The Secrets of Gua Kandu: Revealed

"Kinta is a curious valley, walled with abrupt limestone cliffs and pinnacles, and ranges of weird hills full of caves, which gave the landscape the same wild character as those of Moulmein."

-C.M. Enriquez, Malaya: An Account of its People, Flora and Fauna, 1927.

The lush rainforests of Gunung Kandu.

Towering white cliffs draped in lush vegetation overlooking the vast valley below, Gunung Kandu (Kandu Mountain) has remained as it is millions of years ago. It has seen Paleolithic men chasing wild beasts across the bushlands, early Sumatran settlers clearing forests for fruit orchards and colonial era western adventurers wandering into its forests. Now, in its old age, it is inviting a new breed of visitors- tourists. And here I am with them, beating through the belukar (regenerating bushlands) on its foothills.

The forests near the entrance of Gua Kandu.

Minutes later, we emerged from the thick foliage and into a treeless chasm. A large, dark and forbidding gap in the hill signals the entrance to the ancient geological formation of Gua Kandu (Kandu Cave). Spanning 1100m in length with multiple entrance and passageways, it is the 7th longest cave in the Malay Peninsular. Having been shortlisted as one of the ten most important karst conservation sites in Kinta by the Malaysian Nature Society, its hill owns the typical karst title as one of the significantly high endemic wildlife diversity locations in Perak state, Malaysia.

Thus, it takes no time to spot one. I found these ferns, most probably endemics, growing on calcified red guano.

However pristine the cave may be, Gua Kandu has its fair share of vandalism by irresponsible visitor.

Our guide, David of Gopeng Rainforest Resort, made a quick briefing to our motley gruop of thrill-seeking tourists and wildlife enthusiasts. Soon, we were heading into the darkness through a low passage. It seems that Gua Kandu used to be a water cave with a stream running throughit, much like that of Gua Anak Tempurung.

The water stains along the wall of the cave possibly shows water levels of an ancient subterranean stream.

Dried crystals along the cave ceiling may well be growing wet crystals thousands of years ago.

As in many caves in Kinta Valley, Gua Kandu is a communist guerrilla hideout during the Malayan Emergency days. The insurgents made use of the impenetrable darkness of the cave as barrier for their enemies. Therefore, it is no surprise that we found remains of their presence in the form of graffiti (as seen below).

Remnants of a dark past on the walls of one of the cave's chambers.

Walking deeper into the cave, we came across an area with active, wet speleoterms (stalactites and stalagmites).

Various colours of stalactites indicate a rich composition of minerals and dissolved metal oxides.

Beaitiful "pillar" speleoterms displaying rust colours due to high iron contents in the dissolved limestone.

A smaller version of the "cascading" speleoterm can be seen along the cave walls. these are quite rare.

Surprisingly, there are a small number of fungus growing on bits and pieces of plant debris deep in the cave.

45 minutes into the cave, we had to clamber between a narrow sandwich of rock and guano floor before emerging into a larger chamber. The scene here is surreal with large sinkholes across the cave floor and a low ceiling over them.

One of the sinkholes in the low cave chamber.

Coming out of the tunnel, we passed a deep pool of water with steep guano deposits on its side. Roosting bats chattered high above us as our flashlights broke the darkness of the chamber. Larger flow stones can be seen on both sides. Magical "curtain" stalactites soar up into the chasm above.

An otherworldly scene in the cave.

Large curtain stalactite reminiscent of a frozen waterfall.

Another speleoterm resembling a pipe organ bathed in natural light from a cave opening nearby.

The two cave openings that allow some light into the dark recesses of Gua Kandu.

Passing several circular cave openings, we walked across a guano filled platform flanked by walls reaching up to 20m to the end of the passage way. Here, a small cliff gave way to a lower cave floor. We descended down the cliff with assistance of a rope and squeezed through a natural undercut at the cul-de-sac of the lower platform.

A strange composition of a rock vein resembling Statute of Liberty.

The chamber behind this structure was even more impressive with its ceiling almost 30m above us and speleoterms perching up the rocky slopes on both left and right, like guardians of an ancient temple.

The immense size of the chamber with its majestic formations.

A stalagmite with the uncanny appearance of a perching monkey.

Scaling to the top of the slope on the right, we spotted a peculiar shaped rock with the features of a lion head. Bright sunlight floods the area with two large openings facing the North-South Highway. From here, its a long way down a deep algae covered rock valley before climbing back up to the cave opening and out into the forests. However, we chose not to pick that path and descended back into the dark valley we had came out from instead.

The Lion's head is arguably one of Gua Kandu's most famous icon.

The cave opening facing the North-South Highway.

The deep valley between the slope and the cave opening is rugged and tricky to navigate.

