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Coordinates: 2°46′43″S 38°46′18″E / 2.77861°S 38.77167°E / -2.77861; 38.77167
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'''Tsavo East National Park''' is a [[national park]] in [[Kenya]] with an area of {{cvt|13747|km2}}. It was established in April 1948 and covers a semi-arid area previously known as the Taru Desert. The [[Tsavo River]] flows west to east through the national park, which is located in the [[Taita-Taveta County]] of the former [[Coast Province]].
'''Tsavo East National Park''' is a [[national park]] in [[Kenya]] with an area of {{cvt|13747|km2}}. It was established in April 1948 and covers a semi-arid area previously known as the Taru Desert. Together with the [[Tsavo West National Park]], it forms an area of about 22,000 square kilometers. The [[Tsavo River]] flows west to east through the national park, which is located in the [[Taita-Taveta County]] of the former [[Coast Province]].


==Geography==
==Geography==
{{Refimprove section|date=April 2023}}
Tsavo East National Park is generally flat, with dry plains across which the [[Galana River]] flows. Other features include the [[Yatta Plateau]] and Lugard Falls.<ref>{{Cite web|title=Tsavo East & West - Africa and Beyond|url=http://www.africaandbeyond.co.uk/africa-holidays/kenya/tsavo-east-and-west|website=www.africaandbeyond.co.uk|access-date=2020-05-24}}</ref><ref>{{Cite web|title=Tsavo National Parks|url=https://www.tsavopark.com/|website=Tsavo Park}}</ref>
Inside Tsavo East National Park, the Athi and Tsavo rivers converge to form the [[Athi-Galana-Sabaki River]]. Most of the park consists of semi-arid grasslands and [[savanna]].{{cn}}
Tsavo East National Park is generally flat, with dry plains across which the [[Galana River]] flows. Other features include the [[Yatta Plateau]] and Lugard Falls.<ref>{{Cite web|title=Tsavo National Parks|url=https://www.tsavopark.com/|website=Tsavo Park}}</ref>
Inside Tsavo East National Park, the Athi and Tsavo rivers converge to form the [[Athi-Galana-Sabaki River]]. Most of the park consists of semi-arid grasslands and [[savanna]].{{cn|date=April 2023}}<ref>{{Cite web |title=TSAVO LAND OF LEGENDS |date=10 September 2020 |url=https://africageographic.com/stories/tsavo-land-of-legends/}}</ref>


[[File:Mudanda Rock in Tsavo East National Park (edited).jpg|thumb|Viewpoint from the top of Mudanda Rock]]
[[File:Mudanda Rock in Tsavo East National Park (edited).jpg|thumb|Viewpoint from the top of Mudanda Rock]]
⚫
The Mudanda Rock is a {{cvt|1.6|km}} [[inselberg]] of stratified rock that acts as a water catchment that supplies a natural dam below. It offers an excellent vantage point for the hundreds of elephants and other wildlife that come to drink during the dry season.{{cn|date=April 2023}}
The Yatta Plateau, the world's longest [[lava flow]], runs along the western boundary of the park above the [[Athi-Galana-Sabaki River]]. Its {{cvt|290|km}} length was formed by lava from [[Ol Donyo Sabuk]] Mountain.<ref>{{cite book|last1=British Museum Natural History |title=Alkaline rocks and carbonatites of the world |date=2001|publisher=The Geological Society |location=London |isbn=9781862390836|page=135|url=https://books.google.com/books?id=K48ZMBWtoi4C&pg=PA135}}</ref>
The Yatta Plateau, the world's longest [[lava flow]], runs along the western boundary of the park above the [[Athi-Galana-Sabaki River]]. Its {{cvt|290|km}} length was formed by lava from [[Ol Donyo Sabuk]] Mountain.<ref>{{cite book|last1=British Museum Natural History |title=Alkaline rocks and carbonatites of the world |date=2001|publisher=The Geological Society |location=London |isbn=9781862390836|page=135|url=https://books.google.com/books?id=K48ZMBWtoi4C&pg=PA135}}</ref>
⚫
The Mudanda Rock is a {{cvt|1.6|km}} [[inselberg]] of stratified rock that acts as a water catchment that supplies a natural dam below. It offers an excellent vantage point for the hundreds of elephants and other wildlife that come to drink during the dry season.{{cn|date=April 2023}}
Lugard Falls, named after [[Frederick Lugard]], is a series of white water rapids on the Athi-Galana-Sabaki River.{{cn|date=April 2023}}
Lugard Falls, named after [[Frederick Lugard]], is a series of white water rapids on the Athi-Galana-Sabaki River.
Aruba Dam was built in 1952 across the [[Voi River]]. The [[reservoir (water)|reservoir]] created by the dam attracts many animals and water birds.{{cn|date=April 2023}}
Aruba Dam was built in 1952 across the [[Voi River]]. The [[reservoir (water)|reservoir]] created by the dam attracts many animals and water birds.{{cn|date=April 2023}}


