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Saturday, 10 September 2011

trees


                
A tree is a perennial woody plant. It is most often defined as a woody plant that has many secondary branches supported clear of the ground on a single main stem or trunk with clear apical dominance.[1] A minimum height specification at maturity is cited by some authors, varying from 3 m[2] to 6 m;[3] some authors set a minimum of 10 cm trunk diameter (30 cm girth).[4] Woody plants that do not meet these definitions by having multiple stems and/or small size are calledshrubs. Compared with most other plants, trees are long-lived, some reaching several thousand years old and growing to up to 115 m (379 ft) high.[5]
             









Wednesday, 7 September 2011

beautiful mountain in pakistan norten side




Flowers on the mountain at Babusar pass.

A beautiful valley of river, mountains and snow.

The beautiful view of the village name "Lawat" in State of Azad Jammu and Kashmir surrounded by thick forests all around it.

NOTE: This picture is taken by Ali Ifthikar.

Another view from the Swat Valley, Pakistan. The Area is rich in Cedar and Deodar Forests.

The chair lift at Malam jabba will take you to the height of 11,500 ft wheras the Malam Jabba resort is located at 10,500 ft from Sea Level. Although the way to reach top from Chair Lift is very easy but the Hiking has its own pleasure and i enjoyed hiking to top from here. Although not quite difficult for regular hikers but it can be the first hike of new hikers also.

The Beautiful Peak by the name of "Braak Zhan" in Raikot Glacier in Pakistan. The Lush Green meadows lying below the peak. This is the Last strong hold of western Himalayas before meeting with Karakoram Mountains. In eastern part of North Pakistan and western Kashmir the Himalaya mountains are blessed with lush green Meadows and the beautiful evergreen forests.

Beautiful meadows at Zarkhana in Lower Chitral,Pakistan.

The most Inspiring and the most lovely hill station of Pakistan. Lalazar situated behind the Kashmir Valley which is often termed as the most beautiful place on this earth.

Monday, 5 September 2011

Waterfalls

  
                                                                                 WATERFALLS
  

Formation

Formation of a waterfall


Waterfalls are commonly formed when a river is young.[1] At these times the channel is often narrow and deep. When the river courses over resistantbedrock, erosion happens slowly, while downstream the erosion occurs more rapidly.[1][2] 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.[1] 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.[3] The rate of retreat for a waterfall can be as high as one and half meters per year.[1]
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.[1] In addition to gradual processes such as erosion, earth movement caused by earthquakes or mudslides 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, whereby a stream or river flowing into aglacier 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.[1] 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 alogarithmic scale. Class 10 waterfalls include Niagara Falls, Paulo Afonso Falls and Khone Falls.
Classes of other well-known waterfalls include Victoria Falls and Kaieteur Falls (Class 9); Rhine Falls and Gullfoss (Class 8); Angel Falls and Dettifoss (Class 7); Yosemite Falls, Lower Yellowstone Falls and Umphang Thee Lor Sue Waterfall (Class 6); Sutherland Falls (Class 5).[4]

[edit]Types


Dark Hollow Falls, near Skyline Drive,Virginia, is an example of a cascade waterfall
  • Block: Water descends from a relatively wide stream or river.[2][5]
  • Cascade: Water descends a series of rock steps.[2][5]
  • Cataract: A large, powerful waterfall.[5]
  • Chute: A large quantity of water forced through a narrow, vertical passage.[5]
  • Fan: Water spreads horizontally as it descends while remaining in contact with bedrock.[5]
  • Frozen: Any waterfall which has some element of ice.[5]
  • Horsetail: Descending water maintains some contact with bedrock.[5]
  • Plunge: Water descends vertically, losing contact with the bedrock surface.[5]
  • Punchbowl: Water descends in a constricted form and then spreads out in a wider pool.[5]
  • Segmented: Distinctly separate flows of water form as it descends.[5]
  • Tiered: Water drops in a series of distinct steps or falls.[5]
  • Multi-step: A series of waterfalls one after another of roughly the same size each with its own sunken plunge pool.[5]

[edit]Examples of famous waterfalls


Havasu Falls, near Supai, Arizona, is an example of a plunge waterfall

Powerscourt Waterfall, near Enniskerry,Wicklow County, Ireland, is an example of a horsetail waterfall

Aerial view of Niagara Falls in the state of New York, US, and province of Ontario,Canada

Duruitoarea waterfall in Ceahlău,Romania


Plitvice lakes, Croatia
Significant waterfalls,[6] listed alphabetically: