Mountains of North

Contrary to popular belief, the height of a mountain is measured from the base to the apex. Mt. Everest stretches 8848 meters above sea level, but it has a head start due to the general uplift from the Himalayas. The Hawaiian volcano Mauna Kea is 10,314 meters from base to apex, so even though it only reaches to 4205 meters above sea level, it is a bigger mountain than Everest. (These results only apply to an incorrect manner in which one would measure a mountain. This measurement is based upon how high above sea level the mountains peak is located. The correct way to measure a mountain would be to obtain actual height from base to apex

In Nepal there are mount Everest, mt. Lotse , Mt. Makalu , Mt Annapurna,Mt Machhapuchra,Mt Kanchanga etc located . They attract many local as well as foreign tourists. Every year thousands of tourists go there to view it 's natural scenery.

Tour Sites

This Christchurch to Queenstown tour has been designed for average to experienced mountain bikers, who have less time to spare but who want a power-packed cycling adventure! You will bike through the scenic wonderland that is the South Island experiencing the diversity of sparkling lakes, steep alpine passes, sweeping pastoral landscapes, sheer sided fiords and the grandeur of breathtaking mountain views.Our route takes you along quiet roads, past beautiful lakes and across private farmland. You will travel over high Alpine passes surrounded by dense bush and high, rugged peaks, down through lush river valleys and across wide, rolling pastoral plains. Taste New Zealand’s delicious cuisine, washed down with our fine wine and finish your tour in the outdoor adventure capital of the world!

Streams

Therec are many beautifStreaming media are multimedia that are constantly received by, and normally presented to, an end-user while being delivered by a streaming provider (the term "presented" is used in this article in a general sense that includes audio or video playback). The name refers to the delivery method of the medium rather than to the medium itself. The distinction is usually applied to media that are distributed over telecommunications networks, as most other delivery systems are either inherently streaming (e.g., radio, television) or inherently non-streaming (e.g., books, video cassettes, audio CDs). The verb 'to stream' is also derived from this term, meaning to deliver media in this manner. Internet television is a commonly streamed media.ul place like eye catching . They are the wonder of world .

Leaves

In botany, a leaf is an above-ground plant organ specialized for photosynthesis. For this purpose, a leaf is typically flat (laminar) and thin. There is continued debate about whether the flatness of leaves evolved to expose the chloroplasts to more light or to increase the absorption of carbon dioxide. In either case, the adaption was made at the expense of water loss. In the Devonian period, when carbon dioxide concentration was at several times its present value, plants did not have leaves or flat stems. Many bryophytes have flat, photosynthetic organs, but these are not true leaves. Neither are the microphylls of lycophytes. The leaves of ferns, gymnosperms, and angiosperms are variously referred to as macrophyll, megaphylls, or euphylls.
Leaves are also the sites in most plants where transpiration and guttation take place. Leaves can store food and water, and are modified in some plants for other purposes. The comparable structures of ferns are correctly referred to as fronds. Furthermore, leaves are prominent in the humA structurally complete leaf of an angiosperm consists of a petiole (leaf stem), a lamina (leaf blade), and stipules (small processes located to either side of the base of the petiole). The petiole attaches to the stem at a point called the "leaf axil." Not every species produces leaves with all of the aforementioned structural components. In some species, paired stipules are not obvious or are absent altogether. A petiole may be absent, or the blade may not be laminar (flattened). The tremendous variety shown in leaf structure (anatomy) from species to species is presented in detail below under Leaf morphology. After a period of time (i.e. seasonally, during the autumn), deciduous trees shed their leaves. These leaves then decompose into the soil.an diet as leaf vegetables.

