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RATES and RESERVATION: |
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in association with |
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2) OVERLAND MOBILE SAFARIS
- various options
Okavango - Savuti - Central Kalahari - Makgadikgadi
- Chobe - Zambia Vic Falls
Start and end Jo'burg
International Airport
9 or 12 Days of authentic wildlife Safari
and stunning spectacle!
To
download Power Point a presention of these Safaris click
on image. |
Pre
and Post conference
This safari consists
of a core itinerary followed or preceded by optional itineraries
| Includes: . Start and end Jo'burg International Airport . Johannesburg overnight B&B . flights to & from Johannesburg . light aircraft transfers per itinerary . upgraded tents . vehicles . park & reserve fees . camp fees . guide . all meals (except at lodges where stipulated) . Sunset Zambezi cruise and visit to Victoria Falls (where this option is selected). Go to pre-conference itineraries Go to post-conference itineraries Go to descriptions of safaris Go to Power Point Presentation |
Notes
on rates |
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We are attempting to keep costs as low as possible for Ithala 2004 delegates. The rates posted may vary, depending on currency fluctuation, flight availability and airline costs for 2004. Rather than post a higher rate to cover all eventualities we have posted the best rate we can but you will need to confirm. Please confirm the exact rate & availability at the time of booking which should be by 20% deposit as soon as possible.
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PRE-conference
Core itinerary NE-1B
- (options precede this):
9 nights of
authentic Safari and stunning sites - Semi-Participation
Inclusive of flights from and to Johannesburg airport to meet the Ithala 2004 transfer
Day 1 (July 29): Fly Johannesburg to Maun and transfer to concession area NG32 - N.E. Okavango area (Camping: Fully Inclusive - excluding drinks)
Day 2 (July 30): NG32 - activities (Camping: Fully Inclusive - excluding drinks)
Day 3 (July 31): Safari to wonderful Moremi Wildlife Reserve - set up camp (Camping: Fully Inclusive - excluding drinks)
Day 4 (August 1): Game viewing & activities in Moremi Wildlife Reserve (Camping: Fully Inclusive - excluding drinks)
Day 5 (August 2): Safari to magical Savute Grassland/Marshes (Camping: Fully Inclusive - excluding drinks)
Day 6 (August 3): Chobe Safari Lodge (Camping; Breakfast, Lunch & Dinner) - Cruise on Chobe River into famous Chobe National Park
Day 7 (August 4): Morning at Chobe Safari Lodge and then transfer across the Zambezi River to Lost Horizons Lodge (B&B) on the Zambia side Victoria Falls - (Option: Sunset cruise on the upper Zambezi)
Day 8 (August 5): Lost Horizons (B&B) - (Option: visit the Falls)
Day 9 (August 6): Breakfast at Lost Horizons, transfer to Livingstone airport and on to Johannesburg. Overnight Jo'burg - Holiday Inn Garden Court
Day 10(August 7): Transfer to Ithala 2004 (not included in cost - separate booking required)
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CORE
SAFARI - (NE-1B) - semi-participation |
Optional extension to and PRECEDING
the above Safari - NE-1B Extension
12 nights
Add 3 nights extra and get a truly mind-expanding
experience - visit the Central Kalahari Game Reserve
Day 1 (July 26): Fly Johannesburg to Maun and transfer by light aircraft to Rakops / Central Kalahari to be met by your game vehicle - set up camp (Camping: Fully Inclusive - excluding drinks)
Day 2 (July 27): Central Kalahari - drives etc. (Camping: Fully Inclusive - excluding drinks)
Day 3 (July 38): Drive to LeRoo-La-Tau / Makgadikgadi National Park (Camping: Fully Inclusive - excluding drinks)
Day 4 (July 29): Transfer drive to Maun to meet main itinerary above
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SAFARI EXTENSION
- (NE-1B Extension) - semi-participation |
POST-conference
Core itinerary NE-2A - (options follow
this):
9 nights of authentic Safari
and stunning sites - Semi-Participation
