Kala Chitta Range
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Kala Chitta Range
Kala Chitta Range (in Punjabi and ur, ''Kālā Chiṭṭā'') is a mountain range in the Attock District of Punjab, Pakistan. Kala- Chitta are Punjabi words meaning Kala the Black and Chitta means the white. The range thrusts eastward across the Potohar plateau towards Rawalpindi. Pakistan's Kuldana Formation is best known for its fossil mammals, including primitive cetaceans such as Pakicetus and their close relatives. Kuldana mammals have been considered in different studies as early Luthecians (early Middle Eocene), late Ypresians (late early Eocene) or, recently, they encompass much of Ypresians up to early Lutheian time (early part of the early Eocene to early Eocene medium). Kuldana Formation The Kuldana Formation is located in the Kata Chita hills and is a thin, 20-120 m thick tongue of low-lying continental red beds that lie within a much thicker sequence of foraminifera-rich marine formations. Shallow planktonic and benthic foraminifera limit the age of the Kuld ...
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Punjab, Pakistan
Punjab (; , ) is one of the four provinces of Pakistan. Located in central-eastern region of the country, Punjab is the second-largest province of Pakistan by land area and the largest province by population. It shares land borders with the Pakistani provinces of Khyber Pakhtunkhwa to the north-west, Balochistan to the south-west and Sindh to the south, as well as Islamabad Capital Territory to the north-west and Autonomous Territory of AJK to the north. It shares an International border with the Indian states of Rajasthan and Punjab to the east and Indian-administered Kashmir to the north-east. Punjab is the most fertile province of the country as River Indus and its four major tributaries Ravi, Jhelum, Chenab and Sutlej flow through it. The province forms the bulk of the transnational Punjab region, now divided among Pakistan and India. The provincial capital is Lahore — a cultural, modern, historical, economic, and cosmopolitan centre of Pakistan. Other major cities ...
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Khyber Pakhtunkhwa
Khyber Pakhtunkhwa (; ps, خېبر پښتونخوا; Urdu, Hindko: خیبر پختونخوا) commonly abbreviated as KP or KPK, is one of the Administrative units of Pakistan, four provinces of Pakistan. Located in the Geography of Pakistan, northwestern region of the country, Khyber Pakhtunkhwa is the smallest province of Pakistan by land area and the Demographics of Pakistan, third-largest province by population after Punjab, Pakistan, Punjab and Sindh. It shares land borders with the Pakistani provinces of Balochistan, Pakistan, Balochistan to the south, Punjab, Pakistan, Punjab to the south-east and province of Gilgit-Baltistan to the north and north-east, as well as Islamabad Capital Territory to the east, Azad Jammu and Kashmir, Autonomous Territory of Azad Jammu and Kashmir to the north-east. It shares an Durand Line, international border with Afghanistan to the west. Khyber Pakhtunkhwa is known as a tourist hot spot for adventurers and explorers and has a varied landsca ...
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Attock District
Attock District (Urdu and pnb, ) is a district in Pothohar Plateau of the Punjab Province of Pakistan. Its capital is Attock city. The district was created in April 1904 by the merging of tehsils of nearby districts. Its former name was Campbellpur. Today the district consists of 6 tehsils: Attock, Fateh Jang, Hazro, Hassan Abdal, Jand and Pindi Gheb. It is located in the north of the Punjab province, bordered by Chakwal to the south, Mianwali to the southwest, Rawalpindi to the east, Kohat to the west, Nowshera to the northwest, and Swabi and Haripur to the north. History The original name of Attock District was Attock. It was changed to Campbellpur after the Commander-in-Chief of British forces Sir Colin Campbell, who rebuilt the city of Campbellpur. The name Attock was restored in 1978. Demographics According to the 2017 census of Pakistan the district had a population of 1,886,378, of which 938,650 were male and 947,597 were female. 1,395,470 (73.98%) liv ...
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Potohar Plateau
The Pothohar Plateau ( ur, ) is a plateau in north-eastern Pakistan, located between Indus River and the Jhelum River, forming the northern part of Punjab. Geography Potohar Plateau is bounded on the east by the Jhelum River, on the west by the Indus River, on the north by the Kala Chitta Range and the Margalla Hills, and on the south by the Salt Range. The southern end of the plateau is bounded by the Thal desert. The 5000 square miles of the plateau range from an average height of 1200 to 1900 feet above the sea level. Sakesar in the Salt Range is the highest mountain of the region and Tilla Jogian is the second highest. The Sivapithecus indicus fossil skull of an extinct ape species was discovered in Potohar plateau. Economy The plateau covers about 7 percent of all the cultivated land of Pakistan and most of it is very fertile, but the region does not have any proper irrigation system, with the agriculture being largely dependent on rainfall. The plateau is the location ...
