editing app. Its interface is not just attractive, but also intuitive! Besides having an excellent camera, it serves just-like Instagram. It offers a huge set of filters, scene modes, borders, shooting options like stabilizer and separate exposure, and other insta-like effects, but with a professional touch to it. The only drawback here is that it isn't as social as insta. We say, despite having great post-shot polishing features, it expertise area is capturing the best picture possible.

Download from Google Play
Download from iTunes

CAMERA AWESOME
Platform: iOS, Android | Price: Free
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This SmugMug camera app is blazing fast. With easy-to-use interface, you get 9 awesome features for free including―presets, filters, textures, etc. Besides, you can buy several other features for gaining more control over editing options―giving you nearly 300 effects and editing tools. The 'Awesomize' feature serves you with powerful auto-fixes. You can share your pictures across Facebook, Twitter, Flickr, YouTube, or you can leave it all on its auto-share feature.

2015年5月25日星期一

How Was the Himalayan Mountain Range Formed?

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The Himalayas are one of the most magnificent natural structures on Earth. In this article, we shall explore the physical process which has been instrumental in the formation of this great mountain range.
Himalayan mountain range formation
Did You Know?
The theory of continental-drift, put forth by the German meteorologist Alfred Wegener in around 1912, is the most widely accepted theory that explains the formation of the Himalayas.
Stretching for approximately 2,900 km (1,800 m), the Himalayas are literally the roof-top of the world. These mountains, which are located between four countries: Pakistan, India, China, and Nepal, are the tallest on Earth.
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The Himalayan mountain range is the only one on our planet that comprises mountain peaks which rise over a staggering 8,000 meters. The tallest one among them―Mount Everest―rises to a breathtaking 8,848 meters, making it the tallest mountain peak on Earth.

So what was it that caused these mountains to attain such enormous proportions, becoming bigger than anything on Earth? How were they formed? Let's find out.

Plate Tectonics

In geology, a plate is a large rigid slab of solid rock. It is believed that the outermost layer of the Earth is divided into a number of small and large plates that float atop the hotter, denser, and more mobile material underneath, which is driven by the internal heat of the Earth. As such, these plates too are in motion, albeit at much slower speeds.

The term tectonics in Greek means 'to build'. Together, the term plate tectonics refers to the theory which describes how the surface of the Earth, as we see today, was built by the motion of the plates underneath.

Presently, it is thought that there are seven giant plates and a few other smaller ones that are in motion relative to each other on the Earth's surface. All the continents and the oceans lie on top of these plates. However, millions of years ago, there may have been more or less of these plates.

Pangaea Formation and Break-up: Continental Drift

Nearly 300 million years ago, all the major continents that we see today: Asia, Africa, North America, South America, Antarctica, Europe, and Australia, were absent. Instead, there was only a single giant super-continent, known as the Pangaea, which was located predominantly in the southern hemisphere of the Earth.

Pangaea was formed due to the movement of tectonic plates. It is believed that millions of years ago, giant accumulations of rock debris that spread over the tectonic plates were brought together when the plates moved towards each other. This caused the amalgamation of these debris into one giant debris, which gave rise to the Pangaea.

However, the movement of the plates continued on even after this. As a result, this super-continent began disintegrating into distinct pieces, each carried atop moving tectonic plates. Some of these pieces moved apart, while others collided and combined with one another, forming the continental landmasses that we see today.

How the Himalayan Mountains were Formed

Several million years ago, the grand Himalayan mountain range that we see today, did not exist. The Asian continent stood where it is today, but the Indian subcontient was nowhere in its vicinity. India, in fact, was an island floating near the coast of Australia.

Around 220 million years ago, when the Pangaea was breaking apart, the landmass of India, carried atop the Indo-Australian plate, began its slow migration northwards, towards the Eurasian plate on which the massive continent of Asia lay.

