March 2007                                                                                                                                                                               © Janet Davis

 

Mount Kenya Safari Club – March 7 - 8:

 

 

Once again, our group was divided into three small planes chartered by Micato to take us northeast from the Mara’s airstrip over the Great Rift Valley to Nanyuki, the airport closest to our final destination, the Mount Kenya Safari Club.  

 

 

I had come to enjoy our scenic flights over the Eastern Rift Valley with its fertile farmland, volcanic craters and ridged escarpments.  In fact, I sometimes wished I could ask the pilot to veer a little closer to a volcano or fly along a valley wall.  It was fascinating to get a bird’s eye view of one of  earth’s finest examples of plate tectonics, or continent-building.   I came home wanting to know a little more about the geological beginnings of this place we’d been.  So -- in an oversimplified African nutshell -- this is roughly how it goes.  (If you’re not interested, please skip the next six paragraphs).

 

 

Once upon a time, about 150 million years ago, Africa was not a separate continent but part of a supercontinent geologists call Gondwana which also encompassed what are now the land-masses of South America, Antarctica, India and Australia.  About 125 million years ago, Africa and South America began “rifting” apart, finally separating completely about 90 million years ago.  At the same time, India began moving northward, colliding with Eurasia roughly 50 million years ago and pushing up the Himalayas in the process.  Over the eons, New Zealand, Australia and Antarctica all separated from Gondwana in the same way.       

 

 

Of course, land-masses do not just “drift” or “rift” magically away from each other.  Their movements come as a result of boundary interactions between the the planet’s tectonic plates.  These plates make up earth’s lithosphere and are composed of the outer oceanic or continental crust and the uppermost part of the mantle.  The lithosphere ranges in thickness from a few miles to more than 200 miles under stable continental shields.  It floats on the weak, warm mantle region below, the asthenosphere, where temperatures can melt rock and magma can be released upwards from deeper in the earth.  According to Nick Culshaw, geology professor at Dalhousie University:  “The asthenosphere’s arbitrary boundary is defined by a thermal profile, say 1250° Centigrade, and is thought of as being a very, very, very slow-moving liquid, whereas the lithosphere is a buoyant solid.  So the plates are like icebergs floating in an ocean, i.e. the asthenosphere.”  (For more on the earth’s lithosphere and asthenosphere, see this page.)  

 

 

When plate boundaries meet, violent events sometimes occur, including earthquakes, volcanoes and tsunamis.  An example is the 2004 Asian tsunami caused by buckling at a subduction zone on the ocean floor during a powerful earthquake 19 miles below sea level.  The earthquake occurred when the edge of an oceanic plate slipped suddenly below a continental plate. (For more on tsunamis and earthquakes, see this page from PBS.)  The Rift Valley’s Crater Highlands in Tanzania are an excellent and scenic example of volcanism resulting from colliding plates.

 

 

Once the African continental plate finally stood alone, large parts of it anchored with stable Precambrian bedrock (like those granite outcrops or kopjes in the Serengeti), it became subject to its own tectonic forces, splitting or “rifting” along the unstable African Rift Zone into two sections, the Nubian subplate in the west, and the Somalian subplate in the east.  The crack between the two eventually widened into the 4000-mile-long Rift Valley, which begins in Turkey and extends south and east through Ethiopia, Kenya and Tanzania to Mozambique.   The East African Rift System consists of western and eastern segments.  The western is called The Albertine Rift and goes through Uganda, Rwanda and Burundi, forming large freshwater lakes, including Lake Tanganyika.  The Eastern or Gregory Rift – our safari territory -- extends from the Kenya-Ethiopia border to northern Tanzania and its crater highlands in the south.   At the top of the African Rift in Ethiopia’s Afar Triangle where three plates (Nubian, Somali and Arabian) come together, violent earthquakes are currently causing such huge crevices to form that geophysicists believe that in 10 million years, the Red Sea will flow through Africa, separating the countries on its horn, Somalia, Ethiopia, Eritrea and Dijbouti, from the “old” African continent.   Needless to say, this is exciting researchers who believe they are witnessing the birth of a new ocean.

