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Duncan Murrell - A Whale of a Time

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Duncan Murrell - A Whale of a Time

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  • My friend standing under a stagnating glacier at Wolf Point, Glacier Bay National Park and Preserve, Southeast Alaska, USA.<br />
<br />
My friend and I came across this “stagnating” glacier in Glacier Bay and because it was stagnating there were ice caves that had opened up beneath it. A stagnating glacier is a glacier that is neither advancing nor retreating, but melting in situ, in totality. It was amazing being able to walk beneath a glacier although somewhat precarions because stones were being dropped from the ice as it melted. The colour of the ice with the light shining through it from above was extraordinary; it was definitely one of the most “other-wordly” places that I have ever been to. If you looked closely into the ice you could see and hear all of the tiny capillaries of melt water that were gradually draining the life from the glacier. I wondered how long it had been “alive” for?<br />
Geologists believe that Glacier Bay existed during a minimum of four glacial periods ending with the Little Ice Age, which has a 4,000 years old record, as the latest period. All glaciers in the park today are said to be remnants of this glacial period.
    ice.tif
  • The McBride tidewater Glacier, Glacier Bay national Park and Preserve, Southeast Alaska, USA.<br />
<br />
The Glacier Bay Basin is a myriad combination of tidewater glaciers, snow-capped mountain ranges, ocean coastlines, deep fjords, and freshwater rivers and lakes that provide widely varying land and seascapes, and hosts a mosaic of plant communities, and a great variety of marine and terrestrial wildlife. It has many branches, inlets, lagoons, islands, and channels that hold prospects for scientific exploration and a visual treat for the visitor.<br />
Glacier Bay, the body of water, covers an area 1.375 square miles (3,560 km2) of glaciers and accounts for 27% of the park area. It was a large single glacier of solid ice until early 18th century. It started retreating and evolved over the centuries into the largest protected water area park in the world. It was formerly known as the Grand Pacific Glacier about 4,000 feet (1200 m) thick and about 20 miles (32 km) in width, which has since then, over the last more than 200 years retreated by 65 miles (105 kms) to the head of the bay at Tarr Inlet, and in this process left separate 20 other glaciers, including this one, in its trail.<br />
Glaciers are very dynamic entities and there are seven “active” tidewater glaciers in Glacier bay, which are advancing into the sea and thus calve off large chunks of ice that fall into the sea with a thunderous noise, raising large waves.
    ice-5.tif
  • My friend and I came across this “stagnating” glacier in Glacier Bay and because it was stagnating there were ice caves that had opened up beneath it. A stagnating glacier is a glacier that is neither advancing nor retreating, but melting in situ, in totality. It was amazing being able to walk beneath a glacier although somewhat precarions because stones were being dropped from the ice as it melted. The colour of the ice with the light shining through it from above was extraordinary; it was definitely one of the most “other-wordly” places that I have ever been to. If you looked closely into the ice you could see and hear all of the tiny capillaries of melt water that were gradually draining the life from the glacier. I wondered how long it had been “alive” for?<br />
Geologists believe that Glacier Bay existed during a minimum of four glacial periods ending with the Little Ice Age, which has a 4,000 years old record, as the latest period. All glaciers in the park today are said to be remnants of this glacial period.
    Southeast-Alaska-glaciation11.jpg
  • My friend and I came across this “stagnating” glacier in Glacier Bay and because it was stagnating there were ice caves that had opened up beneath it. A stagnating glacier is a glacier that is neither advancing nor retreating, but melting in situ, in totality. It was amazing being able to walk beneath a glacier although somewhat precarions because stones were being dropped from the ice as it melted. The colour of the ice with the light shining through it from above was extraordinary; it was definitely one of the most “other-wordly” places that I have ever been to. If you looked closely into the ice you could see and hear all of the tiny capillaries of melt water that were gradually draining the life from the glacier. I wondered how long it had been “alive” for?<br />
Geologists believe that Glacier Bay existed during a minimum of four glacial periods ending with the Little Ice Age, which has a 4,000 years old record, as the latest period. All glaciers in the park today are said to be remnants of this glacial period.