India Asia Collision
Collision of India and Asia

Nearly 80 million years ago, India was located 6,400 km (4,000 m) to the south of the continent of Asia. Over the span of the next several million years, India kept on traveling north, at an estimated rate of 5 - 15 cm/year, until it finally collided with Asia.

Before this collision took place, there existed a vast sea, known as the Tethys, which stretched latitudinally on the site that is presently occupied by the Himalayan mountain range. As India closed-in upon Asia, several rivers from it, in addition to those from Asia, began depositing large amounts of sediments into the seabed of the Tethys which lay in the middle. This large-scale deposition made the Tethys very shallow.

Approximately 55 million years ago, India began closing-in on Asia, covering up the Tethys sea. When the two landmasses finally collided, 10 million years ago, the Tethys sea was completely closed. Due to the enormous impact, the already shallow seabed, which by now had a large accumulation of sediments, rapidly folded and was elevated, rising up high and forming longitudinal ridges and valleys. This was the birth of the Himalayas.

As India continued its northward ascent, it began to wedge itself underneath the Asian continent. This happened because the northern coastline of India was denser and much more firmly attached to the seabed, as compared to Asia. Therefore, when these gigantic landmasses collided, India wedged itself underneath, causing the softer soil of the southern coastline of Asia to be pushed upward, rather than the other way round. This pushed the Himalayas, along with the entire Tibetan region upwards, further adding to the height of this enormous mountain range.

Tectonic Plates Collision
Formation of the Himalayas

As the Indian subcontinent continued pushing against Asia, the Himalayas continued to rise. This mountain range rose and spread very rapidly; much faster than most other mountain ranges on the Earth. In fact, the Himalayas are still growing even today. Everest and its siblings are known to grow by a few centimeters each year. This is in contrast to many other mountain ranges, such as the Appalachian Mountains, which were formed around 300 million years ago, and are actually becoming smaller due to erosion.

The reason why the Himalayas are still growing is the same as the one behind its formation - the movement of tectonic plates. The plate carrying India is still moving northwards, as is evidenced by the frequent earthquakes that occur in and around the surrounding region. Therefore, as long as this tectonic activity continues to take place, the Himalayas will probably continue to rise.

Now, if you were to calculate the tentative height of the Himalayas based on its current rising rate for the nearly 40 million years of its existence, you would find that it should be around 400 km tall! To put things in perspective, the International Space Station orbits the Earth at a height between 300 - 400 km (185 - 250 m). So why was it that these already gigantic mountains have not reached the mammoth proportions that the calculations predict?

One of the reasons is that, the rate of vertical growth of the Himalayas over the years has been variable, and some of force originating from the push of India against Asia has been subverted in favor of horizontal growth and expansion. The other likely reasons are the Earth's gravity and erosion, which have significantly reduced the growing potential and the height of the Himalayas.

The Future of the Himalayas

Owing to the continued northward motion of India, the Himalayan region remains geologically active, and continues to rise. Scientists believe that this rate of growth is likely to remain constant for the next 5 - 10 million years. This fact allows us to get a fair estimate of the development of this mountain range, and its effects on the surrounding region in the coming future.

Ten million years from now, India will plow an estimated 180 km into Tibet. Nepal lies between the lower boundary of the Himalayas and to the upper border of the plains of India. Due to India's motion, in the distant future, Nepal will cease to exist, but the Himalayan mountain range will remain, and continue to advance on India.
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Continued geological activity will cause frequent earthquakes in this unstable region. The physical structure of this mountain range will comprise large mountains in the north and smaller ones to the south. They will continue to grow, and also be eroded at the same time. However, the net effect will most likely be that, the Himalayas will get bigger and even more spectacular with time.