 

 

Technically, the Rift Valley is a graben, defined by the U.S. Geological Survey as  a down-dropped block of the earth’s crust resulting from extension or pulling of the earth’s crust”.   But looks are misleading; even though this “valley” appears low and verdant beneath its high walls, much of Kenya’s Rift Valley is higher than Denver and even Vail with elevations ranging from 5890 to 9850 feet. There’s a geological explanation for this, according to Nick Culshaw:  “Not only are there grabens at the top, but the bottom lithosphere boundary traces out a huge upside-down graben.   The asthenosphere comes quite close to the surface here.  Because the asthenosphere is so close to the surface, the lithosphere heats up and, metaphorically speaking, the iceberg becomes less dense and stands high in the ocean.  The high elevations of the Rift are due to this thermal effect of rifting.” 

 

 

Therefore, Professor Culshaw concludes, plate tectonics are really responsible for the supremacy of Kenya’s fabled long-distance runners, most of whom belong to the Kalenjin tribe.  For if Kipchoge Keino hadn’t been training in Kenya’s Nandi Hills atop grabens stacked so high that the air literally thinned out above them, he might never have shocked the world in 1965 by shaving 7 seconds off the 3000-meter record and then winning two Gold and two Silver Medals in Mexico in ’68 and Munich in ’72.  And if it weren’t for plate tectonics, the world might never have heard of some of the other runners who grew up in Africa’s Rift Valley and who, like Keino, were products of the running program at St. Patrick’s School in Eldoret:  Mike Boit, Peter Rono, Wilson Kipketer, Ibrahim Hussein, and others.   So there you have it: plate tectonics and high-altitude runners!   (Read more about Kenyan runners here.  And check out a good story about Kip Keino on this site.)

 

On to the Mount Kenya Safari Club…..

 

 

After landing at the airstrip in the little town of Nanyuki which is right on the equator at Latitude 00:00, we were overjoyed to see Nathan Masambu, the Kenyan driver we’d hugged farewell at Amboseli.  “No, I’m not Nathan,” he said, “I’m his twin brother.”  We played along for the next few days, enjoying the good-natured humor of our favorite safari guide.

 

 

On arriving at the Mount Kenya Safari Club, we were served refreshing drinks and picked up our room keys.  If Micato thought we’d appreciate a luxurious finale at the end of our whirlwind safari through five game parks in two countries, they were absolutely right.  Our suite in a cottage near the bottom of the club’s grounds was lovely.  But I was keen to learn more about the various trees and plants on the property, so I booked a late afternoon walking tour with Simon Mureitha, one of the club’s naturalists.  In the meantime, we ate lunch in the club’s light-filled dining room.

 

 

Mount Kenya Safari Club has a storied history.  Currently owned by Fairmont Hotels, it was founded in 1959 by actor William Holden and two partners who bought 2000 acres around the old British hotel, the Mawingo (est. 1939), re-opening it as a private club and wildlife sanctuary.   Founding members included Conrad Hilton, Bob Hope, Clark Gable, John Wayne, Walt Disney, Joan Crawford, Lord Mountbatten and Sir Winston Churchill.   More recent members include the Aga Khan, the presidents of Gabon and Sudan, members of the Saudi royal family and Kenya’s former president, Daniel Arap Moi.  (Read this jaunty 1960 article from Time Magazine’s archives on the club’s opening).   

 

 

My nature walk with Simon around the club’s current 100-acre property took us down into the area around the Likii River.  Here we saw many plants used as herbal remedies by Kenya’s native tribes, including the silvery-grey plant nicknamed Maasai deodorant (Tarchonanthus camphoratus) and used for that purpose by them.  There was a nightshade species (Solanum incanum) whose roots are boiled by the  Kikuyu for stomach disorders.   Some plants were simply ornamental, like  the  beautiful Thomson’s kniphofia (K. thomsonii) with its aloe-like orange flowers.   On the club’s 9-hole golf course, Simon pointed out interesting trees including the African podocarpus, cassonia and hoop vine (Araucaria cunninghamicus).   Returning to the hotel,  he identified many of the exotic tropical plants used in the landscaping, including pink pandorea, golden showers vine, white beaumontea, blood-red trumpet vine, tecomaria and cuphea.  And the 10-foot-tall poinsettias on the grounds were still in bloom, including a gorgeous yellow one near the pool. 