[[Tsavo West National Park]] is more mountainous and wetter, with swamps, [[Lake Jipe]] and the [[Mzima Springs]]. It is known for birdlife and for its large mammals. It is also home to a black rhino sanctuary.<ref>{{Cite web|title=Wildlife Parks|url=https://spsafaritours.com/index.php?option=com_content&view=article&id=179&Itemid=510|website=spsafaritours.com|access-date=2020-05-24}}</ref>
[[Tsavo West National Park]] is more mountainous and wetter, with swamps, [[Lake Jipe]] and the [[Mzima Springs]]. It is known for birdlife and for its large mammals. It is also home to a black rhino sanctuary.{{cn|date=April 2023}}


==Archaeology and history==
==Archaeology and history==
Although a few [[Early Stone Age]] and [[Middle Stone Age]] archaeological sites are recorded from ground surface finds in Tsavo, there is much evidence for thriving [[Late Stone Age]] economy from 6,000 to 1,300 years ago. Research has shown that Late Stone Age archaeological sites are found close to the [[Galana River]] in high numbers. The inhabitants of these sites hunted wild animals, fished and kept domesticated animals. Because of the sparse availability of water away from the Galana River, human settlement in Tsavo focused on the riparian areas and in rock shelters as one moves west.<ref>Wright, David (2005) Environment, Chronology and Resource Exploitation of the Pastoral Neolithic in Tsavo, Kenya. PhD Dissertation. Department of Anthropology, University of Illinois at Chicago.</ref><ref>{{Cite journal|last=Wright|first=David K.|date=2007 |title=Tethered mobility and riparian resource exploitation among Neolithic hunters and herders in the Galana River basin, Kenyan coastal lowlands|journal=Environmental Archaeology|volume=12|issue=1|pages=25–47 |doi=10.1179/174963107x172732|s2cid=140626061}}</ref>
Although a few [[Early Stone Age]] and [[Middle Stone Age]] archaeological sites are recorded from ground surface finds in Tsavo, there is much evidence of thriving [[Late Stone Age]] economy from 6,000 to 1,300 years ago. Research has shown that Late Stone Age archaeological sites are found close to the [[Galana River]] in high numbers. The inhabitants of these sites hunted wild animals, fished, and kept domesticated animals. Because of the sparse availability of water away from the Galana River, human settlement in Tsavo focused on the riparian areas and in rock shelters as one moves west.<ref>{{Cite journal |last=Wright|first=D. K.|date=2007 |title=Tethered mobility and riparian resource exploitation among Neolithic hunters and herders in the Galana River basin, Kenyan coastal lowlands |journal=Environmental Archaeology |volume=12|issue=1|pages=25–47 |doi=10.1179/174963107x172732|s2cid=140626061}}</ref>


[[Swahili people]] traded with the inhabitants of Tsavo for ivory, catskins, and probably slaves as early as 700 AD (and probably earlier). There is no evidence for direct Swahili "colonization" of Tsavo. Instead, trade was probably accomplished by moving goods to and from the Swahili Coast via extended kin-networks. Trade goods such as cowry shells and beads have been recovered from archaeological sites dating to the early Swahili period.<ref>Wright, David (2005). New perspectives on early regional interaction networks in East Africa: A view from Tsavo National Park, Kenya. African Archaeological Review 22(3): DOI: 10.1007/s10437-005-8041-7</ref>
[[Swahili people]] traded with the inhabitants of Tsavo for ivory, catskins, and probably slaves as early as 700 AD (and probably earlier). There is no evidence for direct Swahili "colonization" of Tsavo. Instead, trade was probably accomplished by moving goods to and from the Swahili Coast via extended kin-networks. Trade goods such as cowry shells and beads have been recovered from archaeological sites dating to the early Swahili period.<ref>Wright, D. (2005). New perspectives on early regional interaction networks in East Africa: A view from Tsavo National Park, Kenya. African Archaeological Review 22(3): DOI: 10.1007/s10437-005-8041-7</ref>