2015年5月24日星期日

Things You Need to Know About Icebergs

It is common knowledge that icebergs are large floating chunks of ice. However, these frozen behemoths are very deceptive, and there is a lot that we don't know about them. In this article, we shall look at a few interesting facts, such as where icebergs come from, how they are formed, and much more.
Fact about icebergs
Fast Fact!
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The term 'iceberg' refers to large pieces of ice that are wider than 5 meters (16 feet). Smaller chunks of ice are known as 'growlers' or 'bergy bits'.
Like penguins or polar bears, icebergs too are very unique and symbolic to the polar regions, so much so that Greenlanders once used them to identify seasons and towns. The term 'iceberg' is borrowed from the dutch word 'ijsberg', which literally means ice mountain. This name is apt, as icebergs are usually large, magnificent mountainous masses of free-floating ice, that wander the oceans till they melt. While these slabs of ice look sterile and devoid of life, they actually harbor complete ecosystems, and have a big impact on any ecosystem that they may pass through.

Icebergs seem to either exude awe or an aura of danger, as they move around in oceans at higher latitudes, creating an atmosphere of peril for ships, similar in manner to naval mines. However, they also hold a lot of promise. Apart from helping oceanographers and other scientists in their studies, it has been proposed to tow icebergs to drought stricken areas to solve water shortage problems, but the logistics and possible environmental damage has deterred any such effort to be made so far.

Interesting Facts About Icebergs
Origins and Formation
When glaciers on land form due to snowfall over several hundred years, each new layer of snow compresses the ones below it, until glacial ice is formed around 70 meters below the surface. The glacier gradually creeps towards open sea under its own weight, and once it reaches the water, the edges of the glacier breaks off due to the motion of the tides, and slips into the ocean, and icebergs are formed. This process is called calving. The ice usually floats with the sea currents, gradually melting with a fizzing sound as it moves towards warmer waters.

Most of the world's icebergs come from around Antarctica, the glaciers of western Greenland, and the glaciers near Canada's arctic area. As of now, 30,000 - 40,000 icebergs are formed each year. Because they have an interior temperature of -15 to -20 degrees Centigrade, many of them travel thousands of miles and take at least a year or two to melt completely.

Composition
Due to the fact that icebergs are found at sea, they are wrongly assumed to be formed of salty sea water. In reality, they are made of pure freshwater and snow. Therefore, the ice is completely safe to consume. In rare cases, melted water in the glacier or dust from volcanoes may enter the iceberg's crevasses. This can cause the structure to acquire blue, brown, or blackish streaks.

Streaked Iceberg
Flipped Iceberg Showing Blue Streaks

Physical Characteristics
Icebergs are made of ice that may be around 10,000 years old. Due to their massive size, many of them weigh over 10 million tons, although you may also find a few smaller ones which could weigh anywhere between 100,000 and 200,000 tons. Despite their weight, they float in ocean water, because water is denser as a liquid (density of seawater is 1025 kg/m3) than as a solid (density of pure ice is 920 kg/m3). Also, icebergs contain a large amount of air bubbles, which gives them their white appearance, and increases their buoyancy.

However, due to their immense weight, they float with only about ⅞ to ⅒ of their mass above the water. Also, the width of the ice below the water is around 20 - 30% larger than what is above the surface. So, the only natural source affecting their movement significantly is the ocean currents, which push them around at a leisurely pace ranging between 0.4 and 2.2 mph. When near land, icebergs often get stranded, and create deep and wide troughs in the sea bed, which can last for decades.

Iceberg Types
Icebergs can be classified into various categories, depending on their size and shape:
Classification by Size

Very Large Iceberg: These are the biggest and heaviest varieties, and icebergs come under this category if they are larger than 75 meters in height, and 200 meters in length.
Large Iceberg: The second-largest type, these can be as big as a sports stadium, with heights ranging between 46 - 75 meters in height, and 121 - 200 meters in length.
Medium Iceberg: Getting as big as a medium-sized hotel, these range between 16 - 45 meters in height, and 61 - 120 meters in length.
Small Iceberg: These small icebergs are about as big as a small building, and range between 5 - 15 meters in height, and 15 - 60 meters in length.
Bergy Bits: Although not considered as true icebergs, these cottage-sized chunks of ice come in sizes between 1 - 5 meters in height, and 5 - 15 meters in length.
Growlers: The smallest type in the iceberg family, these pieces of ice are smaller than 1 meter in height, and 5 meters in length.