Inclusive of flights from and to Johannesburg airport to meet the Ithala 2004 transfer
Day 1 (August 13): Transfer from Ithala 2004 (not included in cost - separate booking required) Overnight in HIGC Jo'burg
Day 2 (August 14): Fly Johannesburg to Maun and then light aircraft transfer to Rakops / Central Kalahari to meet your vehicle - set up camp. (Camping: Fully Inclusive - excluding drinks)
Day 3 (August 15): Central Kalahari - drives etc. (Camping: Fully Inclusive - excluding drinks)
Day 4 (August 16): Transfer to Xwagara - Makgadikgadi National Park (Camping: Fully Inclusive - excluding drinks)
Day 5 (August 17): Road transfer Maun - Gateway to the Okavango - Mokoro-camping in the S. Delta (walks) (Camping: Fully Inclusive - excluding drinks)
Day 6 (August 18): Mokoro-camping S. Delta (walks) (Camping: Fully Inclusive - excluding drinks)
Day 7 (August 19): Mokoro back to vehicle and on to Moremi Wildlife Reserve (Kazakini)
Day 8 (August 20): Xakanaxa -Okavango/Moremi-camping
Day 9 (August 21): Xakanaxa -Okavango/Moremi-camping
Day 10 (August 22): Depart Moremi for Maun and flight to Johannesburg - in time for most evening flight departures
CORE SAFARI - (NE-2A) - semi-participation
Cost per person twin sharing: $2259 USD p. person To get today's approximate rate (This rate must be confirmed - see note at top of page)
Inclusive of:
All flights as per itinerary.
Tents, bed packs, guides, transport, camp fees, park fees, activities and meals as per itinerary.
Hotel in Johannesburg night of transfer from Ithala 2004 for flight following morning.
Excludes:
Tips, gratuities, curios, personal items, any required VISA fees, alcoholic drinks
NOTE: This package requires a minimum of 6 persons to run. Should more people, up to a maximum of 12, book this Safari it may be possible to negotiate a small reduction p.p.
NOTE: Most departures to Europe, the USA and the far East leave Johannesburg International in the evening well after the arrival of the flight from Maun. However, if you flight is earlier than 8 pm you should check this connection carefully and consider a following day departure
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Optional extension to above Safari
NE-2A Extension
12 nights
Add 3 nights extra and get
a truly mind-expanding experience - visit Chobe National Park and
Victoria Falls - Zambia side
Day 1 (Aug 22): Fly from Maun to Kasane and the Chobe Safari Lodge - gateway to the famous Chobe National Park and the Chobe River (Dinner, Bed & Breakfast)
Day 2 (Aug 23): Transfer over the mighty Zambezi River to Lost Horizons Lodge - Zambia side Victoria Falls (B&B). (Option: River cruise on the upper Zambezi).
Day 3 (Aug 24): Lost Horizons (Ootion: visit the Falls) (B&B)
Day 4 (Aug 25): Transfer to Livingstone airport for flight to Johannesburg
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SAFARI EXTENSION
- (NE-2A Extension) - semi-participation |
Outline of Safaris
Basics: We explore
the less traveled, remote game areas that give you a true feeling of the beauty
of Africa and it's wilderness. Experience the ruggedness of the African bush
with a "hands-in" (rather than a "hands-on") involvement,
become part of the environment and not just a spectator.
The Safaris are organised
on a semi-participation basis i.e. you get to pitch your own tents (normally
easy-to-erect Safari bow-type tents but for the Ithala 2004 package the tents
have been increased from 2.1 to 2.4 m and will be erected with some help) and
can help with food preparation or simply sit back and relax around an open camp
fire. The trail accommodates a maximum of only 12 people so that every one can
enjoy a very personal experience with the African bush. All safaris will be
conducted by Professional Botswana safari guides who have in-depth knowledge
of the areas of operation and a great will to share the mystery of Africa with
you. We take great pride in the service standards of the personnel working with
Bush Ways Safaris. We are completely committed to the conservation and preservation
of the African bush and work closely with the local communities of the areas
in which we operate.
