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Battle Of Point 175
The Battle of Point 175 was a military engagement of the Western Desert Campaign that took place during Operation Crusader from 29 November – 1 December 1941, during the Second World War. Point 175 is a small rise just south of the Trigh Capuzzo, a desert track east of Sidi Rezegh and south of Zaafran, with a good view of the vicinity. In early November 1941, the feature was held by German infantry of ''Division z.b.V. Afrika'' (later named the 90th Light ''Afrika'' Division). Troops of the 2nd New Zealand Division and Infantry tanks of the 1st Army Tank Brigade attacked and captured Point 175 on 23 November, during the Battle of Sidi Rezegh, at the start of Operation Crusader. The New Zealand troops then attacked westwards and made contact with the Tobruk garrison, which had broken out to meet them. From the New Zealanders defended the point and the area to the west against Axis attempts to sever the link with the Tobruk garrison and regain control of the local roads. The n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Operation Crusader
Operation Crusader (18 November – 30 December 1941) was a military operation of the Western Desert Campaign during the Second World War by the British Eighth Army (United Kingdom), Eighth Army (with Commonwealth, Indian and Allied contingents) against the Axis forces (German and Italian) in North Africa commanded by Erwin Rommel. The operation was intended to bypass Axis defences on the Egyptian–Libyan frontier, defeat the Axis armoured forces and relieve the 1941 Siege of Tobruk. On 18 November 1941, the Eighth Army launched a surprise attack. From 18 to 22 November, the dispersal of British armoured units led to them suffering 530 tank losses and inflicted Axis losses of about 100 tanks. On 23 November, the 5th South African Brigade was destroyed at Sidi Rezegh ( ) but inflicted many German tank casualties. On 24 November Rommel ordered the "dash to the wire" and caused chaos in the British rear echelons but allowed the British armoured forces to recover. On 27 November, t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Western Desert (North Africa)
The Western Desert of Egypt is an area of the Sahara that lies west of the river Nile, up to the Libyan border, and south from the Mediterranean Sea to the border with Sudan. It is named in contrast to the Eastern Desert which extends east from the Nile to the Red Sea. The Western Desert is mostly rocky desert, though an area of sandy desert, known as the Great Sand Sea, lies to the west against the Libyan border. The desert covers an area of which is two-thirds of the land area of the country. Its highest elevation is in the Gilf Kebir plateau to the far south-west of the country, on the Egypt-Sudan-Libya border. The Western Desert is barren and uninhabited save for a chain of oases which extend in an arc from Siwa, in the north-west, to Kharga in the south. It has been the scene of conflict in modern times, particularly during the Second World War. Administratively the Western Desert is divided between various governorates; in the north and west, the Matrouh Governorate adm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Afrika Korps
The Afrika Korps or German Africa Corps (, }; DAK) was the German expeditionary force in Africa during the North African Campaign of World War II. First sent as a holding force to shore up the Italian defense of its African colonies, the formation fought on in Africa, under various appellations, from March 1941 until its surrender in May 1943. The unit's best known commander was Field Marshal Erwin Rommel. History Organization The Afrika Korps formed on 11 January 1941 and one of Hitler's favourite generals, Erwin Rommel, was designated as commander on 11 February. Originally Hans von Funck was to have commanded it, but Hitler loathed von Funck, as he had been a personal staff officer of Werner von Fritsch until von Fritsch was dismissed in 1938. The German Armed Forces High Command ('' Oberkommando der Wehrmacht'', OKW) had decided to send a "blocking force" to Italian Libya to support the Italian army. The Italian 10th Army had been routed by the British Commonwealth ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Siege Of Tobruk