    Southeast-Alaska-glaciation9.jpg
  • My friend and I came across this “stagnating” glacier in Glacier Bay and because it was stagnating there were ice caves that had opened up beneath it. A stagnating glacier is a glacier that is neither advancing nor retreating, but melting in situ, in totality. It was amazing being able to walk beneath a glacier although somewhat precarions because stones were being dropped from the ice as it melted. The colour of the ice with the light shining through it from above was extraordinary; it was definitely one of the most “other-wordly” places that I have ever been to. If you looked closely into the ice you could see and hear all of the tiny capillaries of melt water that were gradually draining the life from the glacier. I wondered how long it had been “alive” for?Geologists believe that Glacier Bay existed during a minimum of four glacial periods ending with the Little Ice Age, which has a 4,000 years old record, as the latest period. All glaciers in the park today are said to be remnants of this glacial period.
    Alaska-ice5.jpg
  • My friend and I came across this “stagnating” glacier in Glacier Bay and because it was stagnating there were ice caves that had opened up beneath it. A stagnating glacier is a glacier that is neither advancing nor retreating, but melting in situ, in totality. It was amazing being able to walk beneath a glacier although somewhat precarions because stones were being dropped from the ice as it melted. The colour of the ice with the light shining through it from above was extraordinary; it was definitely one of the most “other-wordly” places that I have ever been to. If you looked closely into the ice you could see and hear all of the tiny capillaries of melt water that were gradually draining the life from the glacier. I wondered how long it had been “alive” for?<br />
Geologists believe that Glacier Bay existed during a minimum of four glacial periods ending with the Little Ice Age, which has a 4,000 years old record, as the latest period. All glaciers in the park today are said to be remnants of this glacial period.
    Southeast-Alaska-glaciation8.jpg
  • The harbor seal (Phoca vitulina), a widespread species in both the north Atlantic and Pacific oceans, is found in Alaska along the coast extending from Dixon Entrance north to Kuskokwim Bay and west throughout the Aleutian Islands. Harbor seals, and other phocid (true) seals, also are called “hair” seals, which helps distinguish true seals from fur seals. Harbor seals haul out of the water periodically to rest, give birth, and nurse their pups. In winter seals spend up to 80% of their time in the water. In spring and summer they spend more time hauled out during pupping and moult season. Reefs, sand and gravel beaches, sand and mud bars, and glacial, pan ice, and sea ice are commonly used for haul-out sites. The moulting lines on these seals are clearly visible.
    Alaska-harbour-seal1.jpg
  • Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.
    Southeast-Alaska-glaciation17.jpg
  • Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.
    Southeast-Alaska-glaciation12.jpg
  • Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.
    Southeast-Alaska-glaciation18.jpg
  • Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.
    Southeast-Alaska-glaciation15.jpg
  • Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.
    Southeast-Alaska-glaciation16.jpg
  • Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.
    Southeast-Alaska-glaciation19.jpg
  • The Glacier Bay Basin is a myriad combination of tidewater glaciers, snow-capped mountain ranges, ocean coastlines, deep fjords, and freshwater rivers and lakes that provide widely varying land and seascapes, and hosts a mosaic of plant communities, and a great variety of marine and terrestrial wildlife. It has many branches, inlets, lagoons, islands, and channels that hold prospects for scientific exploration and a visual treat for the visitor.<br />
Glacier Bay, the body of water, covers an area 1.375 square miles (3,560 km2) of glaciers and accounts for 27% of the park area. It was a large single glacier of solid ice until early 18th century. It started retreating and evolved over the centuries into the largest protected water area park in the world. It was formerly known as the Grand Pacific Glacier about 4,000 feet (1200 m) thick and about 20 miles (32 km) in width, which has since then, over the last more than 200 years retreated by 65 miles (105 kms) to the head of the bay at Tarr Inlet, and in this process left separate 20 other glaciers, including this one, in its trail.<br />
Glaciers are very dynamic entities and there are seven “active” tidewater glaciers in Glacier bay, which are advancing into the sea and thus calve off large chunks of ice that fall into the sea with a thunderous noise, raising large waves.
    Southeast-Alaska-glaciation1.jpg
  • Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.
    Southeast-Alaska-glaciation14.jpg
  • Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.
    Southeast-Alaska-glaciation13.jpg
  • Anthropomorphic iceberg, LeConte Inlet, Southeast Alaska, USA<br />
.<br />
Ice calving off from the tidewater glaciers of Southeast Alaska can assume just about any shape or form, that gradually metamorphoses as they melt. This was one of the most anthropomorphic icebergs that I ever came across washed up on the shore of the Le Conte inlet where the Le Conte Glacier is situated, the southernmost tidewater glacier in North America.