Transport: All
the transport vehicles used are NEW Land Rover 130 Td5's that have been specially
designed for our trails. We also have custom-built trailers with fully stocked
built-in kitchens. Our vehicles and trailers have been developed over a number
of years to make your game viewing experience that much more comfortable and
efficient allowing you more time to take in the scenic beauty and changing ecological
environments of Africa. Not to mention the time gained that can be spent searching
for animals.
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Maun
means "the place of short reeds". Established
in 1915, this once frontier town has turned to tourism and is now the main center
of the tourist industry in Botswana. It is often referred to as the "Gateway
to the Okavango Delta". Maun was best known as being a small outpost in
the "back-of-beyond", and although this is no longer the case, it
is still home to a large mix of characters from all over Botswana, and around
the world. Maun is also the administrative center of the Ngamiland District,
and the seat of power of the BaTawana tribe. Being geared for tourism, Maun
has many restaurants, lodges, camps, curio shops, banks, a post office, and
an international airport. It therefore provides an excellent opportunity for
a brief return to civilization and some shopping, etc. during the course of
the trail.
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The Okavango Delta: "The
river that never finds the sea".
The
Okavango Delta must truly be one of Africa's most enchanted places. A swirl
of lushness in a desert of Kalahari sand, the Delta is a remarkable phenomenon.
It owes its origins to the formation of the rift valley across the course of
the Okavango River. The area was formed over the last 5 million years due to
atmospheric changes and movement of the Earth's crust.
About 5 million years ago, a relatively recent event (geologically speaking)
the southern hemisphere's atmosphere became increasingly dry due to the glaciation
of Antarctica, which absorbed most of the atmospheric moisture. 3 million years
ago, strong easterly winds caused the formation of elongated dunes that run
from east to west across the middle Kalahari. When wetter times returned these
dunes channeled the flow of the rivers in one direction, into Lake Makgadikgadi.
These wetter times also caused the great rivers of the middle Kalahari to flow,
namely the Okavango, Chobe, and Zambezi Rivers. They all traveled eastwards
with the Limpopo River into the Indian Ocean.
Then about 2 million years ago, a geological upheaval of the Earth's crust caused
the formation of a fault, which changed the flow of these great rivers. This
is known as the Kalahari-Zimbabwe axis and runs from Harare, through Bulawayo,
and ends in the eastern side of the Kalahari. This caused the rivers to flow
into and fill up the large basin that was formed, creating one of the greatest
lakes in Africa - Lake Makgadikgadi.
Eventually the lake was filled to capacity and the water had to find a way to
the ocean. Therefore, about 20 000 years ago the waters of this great lake were
forced northwards and then eastwards. This caused the middle and lower Zambezi
to connect, which resulted in the formation of Victoria Falls. With the water
now able to flow out of the lake, a partial draining of the lake occurred. A
drier climatic period followed which caused an increase in evaporation and a
decrease in the river flow. By about 10 000 years ago the drying of the Makgadikgadi
Lake was in an advanced stage. Windblown sand, as well as the Okavango River
depositing increasing amounts of sediment and debris in the lake, were gradually
filling the lake.
The formation of the Gumare fault caused a reduction in the elevation of the
land, thus causing the water of the Okavango River to spread out over a much
larger area of land and forming the now characteristic fan-shaped inland delta
of the Okavango. Today the only remains of the Ancient Lake Makgadikgadi (apart
from the Okavango Delta) are Nxai Pan, Lake Ngami, Lake Xau, the Mababe Depression,
and the two main pans of Makgadikgadi (Sua and Ntwetwe Pans).
A characteristic of the Delta is its annual flood. The Okavango River, which
rises in Angola on the Benguela Plateau, flows southeastward across the Caprivi
Strip in Namibia, tumbles through the Popa Falls rapids, and enters Botswana
at Mohembo. Bringing the result of heavy rains in Angola to Botswana (an estimated
11 billion cubic meters of water every year). The swollen river breaches its
low-water banks and begins the annual inundation of its floodplains. No two
floods are ever the same, but one can say that the permanent Delta is some 16
000 square kilometers in extent, whilst a big flood may seasonally cover as
much as 18 000 square kilometers. It can take 6 months to work its way from
Mohembo, through the labyrinth of channels and lagoons to reach Maun.