The siege of Tobruk lasted for 241 days in 1941, after Axis forces advanced through Cyrenaica from El Agheila in Operation Sonnenblume against Allied forces in Libya, during the Western Desert Campaign (1940–1943) of the Second World War. In late 1940, the Allies had defeated the Italian 10th Army during Operation Compass and trapped the remnants at Beda Fomm. During early 1941, much of the Western Desert Force (WDF) was sent to the Greek and Syrian campaigns. As German troops and Italian reinforcements reached Libya, only a skeleton Allied force remained, short of equipment and supplies. The defenders quickly became known as the Rats of Tobruk. Operation ''Sonnenblume'' forced the Allies into a retreat to the Egyptian border. A garrison, consisting mostly of the 9th Australian Division (Lieutenant-General Leslie Morshead) remained at Tobruk, to deny the port to the Axis, while the WDF reorganised and prepared a counter-offensive. The Axis siege of Tobruk began on 10 Apri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wadi
Wadi ( ar, وَادِي, wādī), alternatively ''wād'' ( ar, وَاد), North African Arabic Oued, is the Arabic term traditionally referring to a valley. In some instances, it may refer to a wet (ephemeral) riverbed that contains water only when heavy rain occurs. Etymology The term ' is very widely found in Arabic toponyms. Some Spanish toponyms are derived from Andalusian Arabic where ' was used to mean a permanent river, for example: Guadalcanal from ''wādī al-qanāl'' ( ar, وَادِي الْقَنَال, "river of refreshment stalls"), Guadalajara from ''wādī al-ḥijārah'' ( ar, وَادِي الْحِجَارَة, "river of stones"), or Guadalquivir, from ''al-wādī al-kabīr'' ( ar, اَلْوَادِي الْكَبِير, "the great river"). General morphology and processes Wadis are located on gently sloping, nearly flat parts of deserts; commonly they begin on the distal portions of alluvial fans and extend to inland sabkhas or dry lakes. In basin and r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Litoranea Balbo
The Libyan Coastal Highway ( ar, الطريق الساحلي الليبي), formerly the Litoranea Balbo, is a highway that is the only major road that runs along the entire east-west length of the Libyan Mediterranean coastline. It is a section in the Cairo–Dakar Highway #1 in the Trans-African Highway system of the African Union, Arab Maghreb Union and others. Built under the rule of the Italian dictator Benito Mussolini in colonial Italian Libya in the 1930s, it was named ''Via Balbia (or ''Litoranea Balbo'') in honour of governor-general Italo Balbo, but renamed to "Libyan Coastal Highway" after independence and enlarged. In the First Libyan Civil War of 2011 the highway was a strategic and symbolic element, as the main route through the contested coastal region between Sirte and Benghazi. History Italian Libya In March 1937, Italian dictator Benito Mussolini made a state visit to Italian Libya to open this new military and civilian highway, built by governor-gen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Escarpment
An escarpment is a steep slope or long cliff that forms as a result of faulting or erosion and separates two relatively level areas having different elevations. The terms ''scarp'' and ''scarp face'' are often used interchangeably with ''escarpment''. Some sources differentiate the two terms, with ''escarpment'' referring to the margin between two landforms, and ''scarp'' referring to a cliff or a steep slope. In this usage an escarpment is a ridge which has a gentle slope on one side and a steep scarp on the other side. More loosely, the term ''scarp'' also describes a zone between a coastal lowland and a continental plateau which shows a marked, abrupt change in elevation caused by coastal erosion at the base of the plateau. Formation and description Scarps are generally formed by one of two processes: either by differential erosion of sedimentary rocks, or by movement of the Earth's crust at a geologic fault. The first process is the more common type: the escarpment is a t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Anglia
East Anglia is an area in the East of England, often defined as including the counties of Norfolk, Suffolk and Cambridgeshire. The name derives from the Anglo-Saxon kingdom of the East Angles, a people whose name originated in Anglia, in what is now Northern Germany. Area Definitions of what constitutes East Anglia vary. The Anglo-Saxon Kingdom of East Anglia, established in the 6th century, originally consisted of the modern counties of Norfolk and Suffolk and expanded west into at least part of Cambridgeshire, typically the northernmost parts known as The Fens. The modern NUTS 3 statistical unit of East Anglia comprises Norfolk, Suffolk and Cambridgeshire (including the City of Peterborough unitary authority). Those three counties have formed the Roman Catholic Diocese of East Anglia since 1976, and were the subject of a possible government devolution package in 2016. Essex has sometimes been included in definitions of East Anglia, including by the London Society o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sirocco