    Alaska-glaciation20.tif
  • Ice calving off from the tidewater glaciers of Southeast Alaska can assume just about any shape or form, that gradually metamorphoses as they melt. This was one of the most anthropomorphic icebergs that I ever came across washed up on the shore of the Le Conte inlet where the Le Conte Glacier is situated, the southernmost tidewater glacier in North America.
    Southeast-Alaska-glaciation20.jpg
  • The LeConte Inlet and Glacier were only a day's paddle from Petersburg so it was a good day out for me whenever I was living in the town. The glacier is the southernmost tide-water glacier in the Northern Hemisphere. I always enjoyed the challenge of trying to navigate my way through the congested ice floes, and then trying to photograph the seals without disturbing them, which most of the time I was able to do because of the stealth that a kayak provides. Being in a kayak also enabled me to get very close and low to icebergs so that I could take close-ups of the amazing icebergs sculpted into infinite shapes and forms, and luminescent with ethereal shades of blue and green. I always used the Indian method of anchoring with a rock tied to an anchor line resting on the bow, and then an additional longer bow line with the last half metre wrapped around the rock, so that when I pushed the kayak out and yanked on the long bow line the rock and anchor line were dislodged and fell into the water.
    Alaska-camping-kayaking8.jpg
  • Meltwater stream emerging from the base of a tidewater glacier in Glacier Bay National Park and Preserve at low tide, Southeast Alaska, USA.
    ice-4.tif
  • Large fluted iceberg in Le Conte Inlet, Southeast Alaska, USA.<br />
<br />
I think that this was the only time that I ever saw a glacier that had melted like this, into very symmetrical fluted ridges. I haven’t found an explanation for this peculiar phenomenon.
    ice-3.tif
  • Ancient “blue” iceberg, Le Conte Inlet, Southeast Alaska, USA.
    ice-2.tif
  • Southeast-Alaska-winter9.jpg
  • Harbor seals show variable movement patterns depending on their sex and age class, with some exhibiting considerable localized travel but noseasonalpatterns,whileothersshowmoreextendedmovements,particularlyduringthewinter. Seasonaluseofglacialfjords,wheremanyfemalesaggregateto give birth on icebergs in the summer, is common. Satellite tagging studies have shown that pups may range up to 232 miles (374 km) from their birth site, although most movements are less than 62 miles (100km) away. Juvenile seals can make more extensive movements of up to 186-310 miles (300-500 km) away from their tagging location; however, most remain within 100km. Adult seals typically make shorter movements and on average are within 37 miles (60km) of their tagging site. More recent tagging of seals that occupy glacial fiords has revealed movements of seals from one glacial fiord to another as well as one extensive movement of a juvenile female seal from Glacier Bay in southeastern Alaska to Prince William Sound, an estimated straight-line distance of ~ 520 miles (830 km). As more seals are being satellite-tagged, much more information is becoming available about winter and summer movements.
    Alaska-harbour-seal2.jpg
  • Palawan-people7.tif
  • Southeast-Alaska-winter7.jpg
  • Southeast-Alaska-glaciation2.jpg
  • Southeast-Alaska-glaciation6.jpg
  • I took this photo near my first real private accommodation in Petersburg. I had gone from living in the forest next to the beach in a shelter made from skunk cabbage leaves, to a polythene shelter in the forest, to a dilapidated old house, then to the cannery bunkhouse, and then to an apartment in the old Petersburg Pilot Newspaper building on Sing Lee Alley. I shared a darkroom in the old building with another local photographer. From there I moved onto the sailboat Avalon.
    Southeast-Alaska-winter3.jpg
  • Southeast-Alaska-winter10.jpg
  • Southeast-Alaska-glaciation4.jpg
  • I think that this was the only time that I ever saw a glacier that had melted like this into very symmetrical fluted ridges. I haven’t found an explanation for this peculiar phenomenon.