More than 95% of
the Okavango's water evaporates before it reaches the Thamalakane River near
Maun. The Thamalakane River drains the area and leads the remainder of the water
to the Boteti River, which flows through a break in the fault to Lake Xau and
eventually the Makgadikgadi Pans. This outflow of water is one of the reason's
why the water in the Delta is fresh, since it carries away the salts. The flooding
of the Okavango is not a violent process. The waters spread gently down the
channels and across the plains. The total fall in height from one end of the
delta to the other is only 62 meters, and that over a distance of some 250 kilometers!
The slow movement of water means a low sediment load and hence the incredible
clarity and purity of the Okavango's water, for which it is justly renowned.
Unique as one of the world's few inland deltas, the Okavango Delta adds enormously
to the variety of experiences open to the visitor. An obvious attraction is
the spectacular game viewing; among the best in the world and certainly situated
in the most unspoilt corner of Africa. Herds of elephants can be seen here,
as well as all the main cats, hyenas, wild dogs and many antelope, including
the rare and shy sitatunga. Not only the wildlife, but also the vegetation makes
for an interesting visit. The only vegetation types that can survive in such
a unique system are reeds and papyrus. Reeds (Phragmites australis and
P. mauritiarius) grow in the water of medium depth and are rooted. Papyrus
(Cyperus papyrus) on the other hand, floats and bends easily with the
current. Papyrus is mainly eaten by Sitatunga. Other interesting plants include:
- The underwater plants such as Bladderworts (Utricularia spp.) and Water
Chestnuts (Trapa natans), as well as; - The floating plants such as Water
Lilies (Nymphaea caerulea). A tree species common only to the perennial
swamp and not to the seasonal swamp, is the Delta Palm (Phoenix reclinata).
Other delta experiences open to the visitor are: - Take to the waters of this
magic world of islands and lagoons by dugout canoe (mokoro) and, or power boat.
- Aircrafts offer flights over the delta, which provides an excellent opportunity
to view the delta system as a whole unit. A very memorable experience!
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Makgadikgadi Pans National Park:
Makgadikgadi
Pans National Park was declared a game reserve in 1970, but in December 1992
it was enlarged and declared a national park. Today it comprises 4 900 square
kilometers. The whole reserve was once submerged beneath the ancient lake Makgadikgadi.
The valley in which the Boteti River is situated once formed the "neck"
of the original hourglass shape of the ancient lake Makgadikgadi. The Boteti
River today forms the western boundary of the Makgadikgadi Pans National Park.
About one fifth of the reserve comprises saltpans and the rest consists mainly
of rolling grassland, which yields very nutritious and desirable grasses. These
grasslands attract thousands of animals each year between October and April.
Apart from the pans area and the grassland, there is the Boteti River with its
thick sand and lush riverine vegetation. Although the Boteti only occasionally
flows to capacity, there are usually perennial pools in this river that attract
waterbuck, bushbuck and have resident hippos. These diverse habitat types (namely:
riverine woodland, scrubland, pure grassland, and saltpans) make the Makgadikgadi
Pans National Park unique.
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Central Kalhari Game Reserve:
Is the last domain of the nomadic Bushmen, whom the area was originally set
aside for to protect, so that they could preserve their way of life without
any knowledge of the encroaching modern world. However, the last of this once
nomadic race can now be found in small villages dotted throughout the reserve.
The vegetation consists mainly of Acacia woodland, Acacia scrub, Terminalia
sericea sandveld and sandveld scrub. The best season is most certainly during
the rainy season when everything is green and thousands of springbok and gemsbok
are attracted to the north, but a visit at any time of the year is most rewarding
in this incredibly beautiful reserve.
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Moremi
Wildlife Reserve: This wildlife reserve was
declared by the BaTawana people in 1963, the first wildlife sanctuary to be
created by an African tribe in their own area, and as such is unique. This act
was described at the time as a shining mark in African tribal history.