Iceberg Shape Chart
Iceberg Shape Categories
Classification by Shape

Tabular: They have a generally flat appearance, and their height is significantly lesser than their width/length. Most of them are seen to be composed of numerous horizontal bands of ice of different shades.
Blocky: These are also a flat-topped variety, but they have steep, tall sides and heights, which are not very different from their width.
Wedged: Another flat-surfaced type, these icebergs have steep, tall cliffs on one side, from where the top slopes gradually go downward to the opposite side, giving it the appearance of a wedge.
Dome: Largely similar to tabular and blocky icebergs, domes differ only by having a smooth and rounded top.
Pinnacle: This variety gets is name by having at least one prominent spire or pyramidal section of ice on it.
Dry Dock: These icebergs have two or more pinnacles, and also a U-shaped slot between the spires close to the water level.

Depending on the shape and size, icebergs can be very unstable, and can even flip over without any warning, which can be highly dangerous. The action of rolling over can release as much energy as an atomic bomb, resulting in tsunamis and earthquakes. While the tabular varieties are generally stable, the wedge or dome-shaped ones are prone to rolling around.

The World's Largest Iceberg
The tallest known iceberg was seen in the North Atlantic ocean, which rose approximately 170 meters above sea level. Considering that the majority of its mass was below water, it was estimated to be as tall as a 60-storey building. However, this is not even close to the size of the biggest icebergs on record. Recently, in 2000, an iceberg named B-15 was spotted by satellite imagery. It was almost as big as the state of Connecticut, measuring over 4,200 square miles. However, even this iceberg was dwarfed by a tabular iceberg spotted by the USS Glacier in 1956, which measured more than 12,000 square miles, and was estimated to be larger than Belgium.

Dangers That Icebergs Pose to Ships
Titanic Disaster
Titanic and the Iceberg
The ice in icebergs is about 10% as strong as dry concrete, and although this does not seem very hard, the size, weight, and momentum of these huge chunks of ice make them extremely dangerous to colliding ships. The large underwater mass of ice is usually sharp and not easily visible, especially in the case of bergy bits and growlers, increasing the chances of an accident. Therefore, the idiom 'tip of an iceberg' is used to indicate situations where a person may be able to see only a part of the whole picture, leading to problems.

An area located 250 miles east and southeast of Newfoundland has been named Iceberg Alley, due to the exceedingly high number of icebergs there, which make conditions for shipping quite treacherous. In a collision with an iceberg, an immense force of hundreds of tons is subjected on the ship's hull, which causes massive catastrophes such as the RMS Titanic disaster of 1912. In that accident, the British ocean liner was traveling towards New York through the Iceberg Alley when it struck an iceberg and sunk with over 1,500 people. While most sea disasters take place due to rough seas and storms, the Titanic sank due to the sea being too calm, as the lookouts could not see waves crashing onto the iceberg, nor the phosphorescence of algae, on that moonless night.

To stop such disasters from ever happening again, the US and 12 other nations got together and created an organization named the International Ice Patrol. Today, this organization uses radar and airplanes to monitor the movement of icebergs which are floating into major shipping lanes. Satellite data is also used to monitor large icebergs floating around Antarctica. However, since the number of ships have increased drastically since 1912, the chances of an accidents still exists. In fact, between 1980 and 2005, there have been over fifty incidents involving sea vessels and icebergs.