{{Refimprove section|date=April 2023}}
19th century British and German explorers document people we now refer to as [[Orma people|Orma]] and Watha during their travels through the "nyika" ("bush" or "hinterland") and generally viewed them as hostile toward their interests. Beginning in the late 19th/early 20th century, the British began a concerted effort to colonise the interior of Kenya and built a railway through Tsavo in 1898. Two [[Tsavo Man-Eaters]] terrorised the construction crews led by [[John Henry Patterson (author)|John Henry Patterson]] who eventually shot the pair not before they had killed one hundred and thirty five Indians and local workers. The railway was eventually completed through to [[Kisumu]] on [[Lake Victoria]].
19th century British and German explorers document people we now refer to as [[Orma people|Orma]] and Watha during their travels through the "nyika" ("bush" or "hinterland") and generally viewed them as hostile toward their interests. Beginning in the late 19th/early 20th century, the British began a concerted effort to colonise the interior of Kenya and built a railway through Tsavo in 1898. Two [[Tsavo Man-Eaters]] terrorised the construction crews led by [[John Henry Patterson (author)|John Henry Patterson]] who eventually shot the pair but not before they had killed one hundred and thirty five Indians and local workers. The railway was eventually completed through to [[Kisumu]] on [[Lake Victoria]].


Tsavo remained the homeland for Orma pastoralists and Watha hunter-gatherers until 1948, when it was gazetted a [[national park]]. At that time, the Orma with their livestock were driven off and the aboriginal population of the Watha people was forcefully relocated to Voi and Mtito Andei as well as other locations within the nearby [[Taita Hills]]. Following Kenyan independence in 1963, hunting was banned in the park and management of Tsavo was turned over to the authority that eventually became the [[Kenya Wildlife Service]]. Tsavo currently attracts photo-tourists from all over the world interested in experiencing the vastness of the wilderness and incredible terrain.
Tsavo remained the homeland for Orma pastoralists and Watha hunter-gatherers until 1948, when it was gazetted a [[national park]]. At that time, the Orma with their livestock were driven off and the aboriginal population of the Watha people was forcefully relocated to [[Voi]] and [[Mtito Andei]] as well as other locations within the nearby [[Taita Hills]]. Following Kenyan independence in 1963, hunting was banned in the park and management of Tsavo was turned over to the authority that eventually became the [[Kenya Wildlife Service]].


== Wildlife ==
== Wildlife ==
{{Refimprove section|date=April 2023}}
It is considered one of the world's biodiversity strongholds, and its popularity is mostly due to the vast amounts of diverse wildlife that can be seen, including the famous 'big five' consisting of [[lion]], [[black rhino]], [[cape buffalo]], elephant and [[leopard]]. The park is also home to a great variety of bird life such as the [[black kite]], [[Balearica|crowned crane]], [[lovebird]] and the [[sacred ibis]].
Tsavo East National Park is considered one of the world's biodiversity strongholds, providing undeveloped homes to vast numbers of animals.


===Mammals===
===Mammals===
Tsavo East National Park is one of the world's largest protected areas, providing undeveloped homes to vast numbers of animals.{{cn}} Famous are the [[Tsavo lion]]s, a population whose adult males often lack manes entirely. In total there are about 675 lions in the Amboseli-Tsavo ecosystem.<ref name="Maclennan">Frank, L., Maclennan, S., Hazzah, L., Hill, T., & Bonham, R. (2006). ''Lion Killing in the Amboseli-Tsavo Ecosystem, 2001–2006, and its Implications for Kenya's Lion Population.'' [http://www.livingwithlions.org/AnnualReports/2006-Lion-killing-in-Amboseli-Tsavo-ecosystem.pdf PDF] Living with Lions, Nairobi, Kenya, 9.</ref>
Famous are the [[Tsavo lion]]s, a population whose adult males often lack manes entirely. As of 2006, there were about 675 lions in the Amboseli-Tsavo ecosystem.<ref name=Maclennan>{{cite report |author1=Frank, L. |author2=Maclennan, S. |author3=Hazzah, L. |author4=Hill, T. |author5=Bonham, R. |date=2006 |title=Lion Killing in the Amboseli-Tsavo Ecosystem, 2001–2006, and its Implications for Kenya's 5Lion Population|publisher=Living with Lions |place=Nairobi, Kenya |url=http://www.livingwithlions.org/AnnualReports/2006-Lion-killing-in-Amboseli-Tsavo-ecosystem.pdf}}</ref>