In the late 1800's a Rinderpest epidemic spread through the continent, wiping
out a large % of the wildlife and cattle in Africa. As wild animals are the
hosts of the Tsetse fly, this led to a natural decrease in the Tsetse fly population
in the area. Now it was possible for the movement of cattle into and through
the area without the fear of disease. The Batawana tribe feared that continued
competition between the returning game and the cattle herds for grazing, and
uncontrolled hunting would lead to the destruction of the habitat and a decrease
in the game populations. During this time, (late 1950's, early 1960's), the
tribe was being governed by Mrs. Moremi, the widow of Chief Moremi III, whose
son, Matiba, was too young to rule. Thus the Moremi Game Reserve was officially
proclaimed on 15 March 1963.
The
Moremi Wildlife Reserve is administered today by the Department of Wildlife
and National Parks; it is a rich and fascinating area. The Moremi Game Reserve
forms an intricate part of the Okavango Delta, comprising permanently swamped
areas, seasonally swamped areas, and dryland. Located
on the northeast side of the delta, it is probably the prime tourist destination
in Botswana, due to the fact that it encompasses several different types of
ecological zones. The total surface area of this reserve is 4 871 square kilometers.
This is almost one-third of the Okavango Delta-a fact Botswana can be very proud
of. The dryland areas of Moremi consist mainly of Mopane veld (Colophospermum
mopane). The giant mopane trees form the canopy woodland and lend an atmosphere
unique to this area. The other main vegetation types are riverine woodland,
floodplain grassland, marginal woodland on the edges of the floodplains, Terminalia
sericea sandveld, Acacia erioloba sandveld, and Hyphaene petersiana island communities.
Teeming with bird life and wildlife makes Moremi a prime wildlife area where
elephant, hippo, buffalo, lion, and most other game (including eland, kudu,
roan antelope, and if you're lucky even leopard) can be seen in abundance. Bird
life (both in the delta and dryland sections) is excellent especially along
the Khwai River. During the dry season a congregation of all species, (bird
and wildlife), along permanent rivers and water holes makes Moremi Game Reserve
one of the most unforgettable wildlife experiences in Africa!
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Chobe
National Park: Chobe National Park Chobe is
a large game reserve covering an area of 10 698 square kilometers, which makes
it the third-largest park/game reserve in Botswana. During the 1930's Botswana
was still a British protectorate known as Bechuanaland. In those days very few
people visited the Chobe riverfront, and the area was used mainly for hunting
and timber. The large elephant population lured many a hunter to the area during
the time when ivory trade was rife, and conservation of wildlife and the environment
was not a high priority. The then commissioner of Botswana, Colonel Charles
Rey, wanted to proclaim the area a reserve, however his dream was only realised
in the early 1960's when the Chobe Game Reserve came into existence under the
Bechuanaland Government proclamation no. 22 of 1961. The Chobe River forms the
northern boundary and in the extreme southwest corner it borders onto Moremi
Game Reserve. The primary function of Chobe Game Reserve is the protection of
the full range of southern Africa's large predators, as well as the localized
puku antelope and migratory elephant population, which can number up to 70 000.
The Chobe National Park offers extreme contrasts and a variety of wildlife experiences
within the confines of one park. It covers a variety of vegetation types and
geological features that vary from the almost tropical habitat of the Linyanthi
swamp to the severe, desert-like landscape of the Savuti, and from the lush
Chobe floodplain grassland to the deep sands of the Brachestegia woodland. It
also has the Mababe Depression with its black cotton soil and Acacia scrub,
as well as the pan-studded mopane and Combretum areas at Nogatsaa.
Four
main areas have been developed in Chobe (namely: Savuti, Chobe River, Linyanthi,
and Nogatsaa), each of which offers a unique experience. The Savuti and Chobe
River Front areas will be discussed, since these are the two areas of focus
during the trail.