    Southeast-Alaska-glaciation7.jpg
  • Southeast-Alaska-glaciation3.jpg
  • Southeast-Alaska-glaciation5.jpg
  • When I was camping on one of the Los Candeleros islets, I was sharing it with three ravens. They were rolling and tumbling acrobatically in the updraughts that were whipping up the precipitous face of the island. I have developed a special affinity with that most ubiquitous, intelligent and successful of all birds over many years in Alaska, where their amazing repertoire of calls is an integral feature of the ancient forests. I have even learnt how to mimic some of their calls and capture their attention. After a few days cutting the ice with my fellow residents one of them started flying out to my kayak to seemingly greet me whenever I returned to the island; it would circle overhead whilst calling out and then escort me back to shore.<br />
After a couple of weeks of familiarisation my glossy black friend vanished. A few days later I landed on a nearby beach at Ensenada Blanca to visit an American living in the local fishing village. As I stepped ashore I noticed a raven flying demonstrably towards me. I replied to its raven calls and it flew overhead and did a few rolls as if it was showing off. The acknowledgement was plain to see, rather like a dog wagging its tail. Then it flew ahead of me and proceeded to harass and dislodge the turkey vultures that were perched in the trees. After each successful assault it called out and then proceeded to dislodge another vulture in the next tree; within seconds the sky was full of screeching, disgruntled vultures! It seemed as if the raven was clearly intoxicated with its own sense of bravado, and maybe it was even trying to impress me. When I arrived at the American’s house at the end of the beach I told him about the hilarious encounter with my shiny black friend and when he looked out of the doorway to see if the raven was still out there he looked at me, laughed, and informed me that it was waiting outside for me, and sure enough it was perched on a cactus just a few metres from the door!
    Kayaking- Gulf-of-California61.jpg
  • The Johns Hopkins Inlet is probably the most spectacular glacial inlet in Glacier Bay, but it was usually so heavily choked with ice that it was virtually impossible to get anywhere near the face of the huge glacier.
    Southeast-Alaska-Avalon22.jpg
  • The total Alaska harbor seal population is estimated at approximately 141,000 in non-glacial sites and approximately 15,000 in glacial fjords. Harbor seals are difficult to census because they can only be accurately counted when they are hauled out. They haul out at different times of the day at thousands of locations in Alaska; both at terrestrial sites and on glacial ice calved from tidewater glaciers. During any survey, some seals are in the water and not available to be counted while others are hauled out, but the proportion of the total population hauled out at any given time is unknown and must be estimated. One way to arrive at this estimate is to radio tag seals in the area, prior to conducting a survey. When the survey is conducted, the proportion of radio-tagged seals that are not hauled out provides a correction factor to estimate the total seal population (e.g., if 3 of 10 tagged seals were not hauled out, an additional 30% would be added to the count of seals hauled out to estimate the total population).
    Alaska-harbour-seal6.jpg
  • I can never forget the amazing lighting on this morning when I was heading out of Tenakee Inlet with some guests aboard my boat "Selena" to take them to see humpback whales bubble net feeding at Point Hayes to the south down Chatham Strait. It was my birthday and I had a very unique and unexpected birthday present. We were motoring down Chatham Strait when I spotted an unusual shape bobbing on the surface: almost like the shape of ice cream sitting in a cone. When I looked through my binoculars I could hardly believe my eyes because I instantly recognised it as being a big bull northern elephant seal (Mirounga angustirostris) on the surface with its unmistakeable big proboscis drooping from its head. I had no idea that they ventured that far north, and after consulting with some local fisherman I was informed that it was indeed a very rare occurrence.
    Alaska-coast12.jpg
  • In Alaska, single pups are born between May and mid-July. Young pups are able to swim almost immediately after birth. They normally remain with their mothers about one month, after which they are weaned and separate from their mother. At that time over half their body weight may consist of fat, providing them a head start on self-sufficiency.While harbor seals will often voluntarily swim close to humans on beaches or in small boats, seals resting on land or ice are wary of people and will rush into the water if approached too closely. If disturbed too often, seals have been known to abandon favorite haul-out sites or their pups. I was able to approach this sleeping seal pup close enough to touch it. They are usually much more alert than sea lions because there is less distracting noise and commotion. I have always been extremely careful not to disturb any of the animals that I have stalked.