Some of the many mammals found in the park include:{{cn}}
Some of the many mammals found in the park include:
* [[Aardwolf]]
* [[Aardwolf]]
* [[Yellow baboon]]
* [[Yellow baboon]]

Latest revision as of 11:08, 28 September 2024

Tsavo East National Park
Map showing the location of Tsavo East National Park
Map showing the location of Tsavo East National Park
Location of Tsavo National Parks
LocationKenya
Coordinates2°46′43″S 38°46′18″E / 2.77861°S 38.77167°E / -2.77861; 38.77167
Area13,747 km2 (5,308 sq mi)
Established1948
Governing bodyKenya Wildlife Service

Tsavo East National Park is a national park in Kenya with an area of 13,747 km2 (5,308 sq mi). It was established in April 1948 and covers a semi-arid area previously known as the Taru Desert. Together with the Tsavo West National Park, it forms an area of about 22,000 square kilometers. The Tsavo River flows west to east through the national park, which is located in the Taita-Taveta County of the former Coast Province.

Geography

[edit]

Tsavo East National Park is generally flat, with dry plains across which the Galana River flows. Other features include the Yatta Plateau and Lugard Falls.[1] Inside Tsavo East National Park, the Athi and Tsavo rivers converge to form the Athi-Galana-Sabaki River. Most of the park consists of semi-arid grasslands and savanna.[citation needed][2]

Viewpoint from the top of Mudanda Rock

The Yatta Plateau, the world's longest lava flow, runs along the western boundary of the park above the Athi-Galana-Sabaki River. Its 290 km (180 mi) length was formed by lava from Ol Donyo Sabuk Mountain.[3] The Mudanda Rock is a 1.6 km (0.99 mi) inselberg of stratified rock that acts as a water catchment that supplies a natural dam below. It offers an excellent vantage point for the hundreds of elephants and other wildlife that come to drink during the dry season.[citation needed] Lugard Falls, named after Frederick Lugard, is a series of white water rapids on the Athi-Galana-Sabaki River. Aruba Dam was built in 1952 across the Voi River. The reservoir created by the dam attracts many animals and water birds.[citation needed]

Tsavo West National Park is more mountainous and wetter, with swamps, Lake Jipe and the Mzima Springs. It is known for birdlife and for its large mammals. It is also home to a black rhino sanctuary.[citation needed]

Archaeology and history

[edit]

Although a few Early Stone Age and Middle Stone Age archaeological sites are recorded from ground surface finds in Tsavo, there is much evidence of thriving Late Stone Age economy from 6,000 to 1,300 years ago. Research has shown that Late Stone Age archaeological sites are found close to the Galana River in high numbers. The inhabitants of these sites hunted wild animals, fished, and kept domesticated animals. Because of the sparse availability of water away from the Galana River, human settlement in Tsavo focused on the riparian areas and in rock shelters as one moves west.[4]

Swahili people traded with the inhabitants of Tsavo for ivory, catskins, and probably slaves as early as 700 AD (and probably earlier). There is no evidence for direct Swahili "colonization" of Tsavo. Instead, trade was probably accomplished by moving goods to and from the Swahili Coast via extended kin-networks. Trade goods such as cowry shells and beads have been recovered from archaeological sites dating to the early Swahili period.[5]

19th century British and German explorers document people we now refer to as Orma and Watha during their travels through the "nyika" ("bush" or "hinterland") and generally viewed them as hostile toward their interests. Beginning in the late 19th/early 20th century, the British began a concerted effort to colonise the interior of Kenya and built a railway through Tsavo in 1898. Two Tsavo Man-Eaters terrorised the construction crews led by John Henry Patterson who eventually shot the pair but not before they had killed one hundred and thirty five Indians and local workers. The railway was eventually completed through to Kisumu on Lake Victoria.