Chobe River Front:
The Chobe National Park was named after the Chobe river, which forms
the northern boundary of the park. The Chobe River area is very rich in plant
life, offering Bachestegia sandveld, mopane woodland, mixed Combretum veld,
floodplain grassland and the riverine woodland. The latter has, unfortunately,
been severely damaged by elephants. Perhaps the greatest attraction of the Chobe
river area is the elephants, which can almost always be seen there. Their late
afternoon visits to the water's edge offer hours of fascinating viewing and
wonderful opportunities for the photographer. Along with the huge herds of elephants,
huge herds of buffalo can also be seen in this area during the dry season. You
can also expect to see tsessbe, waterbuck, roan, eland, sable, giraffe and,
if you are lucky, one of the rare puku. The floodplains of the river make an
ideal viewing area, with mixed patches of open grassland, thickets of bush and
riverine forest. In the river itself you should see hippo, and crocodile. The
Chobe river area has a rich selection of bird life as well. Exquisite sunsets
make this a wildlife experience not to be missed.
Chobe River:
The Chobe river has its origins in the highlands of Angola and flows in a south-easterly
direction. This section of the river is called the Kwando. When it enters Botswana,
it not only changes its name, but also undergoes a dramatic 90 degree change
in course at the point where it meets a major fault line. The name of the river
changes another 3 times before it reaches the Zambezi river. After entering
Botswana the Kwando river becomes the Linyanthi. At Parakurungu it becomes the
Itenge and only near Ngoma Gate does it become the Chobe river. From the point
where the Chobe abruptly bends, The Magwegqana or Selinda spillway links the
Delta to the Chobe. It is popularly believed that the Selinda can flow in both
directions, resulting in the Chobe doing the same. This is not true. In fact,
the water merely backs up for a considerable distance, creating the impression
of a change in the current.
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Savuti:
Within the Chobe National Park, Savuti is perhaps one of
the best known game-viewing areas in the country. Under ideal conditions the
number and variety of animals seen can be quite staggering. The Savuti area
supports mainly Camelthorn (Acacia erioloba) sandveld, Silver Terminalia
(Terminalia sericea) sandveld, scrub savanna, and mopane veld. Savuti's
almost desert-like landscape with a scorching sun, loose, hot sand, animals
escaping the heat by clumping together in the limited available shade, and elephants
impatiently lining up to get to the ever-dwindling water supply, offer a wildlife
experience so different, yet so true to Africa. It is almost impossible to imagine
that this desolate, harsh landscape was once submerged beneath an enormous inland
sea. Geologically the five main features of Savuti (namely the Magwikhwe Sand
Ridge, the Mababe Depression, the Savuti Marsh with its dead trees, the Rocky
Outcrops, and the Savuti Channel) are all intricately linked in the most fascinating
manner. There is still some speculation as to how this once massive lake received
its waters. The most popular explanation is that once the Upper Zambezi, the
Chobe, and the Okavango rivers flowed together, across the north of Botswana
and down to the sea via the Limpopo. A gentle warping of the Earth's crust dammed
this flow to create a vast lake. In time, however, further crustal movement
caused these rivers to find a new route to the sea. The direction of these rivers
changed by faulting; the Upper Zambezi and the Chobe turned to the northeast
and, after plunging over the Victoria Falls, joined what is now the Middle Zambezi.
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Lost
Horizons Lodge: Lost Horizons Lodge is
located on the Zambian side of the Victoria Falls, a few kilometres from the
falls. The lodge has 14 en-suite chalets, plus a well appointed central dining
area and entertainment area. The front lawn is a popular gathering area, whether
at the swimming pool, at the barbeque area or around the campfire. Each chalet
has a view over-looking the valley. The Lodge is fenced off with appropriate
electrical fencing and is positioned on a 65 hectre prestine property with no
fences to the National Park Situated on top of a hill on the edge of the Musi-o-Tunya
National Park, it commands a spectacular view of the Zambezi River above the
falls. It is surrounded by the natural bush, which is regularly frequented by
wildlife, such as elephants making their way to the Zambezi. Nights at the lodge
include bed and breakfast, but lunch and dinner are also available as a separate
charge. A host of exciting activities are on offer in and around the Victoria
Falls, any of which can be booked and arranged at the lodge.