Camping Safari in the Northern Circuit: Serengeti & Co.

$0 7 days from 2 participants Beginner

tour description




Ankunft Tag 1:   Kilimanjaro Airport - Arusha

Abholung am Kilimanjaro Airport und Transfer zum Hotel in Arusha.

Mahlzeiten ( - / - / -)

Safari Tag 2:   Tarangire Nationalpark

Der Tarangire Nationalpark ist Tansanias sechstgrößter Nationalpark und hat seinen Namen vom Fluss Tarangire, der durch den Park fließt. Mit seiner vielseitigen Vegetation und tausenden von Affenbrotbäumen bietet der Park eine Landschaft von atemberaubender Schönheit. Der Park ist bekannt für seinen großen Bestand an Elefanten, die in Gruppen von mehr als 100 Tieren durch ihn ziehen. Aber der Park beherbergt auch Löwen, Giraffen, Gnus, Zebras, Paviane, Antilopen, Gazellen und andere Tierarten. Für Vogelliebhaber ist der Park mit seinen mehr als 550 Arten ein wahres Paradies.

Übernachtung im Camp ( F / M / A )



Safari Tag 3 & 4: Serengeti

Der Serengeti Nationalpark ist mit seinen 30.000 km² Tansanias größter Nationalpark. Die Serengeti ist bekannt für ihre vielen Löwen und riesigen Tierwanderungen von mehr als 2 Millionen Gnus, Zebras, Gazellen und anderen Arten. In der Serengeti besteht immer eine gute Chance Löwen und andere Raubtiere beim Jagen von Gnus, Zebras und Antilopen zu beobachten.

Übernachtung im Camp ( F / M / A )



Safari Tag 5:   Ngorongoro Krater

Das Ngorongoro Naturschutzgebiet/der Ngorongoro Krater ist auf der Welterbe-Liste der UNESCO und der Krater ist der größte Einsturzkrater eines erloschenen Vulkans auf der Welt. Der Ngorongoro Krater entstand vor 2-3 Millionen Jahren, als der Vulkan explodierte und in der Folge in sich zusammenfiel. Der Krater hat eine reiche Tierwelt und es ist möglich zu beobachten, wie Massai ihre Kühe direkt neben Löwen und Nilpferden weiden.

Übernachtung im Camp ( F / M / A )



Safari Tag 6:   Lake Manyara Nationalpark

Ernest Hemingway hielt den Manyara See für den schönsten See Afrikas. Seine mehr als 400 verschiedenen Arten machen seine Tierwelt zu etwas besonderem. Man kann hier alles beobachten, von Elefanten bis zu Pavianen und tausenden von Flamingos, die den Horizont rosa färben. Wir werden uns einen netten Fleck suchen und dort unsere Lunchboxen genießen. Nachmittags geht's zurück nach Arusha.

Übernachtung im Hotel ( F / M / - )


Abreise Tag 7:   Arusha - Heim- oder Weiterreise

Nach dem Frühstück Aufbruch zum Flughafen. Entweder Sie fliegen von hier aus direkt vom Kilimanjaro International Airport nach Hause oder wir bringen Sie zum Arusha Airport für einen Direktflug nach Sansibar, wo Sie am Strand von Sansibar ein paar Tage die Seele baumeln lassen und sich erholen können. Gerne arbeiten wir ein Angebot nach Ihren Bedürfnissen aus (Beispiel siehe unten).

( F / - / - )


Optionaler Anschlussurlaub

Lodgeurlaub auf Sansibar

Kilimandscharo Besteigung

Itinerary may change without further notice due to weather-, road- or any other condition that OVERCROSS or its guides feel will jeopardize the safety of the group or material.


What benefits can you expect?

Inkludierte Leistungen:

  • privates Safari-Fahrzeug: Toyota Landcruiser mit offenem Dach
  • englischsprachiger Guide
  • alle Parkgebühren
  • Transfer vom Flughafen nach Ankunft (nicht bei Abreise)
  • 2 Übernachtung im Hotel am Ankunfts- und Abreisetag inkl. Frühstück
  • Auf Safari: Übernachtungen im 2er-Zelt mit Matratze
  • Mahlzeiten wie beschrieben + auf Safari Trinkwasser (1,5 l pro Tag und Person)

Nicht inkludierte Leistungen:

  • Flüge
  • ​Visa-Gebühren Tansania
  • Reiseversicherung (für nähere Infos klicken Sie bitte hier)
  • Einzelzelt (gegen Aufpreis zubuchbar)
  • Flughafentransfer bei Abreise (einmalig 40,- € für 5 Sitzer Transfer zum Kilimanjaro International Airport)
  • Trinkgelder für Guide (25 US-Dollar pro Tag empfohlen) und Koch (15 US-Dollar pro Tag empfohlen)
  • persönliche Ausgaben

country information

Click here for information on country Tanzania


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  • What is the climate in Tanzania?