Tips to See Icebergs

Your best bet for viewing icebergs is to travel towards the north on the eastern coast of Newfoundland and Labrador, as most icebergs are located in this area near Greenland. It is recommended that you take a guided tour, as the local tour operators would have the requisite experience to get you close to the icebergs without putting you in danger.
Although much riskier, people also use individual kayaks or scuba dive near the icebergs to get some great photographs. But one should never attempt to climb onto one, as the risk of injury and death is quite high.
To get some good photographs, search for different colored streaks, tunnels, caves, rocks, etc., embedded inside the ice. Also look for seabirds that might perch on top of the iceberg. If the bird flies off suddenly, there is a chance that the ice is breaking apart or rolling over, which is also a real visual treat.
The best time to view icebergs is late May or early June, when there is a good chance of spotting seabirds and whales as well.
If you are planning to watch icebergs from land, make sure that you carry a binocular or telescope to increase the chances and quality of a sighting.
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Why are Icebergs Important?
Icebergs play an important role in the sea, by leaking nutrients into the ocean waters around them. Studies have shown that areas near icebergs are usually teeming with sea-life, such as fish and plankton. The freshwater being added into the sea can influence ocean currents around the world, which can drastically affect global climate. Therefore, it is important that oceanographers pay significant attention to them. By studying the breakup of icebergs as they near warmer waters, scientists can predict how the ice shelves of the Arctic and Antarctic region will react to the warming climates of the world in the future.

2015年5月21日星期四

7 Different Types of Taxes That You Pay

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In the U.S., taxes are collected by the federal, state, and local governments. By the law, every working individual is required to file tax returns before a particular date, depending on the type of tax. This article enlists the 7 different types of taxes you pay in the U.S.
Types of taxes that you pay
Astonishing Facts!
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The federal tax code of the US amounts to almost 6000 pages - and contains more than three million words.
In 2010, the tax collection by the US government contributed to almost 25% of the GDP.

Taxation in the U.S. can be rather complicated. The purpose of levying taxes is to obtain revenue to keep the government running and provide public services. Different types of taxes are imposed on working individuals to achieve the same. There are certain tax deductions that can be reduce taxable income, like mortgages, charity, medical bills, etc.

There is no exemption from taxes however. After all, taxation plays an important role in the financial decision-making of a nation. Taxes are very widely classified. The paragraphs below provide some of the important tax types and their descriptions.

An Introduction to the Tax Structure

As mentioned earlier, in the U.S., taxes are collected by the federal and state governments.
There are two principal types of taxes―direct and indirect.
In simple terms, direct taxes are paid directly to the government or any authorized entity, while indirect taxes are collected via a series of taxpayers―mostly by means of increase in the prices of goods.
From an economic perspective, direct taxes are levied on and collected directly from a specific group of people.
Indirect taxes are collected from an organization other than the people actually responsible for the taxes.
Examples of direct taxes include income tax, wealth tax, etc. Examples of indirect tax include excise duty, sales tax, service tax, etc.


Main Types of Taxes

Income Tax

Income tax is levied on every working individual, and is collected by the Internal Revenue Service (IRS).
The states and local governments have their own income taxes as well.
The tax is levied on your personal income, interest income, and revenue from business.
Income tax brackets are generally progressive―the more you earn, the more taxes you pay.
Federal tax rates are higher than the state tax rates.
You can reduce your taxable income by means of certain allowances and deductions.
Remember that not all states have imposed a state tax. A federal income tax is mandatory though.


Property Tax

This is imposed by most local governments, since it is used to finance local services.
The tax is levied on real estate (mostly) and may apply to their property too.
This tax is deductible, and many American citizens may qualify for a interest deduction on mortgage. However, legally, the tax is deductible only if the real estate property is used for public welfare.
Since the tax is imposed on realty, it always depends on the market value of the property. The annual rates may vary between 0.9% to 1.2% of the property's current value.
The total tax amount collected is used to fund public services, such as schools, sanitation, security, etc.
The amount is paid to the local government or the county, based on the state guidelines.


Payroll Tax

The federal as well as state governments make it compulsory to pay payroll taxes.
It is a tax that the employer pays on behalf of the employee, i.e., the amount is deducted from his paycheck.
It is authorized by the Federal Insurance Contribution Act (FICA), and hence, is also called FICA tax.
There are two types of payroll taxes in US―Social Security tax and Medicare. Every employed individual in the U.S. is supposed to have a Social Security number.
Medicare and Social Security are federal run programs that provide benefits, generally for American citizens. Payroll taxes are used to finance these programs. The tax amounts to 7.65% of the income, of which 6.2% is for Social Security, and 1.45% is for Medicare.


Sales Tax

It is a type of indirect tax and is imposed on purchased goods and services.
The amount varies as per the price of the goods as well as the set rules and regulations of the state. Mostly, it is a percentage of the paid price.
It is levied on most of the purchased products, except food items. Also, some states/counties/cities charge a nominal amount on the product price, while others may charge a hefty amount. The percentage varies between 0 to 16%.
The amount is collected by the merchants at the time of sale and deposited with the state authority.
The types of sales tax include vendor tax (it is paid by the person doing business, and depends on the amount of goods sold), consumer tax (it is paid by the buyer at retail outlets and then sent to the state), and a combination tax.
This tax is considered regressive, since families with lesser annual income end up paying a major part of their salary for sales tax.


Excise Tax

Also called excise duty, it is similar to sales tax, except that it is levied on particular goods.
Also, it depends on the number of goods sold, not the amount.
The Federal government may impose a certain percentage of tax on every liter of oil, irrespective of the price per liter.
An excise tax may be charged on items, like beer, cigarettes, gas, etc.
States may charge an additional tax on these goods as well.
This tax is also called 'sin tax', since they are mostly imposed on such goods that are harmful to health. The purpose of excise tax is to make an effort to minimize the purchase of unhealthy items. It is mostly combined with sales tax.


Estate Tax

It is also called inheritance tax. It is levied by the Federal government and some of the state governments too.
The property you leave behind after your death is called estate. If you have more estate than required, the estate tax is to be paid on the inheritance of the property by your heirs.
That is to say, if you have a lot of property―including business revenue, security, cash, insurance, etc., and you distribute the property among your kith and kin, they will have to pay heavy estate tax on the same.
The federal government charges a maximum of 40% of the property for estate tax, while the states use comparatively lower rates. In some states, the amount paid depends on the relation between the deceased and the taxpayer.


Gift Tax

It is similar to the estate tax, but is levied on a large amount of transferred wealth. The wealth here may include shares, donations, cars, etc.
All gifts above USD 14,000 are taxable. The tax collected is 40% of the gift value.
The federal government charges a much lower amount for gifts as compared to estates.
If you plan to leave a huge number of assets for your heirs, it is advisable to seek advice from a tax professional and organize the assets.


Miscellaneous Taxes Paid

Capital Gains Tax: It is paid on the sale of stocks and bonds. You may also be subject to a capital gains tax on the sale of real estate.

Hotel Tax: It is the amount that hotels charge above the regular room rate.

Use Tax: It is paid for the different services that you use, like toll, licenses, cell phone, air travel, rental cars, lease, etc.

Luxury Tax: It is imposed on expensive items like jewelry or automobiles.

Fuel Tax: It is a type of user tax imposed on use of fuel―diesel, oil, gasoline, etc. The money is used for the maintenance of roads and highways.

Corporate Income Tax: It is levied by the states on huge corporations. The amounts vary as per the state.

Unemployment Tax: It is paid to unemployment agencies to help people find jobs. It is levied by the federal government.

Foreign Tax: It is the income tax imposed by the government of the foreign country. You have to pay a percentage of whatever income is earned by you in that country.
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Failure to pay taxes on time may lead to severe repercussions. As a responsible citizen, it is essential to pay taxes on time. You may seek advice from a tax professional if you are confused about which taxes you have to pay.