 

 

 

Sunbirds flitted around the club’s cannas and aloes, demonstrating an interesting botanical fact:  most tropical plants with long, funnel-shaped orange and red blooms have evolved to be pollinated by birds, rather than bees or butterflies.  Bird vision tends to be most acute in the orange-red light spectra, allowing them to find such flowers easily.  In fact, while I was at the pool the next day, I stood quietly in the hot sun trying to photograph a sunbird flitting about in a tall aloe plant.  (And it occurred to me for about the fiftieth time during this trip that it would have been great to have a longer lens than my 75-300 telephoto for all those tiny birds high above me.)

 

 

Wednesday, March 7th would be our last day on safari and we had two stops on our morning game drive, the Sweetwaters Chimpanzee Sanctuary and The Rhino Sanctuary.  Both are contained in the Ol Pejeta Conservancy, a 90,000 acre wildlife reserve which was extended in 2004 to include the 24,000 acre Sweetwaters Animal Reserve and the luxurious Sweetwaters Tented Camp.  Sweetwaters was once called Ol Pejeta Ranch; it was founded by Lord Delamere of Colonial fame and went through various owners including the infamous Saudi industrialist, playboy and arms dealer Adnan Khashoggi.   The Ol Pejeta Conservancy is now owned by the conservation body, Fauna & Flora International. 

 

 

The Sweetwaters Chimpanzee Sanctuary was established in 1993 by renowned primatologist Jane Goodall, along with Lonrho Africa and the Kenya Wildlife Service.  It started with three orphaned chimpanzees who were relocated from the Jane Goodall Institute (JGI) in Burundi, when civil war broke out there.  It has grown to include many chimps since then, brought here from countries throughout East Africa and often in very bad physical condition when they arrive.   Jane Goodall’s history is fascinating.  As a young girl in England, she met the naturalist Sir David Attenborough who impressed upon her the importance of defending our fragile planet.  He also piqued her interest in the higher primates.  She was hired in England as a secretary by paleontologist Louis Leakey, ultimately travelling to Africa to work with Louis and his wife Mary on their excavations at Olduvai Gorge.  In 1960, at Leakey’s request, she went to Tanzania’s Gombe Stream National Park to study the chimpanzee population there, whetting her appetite for what would become her life’s work.  She returned to England and received her degree in ethology (animal behavior) from Cambridge in 1964, after which she returned to Africa to begin her work in earnest.  (Interestingly, the gorilla specialist Dian Fossey was also mentored by Leakey.)

 

 

Upon entering Ol Pejeta Conservancy, we completed our giraffe-spotting hat-trick when a third sub-species of the common giraffe – the beautiful reticulated giraffe (Giraffa camelopardalis reticulata) – crossed the road in front of our van.  The reticulated giraffe is also nicknamed the “crazy-paving” giraffe because its reddish coat resembles paving stones separated by white mortar.   

 

 

 

Our group gathered in an elevated structure where we could look down into the sanctuary over a tall electrified fence built to keep elephants out of the chimpanzee habitat.   We listened to guide Charles Musasia as he told us about the 41 chimpanzees now cared for on the JGI’s 247 acres at Sweetwaters, including three that were born there.  Generally, he said, breeding is not allowed and female chimps are given the Norplant contraceptive vaccine.  But ‘accidents’ have happened, including one sweet baby chimp we saw riding on the back of an adult across the river, when we took a walk through the sanctuary later.  The river serves to separate two populations of chimpanzees within the reserve.   The aim of the JGI is to rehabituate chimpanzees to life in the wild; to that end, the sanctuary is only open 1-1/2 hours in the morning and 1-1/2 hours in the afternoon so the chimps don’t become too accustomed to people.  The life expectancy of chimpanzees in the wild is 30-35 years; in a protected environment they can live 50-60 years.    In my later reading, I found that according to research being done at Germany’s renowned Max Planck Institute on chimpanzee DNA, the human and the chimpanzee genomes differ in their coding genes by only 1.2 percent, but the actual difference in gene expression between us and our primate relative is much higher, around 10 percent.   For example, where we gained the ability to speak, we have progressively lost what the chimpanzee has in spades: a refined sense of smell. 

