.Selection of daytrip tour Africa Natural Tours- Africa Natural Tours ( africanaturaltours.com )
Selection
of daytrip tours: Africa
Natural Tours
AFRICA NATURAL TOURS (The best
tour company in Tanzania)
Specialized
in: Mountain climbing, Wildlife safaris, Cultural tourism and Beach holidays
Contact
+255 653 679 958 OR +255 623 992 830 OR +255 692 436 113
Chemka
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In the middle of desert area
lies the beautiful mineral spring, known locally as ‘Chemka ’meaning boiling or
bubbling in Kiswahili. Located 40km from Moshi, these tranquil springs with
crystal clear, turquoise water are surrounded by huge fig trees which are often
inhabited by (mischievous) monkeys swinging from the branches.
Situated
about 35 kilometres from Moshi, in the heart of the Sanya Plains, lay the
Rundugai Springs. They are an extraordinary phenomenon, rushing up from
underground in the middle of parched and dusty landscape. Locally called Chemka,
meaning boiling, this refers to the way in which the water appears to boil as
it emerges from underground.
In fact, the water is not hot rather it is a
pleasant temperature! This is a good place to visit for a picnic and a swim
too. And the views of Kilimanjaro on a clear day are also fabulous.
Unfortunately, the water is full of fluoride which means the local people can’t
use it for drinking. The crystal-clear, turquoise waters surrounded by
palm trees and winding roots offer a picturesque spot for a relaxing afternoon
swim.
The spring is actually rather
big and over 6 meters deep in some places although you can see the bottom
through the crystal clear waters no matter where you are. You can also wrap
your arms around one of the roots and just let the water flow by as you drift
off into a daydream listening to the monkeys and birds in the treas.
The
backdrop to this secluded spring is the Blue Mountains in the southeast (where
Tanzanite is mined) and Mount Kilimanjaro in the southwest, offering spectacular
views. This is an ideal location for those looking for a place to relax, have a
swim and enjoy Tanzania’s magnificent nature. Your guide and driver will
accompany you to Chemka, where a picnic or BBQ lunch will be provided. This
excursion is perfect for a full day or afternoon out, or to set up camp for an
overnight stay.
Materuni Village
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Materuni
Village is nestled in the slopes of Mount Kilimanjaro, just 30 minutes from
Moshi. Home to the Chagga tribe, the village offers everything from
breath-taking scenery, beautiful fauna and flora and an insight into the local
culture and traditions.
This
innovative and long standing tribe produces a wealth of crops ranging from
bananas, yams and sugar to maize and beans. However, Arabica coffee is the
Chaggas primary cash crop and has been since colonial times.
Once
at Materuni village you will be given a tour of a family run Kahawa Shamba
(coffee farm), where you will learn about the intricacies of growing the
coffee, picking the beans, removing the cover, roasting and crushing and
finally tasting your very own cup of delicious coffee.
Marangu
|
For
those who don’t have the desire or the time to climb to the summit of Mt.
Kilimanjaro, a day hike will give you the opportunity to experience a small but
spectacular piece of this awe-inspiring mountain. You will follow the Marangu
route, also known as the ‘Coca Cola’ route. Starting at the Marangu gate,
1,860m above sea level, your hike begins to ascend through dense forest along a
small stream.
A
3-4 hour hike will take you to Mandara Hut, 2,700m from the base of the mountain.
From here you can enjoy a short walk to the rim of Maundi Crater (a remnant of
a volcanic vent) which offers glorious views of Moshi town on a clear day and
Kibo and Mawenzi peaks. You will have time to take in this natural wonder,
whilst having a picnic lunch before descending back to the Marangu gate
Marangu Waterfalls
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Lake Chala
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Ol Doinyo
Lengai
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Geology
Ol
Doinyo Lengai is unique among active volcanoes in that it produces natrocarbonatite
lava, a unique occurrence of volcanic carbonatite. A few older extinct carbonatite volcanoes are located
nearby, including Homa Mountain.
Lava
Whereas
most lava is rich in silicate minerals, the lava of Ol Doinyo Lengai is a carbonatite. It is rich in the rare sodium and potassium carbonates, nyerereite and gregoryite. Due to this unusual composition, the lava erupts at
relatively low temperatures of approximately 510 °C (950 °F). This
temperature is so low that the molten lava appears black in sunlight, rather
than having the red glow common to most lava. It is also much more fluid than
silicate lavas, often less viscous than water. The sodium and potassium
carbonate minerals of the lavas erupted at Ol Doinyo Lengai are unstable at the
Earth's surface and susceptible to rapid weathering, quickly turning from black to grey in colour. The
resulting volcanic landscape is different from any other in the world.
Ecology
The
carbonated ash spread over the surrounding grasslands leads to a uniquely
succulent, enriched pasture. This makes the area a vital stage on the annual wildebeest beast migration, where it becomes the nursery for the birth
of several thousand calves.
Eruptive activity
1883-1915
The
record of eruptions on the mountain dates to 1883. Flows were recorded between
1904 and 1910 and between 1913 and 1915.
1917
A
major eruption in June 1917 deposited volcanic ash up to 48 kilometres
(30 mi) away.
1926
An
eruption took place for several months in 1926.
1940
An
eruption between July and December 1940 deposited ash as far as Loliondo, 100 kilometres (62 mi) away.
1950s
Several
minor eruptions of lava were observed in 1954, 1955, and 1958.
1960s
Minor
eruptions of lava were observed in the early 1960s.
A
major eruption occurred on 14 August 1966. Geologists J. B. Dawson and G. C.
Clark visited the crater a week later and reported seeing "a thick column
of black ash" that rose for approximately three thousand feet above the
volcano and drifted away northwards towards Lake Natron. When they climbed the
cone-shaped vent, they reported seeing a continuous discharge of gas and
whitish-grey ash and dust from the centre of the pit.
2007
Volcanic
activity in the mountain caused daily earth tremors in Kenya and Tanzania from 12 July 2007 until 18 July 2007
at 8.30pm in Nairobi. The strongest tremor measured 6.0 on the Richter scale. Geologists suspected that the
sudden increase of tremors was indicative of the movement of magma through the
Ol Doinyo Lengai. The volcano erupted on 4 September 2007, sending a plume of ash and steam at least 18 kilometres (11 mi) downwind and covering
the north and west flanks in fresh lava flows.
2008
The
2007 eruption continued intermittently into 2008. At the end of February it was
reported to be gathering strength, with a major outburst taking place on 5
March. Periods of inactivity were followed by eruptions on 8 and 17 April.
Eruptive activity continued until late August 2008. A visit to the summit in
September 2008 discovered that lava emission had resumed from two vents in the
floor of the new crater. Visits to the crater in March/April 2009 showed that
this activity appeared to have ceased.
2010
In
October 2010, two separate lava flows and a small lava lake were photographed
in an over flight.
2013
The
volcano resumed natrocarbonatite lava flow which started to fill the large
crater from the 2007-2008 eruption. As of July 2013, there is a large active hornito on the western edge of the crater floor. During June,
residents near the volcano reported several earthquakes. The new crater is
inaccessible and climbers have only occasionally glimpsed into it.
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