    Tanzania is located near the equator, and temperatures are higher over the year than in Germany. In the higher parts of the country, it is consistently enjoyable, even in the Tanzanian summer. Only in June and July it can get quite chilly at night. Located on the higher sections Tour (Usambara mountains, highlands grave breach), then it can be quite cold at night, but not below freezing.

  • What is meant by desert and what kinds are there?

    Dry deserts do prevent due to their lack of water, the plant growth. At the
    Tropics at about 23, 5 degrees, there are so-called tropic deserts like the Sahara.

    The high-pressure areas there let the clouds dissolve and there is therefore no precipitate.

    These high-pressure areas are established by the intertropical convergence zone. Due to the strong sunlight warms the equatorial region particularly hard, so much water evaporates which prevents the precipitation.
    Descending air masses lead to the degradation of the clouds.
    The different types of desert we travelare: stone, gravel, salt and the sand desert.


    Stone or rock desert:

    Also known as Hammada is covered with dense nature of the blocky, angular fine rock or coarser rock material. These Hamada is the result of the physical

    Often, this rocky desert are coverde with boulders.Plateaus crossed that even with a well-developed havy duty off roaders barely passable. On our safari jeep, we usually travel on the old caravan routes, which is usually like in other forms of the desert

    Alamat acknowledges. Almat are small stone pyramids were usually placed on increases as route of the nomads and caravan leaders. Along the sandy desert, they are usually blown away, and man recognizes the old and new routes in camel carcasses, old tires and the car frame or other veralssenen those who "runs" line. A typical picture is dark colored and the smooth surface of the rocks of a desert rock, due to the smooth shiny surface it is also called desert varnish, results of flexibility accorded by the sun and the creeping permanent audit by the fine desert sand.

    Gravel desert:

    In the Western Sahara, they are called Reg, in the central Sahara, they are called Serir. Gravel deserts caused by erosion of stone or rock desert or by the
    Deposition of gravel where millions of years ago were still glacial. Another cause is a
    physical effect on the surface to collect more and more rocks, since the smaller pebbles or sand grains move down much easier. This process was developed in the desert for thousands of years, because provide moisture, wind and temperature differences for the movement of sand grains. When crossing through this gravel deserts you can still see the tracks after weeks of the knobby tires of motorcycles or the lanes of the SUVs and trucks Expeditions:

    Salt desert

    Chott el Jerid is probably the biggest and most famous salt lake Chott Tunesien.Der term is also used in Algeria and in the Eastern Sahara, the central salt desert, also known as Sebkha. Salt flats occur mostly in arid endorheic
    Sedimentary basins due to strong evaporation. In the Maghreb region of the layer is under-shaped ground conducive to formation of a dei Chotts which Duch promotes its consistency clay to seal the bottom surface. Very many of the deserts lie in the type
    Iran and Central Asia. Salt flats and salt-containing damp voallem deserts such as the Chott el Jerid, they are difficult if not impossible to impassable. Depending on the depth of the drying Sonneneinstarahlung the salt crust / upper class bedinkt passable. Often arise in wells of only a few Zentiumeter "swamp fields and ponds," weren which should in any case not drive through or walk through. The salt is formed mostly by down
    washed up debris from adjacent elevations / mountains, which often contain plenty of salt in endorheic depressions such as the Qattara Depression accumulates naturally as salt-enriched clay and Lehmflächen. This surface is called Salt Flat and Alkali Flats. After precipitation, which are mostly in the winter months, walked these salt lakes.


    The sandy deserts:

    The erg in the Western Sahara and in the Libyan Sahara is a desert is called the surface mainly consists of quartz sand. This is caused by soil erosion, sand a gravel desert. Due to the absolute dry conditions in the sandy deserts due to the lack of vegitation are much harder than stone or gravel deserts. Because of the fine grading of the sand deserts in the lower part of the carrying capacity is solidified, the surface is rather finely and due to the strong sunlight and fine dust-like sand of Einwehung less viable.
    In the northern Sahara dunes are found frequently occurring as longitudinal dunes or sickle.
    In libischen part of the Sahara will find the most beautiful crescent dunes below Seba and the longest sand dunes in Algeria with up to six hundred miles long.

    With the motorcycle and 4x4 suv in the solidified dunes levels passable, but difficult or impossible in up to three hundred feet high Mamutdünen how she finds in Algeria and Libya.

    The world's largest sand desert in Arabia, where we conduct the tours in Oman and the Rub al Khali Dubai. الربع الخالي ar-Rub ʿ al-Khali is the paradise for every off roader. The turning circle running through the desert of Oman, Yemen, and UAE.



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There are no fix dates for this tour. We are happy to set up dates to your liking.