Pongwe
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Pongwe
Pongwe Pogwe is a Tanzanian village belonging to the ward of Kang'ata, Handeni District in the northern Region of Tanga. The local demonym is "Wapongwe" ("Samwepongwe" for men and "Mnamweponge" for women). Geography In Pongwe Pogwe there is a natural spring A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust (pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fres ... water place called Kwekibaya. Kwekibaya is the only source of water for thousands of people and animals. History Cultural beliefs It is believed that if a person not belonging to Wapongwe cleans the water source (the place where water is actually coming out to the surface), Kwekibaya dries out. If this happens, it is only a Wapongwe family member, in Wagongwe tradition, who can please the natural spring to give out water again. Because of the importance of Kwekibaya, there ...
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Handeni District
Handeni District is one of the 11 districts of Tanga Region in Tanzania. The District covers an area of . It is bordered to the west by the Kilindi District and the Handeni Urban District, to the north by the Korogwe District, to the east by the Pangani District, and to the south by the Pwani Region. In 2002 Kilindi District was formed out of the district. The administrative capital of the district is Mkata town. According to the 2002 Tanzania National Census, the population of the Handeni District was 248,633. According to the 2012 census, the population had increased to: 276,646. Administrative subdivisions As of 2012, Handeni District Council was administratively divided into 20 wards. Wards In pop culture The dramatic open area to the north of Handeni was the setting for Ernest Hemingway's classic hunting book, ''Green Hills of Africa ''Green Hills of Africa'' is a 1935 work of nonfiction by American writer Ernest Hemingway. Hemingway's second work of nonfiction, ''Gre ...
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Regions Of Tanzania
Tanzania is administratively divided into thirty-one regions ('' mkoa''). History * In 1975, Tanzania had 25 regions. In the 1970s, the name of the Ziwa Magharibi Region (West Lake Region) changed to Kagera Region. * In 2002, Manyara Region was created out of part of Arusha Region. * In 2012, four regions were created: Geita, Katavi, Njombe, and Simiyu. * In 2016, Songwe Region was created from the western part of Mbeya Region. List of regions Tanzania is subdivided into 31 regions (as of 2016). See also *Districts of Tanzania *List of regions of Tanzania by GDP This is a list of regions of Tanzania by GDP and GDP per capita. Data does only include values for Mainland Tansania without Zanzibar. List of regions by GDP Regions (2011 borders) by GDP in 2018 according to data by the National Bureau of Sta ... * ISO 3166-2:TZ Notes References {{Articles on first-level administrative divisions of African countries Subdivisions of Tanzania Tanzania, Regions T ...
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Tanga Region
Tanga Region (''Mkoa wa Tanga'' in Swahili) is one of Tanzania's 31 administrative regions. The region covers an area of . The region is comparable in size to the combined land area of the nation state of Burundi. The regional capital is the municipality of Tanga city. Located in northeast Tanzania, the region is bordered by Kenya and Kilimanjaro Region to the north; Manyara Region to the west; and Morogoro and Pwani Regions to the south. It has a coastline to the east with the Indian Ocean. According to the 2012 national census, the region had a population of 2,045,205. History The region was previously known as Tanga Province and included Same and Mwanga Districts that are at present in Kilimanjaro Region. Geography Geology and terrain Tanga Region is the 15th largest region by size with an area of , after Songwe Region at . An area occupying 3% of the country. In comparison Tanga is larger than the African nation of Burundi at 25,680 square kilometers. The Tanga Reg ...
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Districts Of Tanzania
As of 2021,there are 31 regions of Tanzania which are divided into 184 districts (Swahili: wilaya). In 2016, Songwe Region was created from the western part of Mbeya Region. The districts are each administered by a district council. Cities are separately administered by their own councils, and while administratively within a region, are not considered to be located within a district. The districts are listed below, by unofficial area then region: Ten most populated districts # Kinondoni Municipal Council, Dar es Salaam Region (1,775,049 inhabitants) # Temeke Municipal Council, Dar es Salaam Region (1,368,881 inhabitants) # Ilala Municipal Council, Dar es Salaam Region (1,220,611 inhabitants) # Geita District Council, Geita Region (807,619 inhabitants) # Sengerema District Council, Mwanza Region (663,034 inhabitants) # Muleba District Council, Kagera Region (540,310 inhabitants) # Kahama District Council, Shinyanga Region (523,802 inhabitants) # Nzega District Counci ...