Tsavo remained the homeland for Orma pastoralists and Watha hunter-gatherers until 1948, when it was gazetted a national park. At that time, the Orma with their livestock were driven off and the aboriginal population of the Watha people was forcefully relocated to Voi and Mtito Andei as well as other locations within the nearby Taita Hills. Following Kenyan independence in 1963, hunting was banned in the park and management of Tsavo was turned over to the authority that eventually became the Kenya Wildlife Service.

Wildlife

[edit]

Tsavo East National Park is considered one of the world's biodiversity strongholds, providing undeveloped homes to vast numbers of animals.

Mammals

[edit]

Famous are the Tsavo lions, a population whose adult males often lack manes entirely. As of 2006, there were about 675 lions in the Amboseli-Tsavo ecosystem.[6]

Some of the many mammals found in the park include:

Birds

[edit]

Over 500 bird species have been recorded in the area, including ostriches, kestrels, buzzards, starlings, weaver birds, kingfishers, hornbills, secretary birds and herons.

Threats

[edit]

Between 2001 and 2006, more than 100 lions, elephants and other wildlife have been killed in the Amboseli-Tsavo ecosystem. Most of them have been speared by young men. The poachers usually do not face serious consequences. In contrast, the game scouts who arrested offenders have been punished by the community.[6]

References

[edit]
  1. ^ "Tsavo National Parks". Tsavo Park.
  2. ^ "TSAVO LAND OF LEGENDS". 10 September 2020.
  3. ^ British Museum Natural History (2001). Alkaline rocks and carbonatites of the world. London: The Geological Society. p. 135. ISBN 9781862390836.
  4. ^ Wright, D. K. (2007). "Tethered mobility and riparian resource exploitation among Neolithic hunters and herders in the Galana River basin, Kenyan coastal lowlands". Environmental Archaeology. 12 (1): 25–47. doi:10.1179/174963107x172732. S2CID 140626061.
  5. ^ Wright, D. (2005). New perspectives on early regional interaction networks in East Africa: A view from Tsavo National Park, Kenya. African Archaeological Review 22(3): DOI: 10.1007/s10437-005-8041-7
  6. ^ a b Frank, L.; Maclennan, S.; Hazzah, L.; Hill, T.; Bonham, R. (2006). Lion Killing in the Amboseli-Tsavo Ecosystem, 2001–2006, and its Implications for Kenya's 5Lion Population (PDF) (Report). Nairobi, Kenya: Living with Lions.
  • Kusimba, Chapurukha M.; Kusimba, Sibel B.; Wright, David K. (2005) The development and collapse of precolonial ethnic mosaics in Tsavo, Kenya. Journal of African Archaeology 3(2):345–365. JAfrArch
  • Thorbahn, P. F., (1979) The Precolonial Ivory Trade of East Africa: Reconstruction of a Human-Elephant Ecosystem. Ph.D., University of Massachusetts, Amherst.
  • Wijngaarden, W. v., and V. W. P. v. Engelen (1985) Soils and Vegetation of the Tsavo Area. Geological Survey of Kenya, Nairobi.
  • Wright, David K. (2005) Environment, Chronology and Resource Exploitation of the Pastoral Neolithic in Tsavo, Kenya. PhD Dissertation, Department of Anthropology, University of Illinois at Chicago. Wright Diss
  • Wright, David K. (2005) New perspectives on early regional interaction networks in East Africa: A view from Tsavo National Park, Kenya. African Archaeological Review 15(3):111–141. AAR
  • Wright, David K. (2007) Tethered mobility and riparian resource exploitation among Neolithic hunters and herders in the Galana River Basin, Kenyan Coastal Lowlands. Environmental Archaeology 12(1):25–47. Env. Archaeology
  • Wright, David K.; Forman, Steven L.; Kusimba, Chapurukha M.; Pierson, James; Gomez, Jeanette; Tattersfield, Peter (2007) Stratigraphic and geochronological context of human habitation along the Galana River, Kenya. Geoarchaeology 22(7):709–730. Geoarch
  • Patterson, John Henry. (1907) Man-Eaters of Tsavo. P 41 – 114.
[edit]
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