Fresh Water Falls

Significant waterfalls are listed alphabetically:
Angel Falls is the world's tallest at 979 metres (3212 feet) in Venezuela.
Bambarakanda Falls is Sri Lanka's tallest waterfall at 263 m.
Bridalveil Fall in Yosemite Valley is 189 m (620 ft) high with a sheer drop when flowing.
Cascata delle Marmore in Italy is the tallest man-made waterfall in the world.
Cautley Spout, at 175 m (580 ft), is the tallest waterfall in England.
Colonial Creek Falls, the second tallest waterfall in North America at 2,584 ft (788 m), is located in the North Cascades National Park, Washington, United States.
Dettifoss, Northeast Iceland is the largest waterfall in Europe in terms of volume discharge, having an average water flow of 200 m3/s.The falls are 100 m wide and have a drop of 44 m down to the Jökulsárgljúfur canyon.
Eas a' Chual Aluinn, at 200 m (658 ft), is the tallest waterfall in both Scotland and the United Kingdom.
Gocta is the fifth tallest in the world at 771 m (2532 ft) and located in the province Chachapoyas, Peru.
Hannoki Falls is the tallest waterfall in Asia at 1,640 ft (500 m) and located in Tateyama, Japan.
High Force on the River Tees is one of the tallest waterfalls in England.
Huangguoshu Waterfall in Anshun, Guizhou, China, is the largest waterfall in Asia.
Iguazu Falls is a tall and extremely wide waterfall located in South America on the Argentina/Brazil border.
James Bruce Falls, the tallest waterfall in North America at 840 m, is located in the Princess Louisa Marine Provincial Park, British Columbia, Canada.
Jog Falls is India's tallest (listed as 314 ranking on the World Waterfall Database), located in Karnataka state, India.
Jurong Falls in Singapore is the tallest artificial waterfall in the world.
Kaieteur Falls (Potaro River in central Guyana), located in the Kaieteur National Park, is 226 m (741 ft).
Krimmler Wasserfälle, at 380 m, is Austria's second tallest waterfall and located in Krimml, Salzburg, Austria.
Multnomah Falls is 611 feet (186 m) high and 30 ft wide.
Niagara Falls are the most powerful falls in North America.
Pissing Mare Falls, at 350 m (1148 ft), is the tallest in eastern North America.
Pistyll Rhaeadr, the tallest waterfall in Wales at 240ft (73m).
Ramnefjellsfossen is the world's third tallest at 808 m (2685 ft), at Stryn, Nesdalen, Norway.
Rhine Falls is Europe's widest and is located in Switzerland.
ShirAbad Waterfall is located in Iran, Golestan,Khanbebin, Shirabad.
St.Clair's Falls is Sri Lanka's widest waterfall 265 ft high.
Swallow Falls is one of Wales's largest waterfalls.
Takakkaw Falls is a 384 m (1260 feet) in Yoho National Park in Canada.
Tequendama Falls is a 132 m high waterfall on the Bogotá River, about 30 km southwest of Bogotá in Colombia.
Tugela Falls is the world's second tallest at 947 m (3110 ft) in KwaZulu-Natal province, Republic of South Africa.
Victoria Falls is the largest waterfall in the world and is more than a mile long. It is located on the Zambezi river on the border of Zimbabwe and Zambia.

Beautiful Falls

Streams become wider and shallower just above waterfalls due to flowing over the rock shelf, and there is usually a deep pool 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.
Waterfalls can occur along the edge of a glacial trough, whereby 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. The rivers are flowing from hanging valleysWaterfalls are grouped into ten broad classes based on the average volume of water present on the fall using a logarithmic 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, Gullfoss and Sutherland Falls (Class 8); Angel Falls and Dettifoss (Class 7); Yosemite Falls, Lower Yellowstone Falls and Umphang Thee Lor Sue Waterfall (Class

Water Falls

Typically, a river flows over a large step in the rocks that may have been formed by a fault line. As it increases its velocity at the edge of the waterfall, it plucks material from the riverbed. 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.
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 or plunge pool 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.

Baatara gorge waterfall near Tannurin, Lebanon.
Streams become wider and shallower just above waterfalls due to flowing over the rock