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Muneer G Babar
Works at International Medical University Malaysia
Attended Khyber College of Dentistry
Lives in Kuala Lumpur
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A beautiful day 
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Master Excel PivotTables in 1 Hour with this Free Webinar:

http://www.myonlinetraininghub.com/registration-xpt-nov15
Learn how to quickly summarise and analyse massive amounts of data with Pivot Tables. Quickly create reports and make it easy to update them.
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NAT KING COLE " when I fall in love "
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Myths and Mysteries of Informal Learning Infographic http://dlvr.it/9zXm4k #OtherInfographics 
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Boss Vs Leader 
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It was high school. I was 16 and I was pissed off. My English teacher assigned us a creative writing assignment: Write anything about being in high school. Anything. So I wrote a story about a school shooting. Except, in my story once the shooter was cornered by police, instead of blowing hi
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Nice View

Waterfalls are commonly formed when a river is young. At these times the channel is often narrow and deep. When the river courses over resistant bedrock, erosion happens slowly, while downstream the erosion occurs more rapidly. As the watercourse increases its velocity at the edge of the waterfall, it plucks material from the riverbed. Whirlpools created in the turbulence as well as sand and stones carried by the watercourse increase the erosion capacity. This causes the waterfall to carve deeper into the bed and to recede upstream. Often over time, the waterfall will recede back to form a canyon or gorge downstream as it recedes upstream, and it will carve deeper into the ridge above it. The rate of retreat for a waterfall can be as high as one and half meters per year.

Often, the rock stratum just below the more resistant shelf will be of a softer type, meaning that undercutting due to splashback will occur here to form a shallow cave-like formation known as a rock shelter under and behind the waterfall. Eventually, the outcropping, more resistant cap rock will collapse under pressure to add blocks of rock to the base of the waterfall. These blocks of rock are then broken down into smaller boulders by attrition as they collide with each other, and they also erode the base of the waterfall by abrasion, creating a deep plunge pool or gorge.

Streams become wider and shallower just above waterfalls due to flowing over the rock shelf, and there is usually a deep area just below the waterfall because of the kinetic energy of the water hitting the bottom. Waterfalls normally form in a rocky area due to erosion. After a long period of being fully formed, the water falling off the ledge will retreat, causing a horizontal pit parallel to the waterfall wall. Eventually, as the pit grows deeper, the waterfall collapses to be replaced by a steeply sloping stretch of river bed. In addition to gradual processes such as erosion, earth movement caused by earthquakes or landslides or volcanoes can cause a differential in land heights which interfere with the natural course of a water flow, and result in waterfalls.

A river sometimes flows over a large step in the rocks that may have been formed by a fault line. Waterfalls can occur along the edge of a glacial trough, where a stream or river flowing into a glacier continues to flow into a valley after the glacier has receded or melted. The large waterfalls in Yosemite Valley are examples of this phenomenon, which is referred to as a hanging valley. Another reason hanging valleys may form is where two rivers join and one is flowing faster than the other. Waterfalls can be grouped into ten broad classes based on the average volume of water present on the fall (which depends on both the waterfall's average flow and its height) using a logarithmic scale. Class 10 waterfalls include Niagara Falls, Paulo Afonso Falls and Khone Falls.

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#WaterfallWednesday #gif #nature #naturegifs   #photography #travel #naturephotography #travelphotography #photooftheweek #trending #trendingnow #picoftheweek #spring #spring2014 #springphotography #springphotos #springpictures #springpics #naturephotos 

Site-ul anunţul urmărit penal după ce mai 
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7 Nis 2015 - Site-ul anunţul este urmărit penal pentru proxenetism, după ce procurorii au stabilit că prin intermediul acestuia erau racolaţi "clienţi" de www.anuntul-galben.ro
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Mendeley for Android – Launching in June! http://bit.ly/1HLzyCi
It's finally happening.  This June (three short months from now) we will be launching the first version of Mendeley for Android! We've done everything we
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LOL. So true
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Have him in circles
246 people
Amjad Ashraf's profile photo
Muhammad Asif's profile photo
leklu My's profile photo
Anwar Ali's profile photo
SPHCA SINDH's profile photo
FaHad MusTafa's profile photo
Adeel Siddiqui's profile photo
jawad shah's profile photo
Ti-Ratana Organisation's profile photo
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Map of the places this user has livedMap of the places this user has livedMap of the places this user has lived
Currently
Kuala Lumpur
Previously
Pakistan - Peshawar
Work
Occupation
Dentist
Employment
  • International Medical University Malaysia
    Associate Professor, 2008 - present
  • Gandhara University Pakistan
    Assistant Professor, 2000 - 2008
Education
  • Khyber College of Dentistry
    Bachelor of Dental Surgery, 92 - 95
  • University of Malaya
    Conservative Dentistry, 98 - 2000
  • University of Peshawar
    PG Diploma in Health Planning & Managment, 2 - 2
  • Gandhara University
    Public Health, 5 - 6
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Male
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  • Snakes and Ladders
Muneer G Babar's +1's are the things they like, agree with, or want to recommend.
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This address is NOT correct, the address for Ministry for Higher Education is No. 2, Menara 2, Jalan P5/6, Presint 5, 62200 Putrajaya. I drove more than 1.5 hours to find the right place.
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