 

 

As the day grew hot, we headed to The Rhino Sanctuary nearby.  Here, we met a  black rhinoceros named Morani (Maasai for warrior) whose life story was rather poignant.   He was born in 1974 at Amboseli National Park where, at the age of 6 months, his mother was shot by poachers.  Found wandering near her, he was rescued and taken to an orphanage in Nairobi and was eventually released back into Amboseli.  He lived there until he was a teenager when he got into a fight with another rhino and was castrated by his protagonist’s horn.   That injury left him vulnerable in the wild so he was brought to safety at Ol Pejeta where he lives on his own 100 acres doing his oh-so-relaxed best to educate the public about the black rhinoceros.   

 

 

The population of black rhinoceroses (Diceris bicornis) in Africa, once estimated to be 65,000, dropped to 10,000 in the early 80s as rhinos were shot for their horns.  Ground rhino horn is still (erroneously) considered to be an aphrodisiac, especially in China, and poachers were so well-paid for their illicit booty that by 2001 the entire African population of black rhinos was estimated at just 3,100.  Currently, the Kenyan count is about 450, of which 40 reside at Ol Pejeta.    The aim here is to manage the population, maximize its breeding potential, increase its numbers and work on conservation issues and anti-poaching legislation.   We finished our stay at the Rhino Sanctuary with a short visit to the excellent little museum at the entrance to Morani’s reserve.  

 

 

As we drove out of Ol Pejeta, we passed a group of oryxes standing at a salt lick.  Driving back towards the hotel, we saw small school children heading home for lunch and asked Nathan to stop the van so we could hand out pens and pencils.  They eagerly held up their hands to grab the goodies with big, happy smiles on their little faces.  

 

 

After lunch, some of the group elected to play golf on the 9-hole course, others to visit the animal sanctuary Holden established on the hotel grounds.  I changed into my bathing suit, grabbed my book and headed to the pool where I ordered a gin-and-tonic and retreated to a chaise lounge.  Although the sun was hot, the water in the pool was freezing but taking a swim and lounging in the sun made me feel that I’d at least had a few hours of traditional holiday down-time.  However, anyone who’s been on safari will tell you that you don’t go to Africa to relax or get a suntan:  you go to see wild animals, soak in the spectacular landscape and try to understand a little more about this amazing continent.

 

 

Our last night held some nice surprises.  After cocktails, group photos and speeches on the club’s terrace, we all loaded into our vans and headed down by the Likii river.  Here, we found a buffet table, barbecues, dining tables and a bar – all set up in a dirt-floored clearing.  We clinked our glasses to toast a fabulous safari, new friends and fantastic memories that would stay with us forever, then we filled up our plates at the buffet.  My own little surprise was a CD I’d brought along containing “golden-oldies” from the 50s and 60s -- our vintage -- and when the background music stopped and Bobby Darin came on singing ‘Dream Lover’, the party got going in earnest.  We laughed and sang and kicked up our heels on the dirt dance floor under the stars until Philip announced it was time to call it a night.

 

 

On Thursday, March 8th, we checked out, drove back to the airport at Nanyuki, hugged Nathan goodbye one more time, and flew back to Nairobi.  A shopping outing for last-minute gifts and souvenirs, a dinner at the Norfolk Hotel, and it was time to say goodbye to the friends we’d made, and to Africa.  

 

 

So, farewell for now, Africa.  But I’ll be back to discover more of your unique magic some day soon.

 

Nairobi                         Amboseli                     Tarangire                     Ngorngoro                               Serengeti                                 Maasai Mara                           

 

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