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Rawalpindi
Rawalpindi ( or ; Urdu, ) is a city in the Punjab province of Pakistan. It is the fourth largest city in Pakistan after Karachi, Lahore and Faisalabad, and third largest in Punjab after Lahore and Faisalabad. Rawalpindi is next to Pakistan's capital Islamabad, and the two are jointly known as the "twin cities" because of the social and economic links between them. Rawalpindi is on the Pothohar Plateau, known for its ancient Hindu and Buddhist heritage, especially in the neighbouring town of Taxila, a UNESCO World Heritage Site. In 1765, the ruling Gakhars were defeated and the city came under Sikh rule, becoming an important city within the Sikh Empire based at Lahore. The city's ''Babu Mohallah'' neighbourhood was once home to a community of Jewish traders that had fled Mashhad, Persia, in the 1830s. The city was conquered by the British Raj in 1849, and in the late 19th century became the largest garrison town of the British Indian Army's Northern command as its climate ...
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Benthic Zone
The benthic zone is the ecological region at the lowest level of a body of water such as an ocean, lake, or stream, including the sediment surface and some sub-surface layers. The name comes from ancient Greek, βένθος (bénthos), meaning "the depths." Organisms living in this zone are called benthos and include microorganisms (e.g., bacteria and fungi) as well as larger invertebrates, such as crustaceans and polychaetes. Organisms here generally live in close relationship with the substrate and many are permanently attached to the bottom. The benthic boundary layer, which includes the bottom layer of water and the uppermost layer of sediment directly influenced by the overlying water, is an integral part of the benthic zone, as it greatly influences the biological activity that takes place there. Examples of contact soil layers include sand bottoms, rocky outcrops, coral, and bay mud. Description Oceans The benthic region of the ocean begins at the shore line (intertida ...
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Foraminifera
Foraminifera (; Latin for "hole bearers"; informally called "forams") are single-celled organisms, members of a phylum or class of amoeboid protists characterized by streaming granular Ectoplasm (cell biology), ectoplasm for catching food and other uses; and commonly an external shell (called a "Test (biology), test") of diverse forms and materials. Tests of chitin (found in some simple genera, and Textularia in particular) are believed to be the most primitive type. Most foraminifera are marine, the majority of which live on or within the seafloor sediment (i.e., are benthos, benthic), while a smaller number float in the water column at various depths (i.e., are planktonic), which belong to the suborder Globigerinina. Fewer are known from freshwater or brackish conditions, and some very few (nonaquatic) soil species have been identified through molecular analysis of small subunit ribosomal DNA. Foraminifera typically produce a test (biology), test, or shell, which can have eithe ...
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Eocene
The Eocene ( ) Epoch is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', "dawn") and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope Carbon-13, 13C in the atmosphere was exceptionally low in comparison with the more common isotope Carbon-12, 12C. The end is set at a major extinction event called the ''Grande Coupure'' (the "Great Break" in continuity) or the Eocene–Oligocene extinction event, which may be related to the impact of one or more large bolides in Popigai impact structure, Siberia and in what is now ...
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Murree Formation
Murree ( Punjabi, Urdu: مری) is a mountain resort city, located in the Galyat region of the Pir Panjal Range, within the Muree District of Punjab, Pakistan. It forms the outskirts of the Islamabad-Rawalpindi metropolitan area, and is about northeast of Islamabad. It has average altitude of . The British built this town during their rule to escape the scorching heat in the plains of Punjab during the summer. Construction of the town was started in 1851 on the hill of Murree as a sanatorium for British troops. The permanent town of Murree was constructed in 1853 and the church was consecrated shortly thereafter. One main road was established, commonly referred to even in modern times, as the mall. Murree was the summer headquarters of the colonial Punjab Government until 1876 when it was moved to Shimla. Murree became a popular tourist station for British citizens of the British Raj. Several prominent Britons were born here including Bruce Bairnsfather, Francis Younghusband, ...
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Mountain Ranges Of Khyber Pakhtunkhwa
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ...
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