    Alaska-harbour-seal3.jpg
  • Bull moose (Alces alces andersoni), Adam’s Inlet, Glacier Bay National Park and Preserve, Southeast Alaska, USA.<br />
<br />
They originated in Asia and crossed into North America shortly before the Bering Land Bridge between Asia and America flooded about 11,000 years ago, and then dispersed throughout Beringia ( prehistoric Interior Alaska and northwest Canada). About 10,000 years ago an ice-free corridor opened up between the huge continental glaciers that covered Canada, allowing animals like moose, grizzly bears and bison to move south from Berangia to the Pacific Northwest into the continental United States.<br />
Moose subsequently evolved into four North American subspecies (and other sub-species found in Scandinavia and Russia). Alaska is home to the world’s largest, Alces alces gigas, as well as a smaller sub-species, Alces alces andersoni. Gigas, also known as Alaska moose or tundra moose, is found in Alaska, the Yukon and northwest British Columbia; andersoni, or anderson’s moose, is found in Southeast Alaska, the eastern Yukon, and central B.C east to Michigan.<br />
Impeded by mountain ranges, icefields and glaciers, moose did not colonize Southeast Alaska until the 20th century. They are far more recent arrivals than Sitka black-tailed deer and wolves, which moved up the coast from the south about 8,000 years ago as the glaciers melted and land was exposed. Moose from British Columbia accressed Southeast via the river corridors and arrived in the Taku River valley south of Juneau and the Stikine River basin near Petersburg about 1910.<br />
I had a memorable encounter with a large herd of moose in Adam’s Inlet in Glacier Bay in the middle of winter. I was standing on the mudflats at low tide and set up my tripod to photograph the moose on the shore. Gradually they started to walk towards me until eventually I was surrounded by at least 20 moose who were more curious about me than afraid; apparently their protected status in the National Park had made them not fear humans.
    wildlife-12.tif
  • They originated in Asia and crossed into North America shortly before the Bering Land Bridge between Asia and America flooded about 11,000 years ago, and then dispersed throughout Beringia ( prehistoric Interior Alaska and northwest Canada). About 10,000 years ago an ice-free corridor opened up between the huge continental glaciers that covered Canada, allowing animals like moose, grizzly bears and bison to move south from Berangia to the Pacific Northwest into the continental United States.<br />
Moose subsequently evolved into four North American subspecies (and other sub-species found in Scandinavia and Russia). Alaska is home to the world’s largest, Alces alces gigas, as well as a smaller sub-species, Alces alces andersoni. Gigas, also known as Alaska moose or tundra moose, is found in Alaska, the Yukon and northwest British Columbia; andersoni, or anderson’s moose, is found in Southeast Alaska, the eastern Yukon, and central B.C east to Michigan.<br />
Impeded by mountain ranges, icefields and glaciers, moose did not colonize Southeast Alaska until the 20th century. They are far more recent arrivals than Sitka black-tailed deer and wolves, which moved up the coast from the south about 8,000 years ago as the glaciers melted and land was exposed. Moose from British Columbia accressed Southeast via the river corridors and arrived in the Taku River valley south of Juneau and the Stikine River basin near Petersburg about 1910.<br />
I had a memorable encounter with a large herd of moose in Adam’s Inlet in Glacier Bay in the middle of winter. I was standing on the mudflats at low tide and set up my tripod to photograph the moose on the shore. Gradually they started to walk towards me until eventually I was surrounded by at least 20 moose who were more curious about me than afraid; apparently their protected status in the National Park had made them fearless of humans.
    Alaska-wildlife-moose1.jpg
  • Amber Mountain National Park, a prominent volcanic massif in the north of the country, is the oldest protected area in Madagascar, and is known for its waterfalls and crater lakes, and is one of the most biologically diverse places in all of Madagascar with 75 species of birds, 25 of mammals, 59 species of reptiles, and ???? species of frogs.<br />
Although it is so accessible and supposedly Madagascar’s most visited natural attraction I was fortunate enough to be there when it was almost empty. The prominent view sites for the park’s waterfalls are really breathtaking. The night walks were very rewarding, especially for an abundance of frog species. The icing on the cake of a very rewarding trip there was discovering a beautiful leaf-tailed gecko on the tree that my hammock was attached to. I discovered it in the middle of the night when I got up to relieve myself. I had trekked far and wide in the hope of finding more of those amazing, elusive creatures and one blessed me with a personal visit in the dead of night.
    Kayaking-Madagascar-journey48.jpg