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Wards Of Tanzania
The administrative divisions of Tanzania are controlled by Part I, Article 2.2 of the Constitution of Tanzania.Article 2.2 provides: ''For the purpose of the efficient discharge of the functions of the Government of the United Republic or of the Revolutionary Government of Zanzibar, the President may, in accordance with the procedures prescribed by law or provisions of such law as may be enacted by Parliament, divide the United Republic into regions, districts and other areas: Provided that the President shall first consult with the President of Zanzibar before dividing Tanzania Zanzibar into regions, districts or other areas.'' Tanzania is divided into thirty-one regions (''mkoa in Swahili''). Each region is subdivided into districts (''wilaya in Swahili''). The districts are sub-divided into divisions (''tarafa in Swahili'') and further into local wards (''kata in Swahili''). Wards are further subdivided for management purposes: for urban wards into streets (''mtaa in Swahil ...
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East Africa Time
East Africa Time, or EAT, is a time zone used in eastern Africa. The time zone is three hours ahead of UTC ( UTC+03:00), which is the same as Moscow Time, Arabia Standard Time, Further-eastern European Time and Eastern European Summer Time. As this time zone is predominantly in the equatorial region, there is no significant change in day length throughout the year and so daylight saving time is not observed. East Africa Time is observed by the following countries: * * * * * * * * * See also *Moscow Time, an equivalent time zone covering Belarus, Turkey and most of European Russia, also at UTC+03:00 *Arabia Standard Time, an equivalent time zone covering Bahrain, Iraq, Kuwait, Qatar, Saudi Arabia and Yemen, also at UTC+03:00 *Eastern European Summer Time, an equivalent time zone covering European and Middle Eastern countries during daylight saving, also at UTC+03:00 *Israel Summer Time, an equivalent time zone covering the State of Israel during daylight saving, also at U ...
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Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ...
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Tropical Savanna Climate
Tropical savanna climate or tropical wet and dry climate is a tropical climate sub-type that corresponds to the Köppen climate classification categories ''Aw'' (for a dry winter) and ''As'' (for a dry summer). The driest month has less than of precipitation and also less than 100-\left (\frac \right)mm of precipitation. This latter fact is in a direct contrast to a tropical monsoon climate, whose driest month sees less than of precipitation but has ''more'' than 100-\left (\frac \right) of precipitation. In essence, a tropical savanna climate tends to either see less overall rainfall than a tropical monsoon climate or have more pronounced dry season(s). In tropical savanna climates, the dry season can become severe, and often drought conditions prevail during the course of the year. Tropical savanna climates often feature tree-studded grasslands due to its dryness, rather than thick jungle. It is this widespread occurrence of tall, coarse grass (called savanna) which has led to ...
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Demonym
A demonym (; ) or gentilic () is a word that identifies a group of people (inhabitants, residents, natives) in relation to a particular place. Demonyms are usually derived from the name of the place (hamlet, village, town, city, region, province, state, country, continent, planet, and beyond). Demonyms are used to designate all people (the general population) of a particular place, regardless of ethnic, linguistic, religious or other cultural differences that may exist within the population of that place. Examples of demonyms include ''Cochabambino'', for someone from the city of Cochabamba; French for a person from France; and '' Swahili'', for a person of the Swahili coast. As a sub-field of anthroponymy, the study of demonyms is called ''demonymy'' or ''demonymics''. Since they are referring to territorially defined groups of people, demonyms are semantically different from ethnonyms (names of ethnic groups). In the English language, there are many polysemic words that hav ...
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Natural Spring
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust (pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels through ...
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