Sirocco ( ), scirocco, or, rarely, siroc (see below) is a Mediterranean wind that comes from the Sahara and can reach hurricane speeds in North Africa and Southern Europe, especially during the summer season. Names ''Sirocco'' derives from '' šurūq'' (), verbal noun of '' šaraqa'', related to the East, ''aš-šarq''. Various names for this wind in other languages include: * it, scirocco * scn, sciroccu * es, siroco * ca, xaloc * mt, xlokk * oc, siròc or * el, σορόκος, sorókos, or romanized: sirókos * sq, Jugu (south) * hr, jugo, lit=southern, or rarely ''širok'' * lij, sciöco or * Libyan Arabic: , romanized: , which means 'coming from the Qibla' * arz, خمسين, Ḫamsīn, which means 'fifty' ('fifty-day wind') * aeb, شلوق, šlūq, probably from with the same meaning as ; or * ary, شرقي, lit=eastern, šarquiyy, pronounced širguī Development Siroccos arise from warm, dry, tropical air masses that are pulled northward by low- ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bedouin
The Bedouin, Beduin, or Bedu (; , singular ) are nomadic Arab tribes who have historically inhabited the desert regions in the Arabian Peninsula, North Africa, the Levant, and Mesopotamia. The Bedouin originated in the Syrian Desert and Arabian Desert but spread across the rest of the Arab world in West Asia and North Africa after the spread of Islam. The English word ''bedouin'' comes from the Arabic ''badawī'', which means "desert dweller", and is traditionally contrasted with ''ḥāḍir'', the term for sedentary people. Bedouin territory stretches from the vast deserts of North Africa to the rocky sands of the Middle East. They are traditionally divided into tribes, or clans (known in Arabic as ''ʿašāʾir''; or ''qabāʾil'' ), and historically share a common culture of herding camels and goats. The vast majority of Bedouins adhere to Islam, although there are some fewer numbers of Christian Bedouins present in the Fertile Crescent. Bedouins have been referred ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erg (landform)
An erg (also sand sea or dune sea, or sand sheet if it lacks dunes) is a broad, flat area of desert covered with wind-swept sand with little or no vegetative cover. The word is derived from the Arabic word ''ʿarq'' (), meaning "dune field". Strictly speaking, an erg is defined as a desert area that contains more than of aeolian or wind-blown sand and where sand covers more than 20% of the surface. Smaller areas are known as "dune fields". The largest hot desert in the world, the Sahara, covers and contains several ergs, such as the Chech Erg and the Issaouane Erg in Algeria. Approximately 85% of all the Earth's mobile sand is found in ergs that are greater than . Ergs are also found on other celestial bodies, such as Venus, Mars, and Saturn's moon Titan. Description Ergs are concentrated in two broad belts between 20° to 40°N and 20° to 40°S latitudes, which include regions crossed by the dry, subsiding air of the trade winds. Active ergs are limited to regions ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Siwa Oasis
The Siwa Oasis ( ar, واحة سيوة, ''Wāḥat Sīwah,'' ) is an urban oasis in Egypt; between the Qattara Depression and the Great Sand Sea in the Western Desert (Egypt), Western Desert, 50 km (30 mi) east of the Libyan Egypt–Libya border, border, and 560 km (348 mi) from the capital. Its fame primarily from its ancient role as the home to an oracle of Ammon, the ruins of which are a popular tourist attraction which gave the oasis its ancient name Oasis of Amun Ra, a List of Egyptian deities#Amun, major Egyptian deity. Geography The Siwa oasis is in a deep Depression (geology), depression that reaches below sea level, to about . To the west the Jaghbub, Libya, Jaghbub oasis rests in a similar depression and to the east , the large Qattara Depression is also below sea level. Name The Ancient Egyptian name of the oasis was ''sḫt jꜣmw'', meaning "Field of Trees". The native Libyan toponym may be preserved in the Egyptian ''t̠ꜣ(j) n d̠rw “tꜣ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