A long beam of sunlight can be seen travelling down from the upper part of the cave and illuminating a section of some beautiful "cascade" formations below. It is a truly amazing sight yet surprisingly natural. We followed the path through the lighted area and ascended to the small exit on the other side of the cave. Turning over a sharp bend, we crossed a dried section of some large "cascade" speleoterms before reaching out through an opening and into the bright forest outside. I have found some Brotia costula varicosa (Torschel 1837) freshwater snail shells with their apex removed lying around loose soil at the cave opening. This is definitely a prehistoric food leftover as there are no sign of any water bodies in the immediate vicinity and this location is some 30m above ground level from the valley below.

A large "cascade" formation near the cave opening. It is a highly sought after find for speleologists and cave enthusiasts.

Finally, we were out under the forest canopy. Now, it's a slow descend down slippery moss covered limestone and avoiding pitfalls disguised by fallen leaves all the way to the foothills.

A typical scene of a karsts' forests on the upper elevations- thick beddings of relatively wet leaves interspersed with algae and moss covered rocks, shrubs and gnarled trees.

The strange thorny leaves of a probably limestone-endemic shrub. Most plants living on limestone soil contains high concentrations of calcium in their tissue which serves as a shell-building source for snails.

A perfect way to end the trip- I've found an interesting snail! This is Platyrhaphe lowi (de Morgan 1885). It fuses mud with its calcium rich mucous and glue them onto its shell, blending it into the soil habitat.

(Note: My special thanks to Gopeng Rainforest Resort for their assistance in making this trip successful.)

Reference:

1.Liz Price, 2001 Caves and Karsts of Peninsular Malaysia. Gua Publications, Kuala Lumpur, Malaysia.

2.Khoo Salma Nasution & Abdur-Razzaq Lubis Kinta Valley: Pioneering Malaysia's Modern Development. Perak Academy, 2005

Pulau Sipadan: The Story So Far

Pulau Sipadan- Jewel of the Celebes Sea

It has amazed thousands of visitors around the world with its serene coral reefs and profusion of marine biodiversity beyond imagination ever since renowned aquatic explorer,

Jacques Cousteau first penetrated into its depths in awe and wonder that is reflected in his well-versed quote- "I have seen no other places like Sipadan, 45 years ago, but now no more. Now we have found an untouched piece of art" during his expedition across the Sulu-Celebes Sea. Superlative descriptions have been a common "trademark" for Pulau Sipadan. Everyone who have visited this 12 hectares island carry their own accounts of adventures, each as amazing as the other. However, underlying all these colourful stories is one that many have not ventured into yet, a story that is as grand as its coral reefs - The Story of the Evolution of Pulau Sipadan into the island we know today.

Semporna town near Pulau Sipadan. The flatland across the shallow strait is Pulau Bum Bum and the tall imposing peaks behind it is Pulau Gaya and Pulau Boheydulang.

Beyond the acknowledgement of Pulau Sipadan as a oceanic, volcanic sea mount in tourists brochures, little else about its origin is mentioned. So, to fill this information gap that some visitors (including me) may wonder about, I've done a small online research to analyse and share this particular island's history with everyone. The following may not be a complete description of the island's formation but nevertheless, it sheds some light to this legendary island's origins.

To fully understand the geological history of Pulau Sipadan, we have to look at the bigger picture that is Sabah, the continental tip of Northern Borneo. Turning the clock back to more than 65 million years ago, much of North Borneo was submerged under deep waters. As the Tertiary period (65 million - 2.588 million years ago) begins, the first lands can be seen breaking the cerulean waters in the form of a chain of islands that resembles much more of a growing underwater mountain range of what is now the tallest in Borneo- the Crocker Range. As time progresses, clouds bringing storms and rains washed the slopes of these majestic mountain-islands, thus distributing alluvial deposits along the coast until these islands became linked.

Mount Kinabalu, at 4095m, is the tallest peak in Crocker Range at present day.

Kinabatangan Delta of present day Borneo gives us a glimpse of what Central Borneo used to be like.

The Eurasian Plate is where the Sundaland (the shallow, light blue area) is. The Philippine plate can be seen as a dark (deep) area off Northeastern Borneo.

The movement of Philippine plate against the Eurasian plate north of Sabah further pushes the mountain range higher and higher while creating a wide floodplain to the east with soil runoff from the highlands during the Miocene period (23.03 - 5.33 million years ago). Meanwhile, the same Philippine plate in the southeastern end of North Borneo starts to drift apart from the Eurasian "mainland", causing a rift and sets off the red hot lava bursting out of the cracked Earth crust from the deep magma below. Soon, the deep seas off the developing floodplains east of Crocker Range (now Central Sabah) were boiling hot with lava and pumice bursting out of the surface all the time. This will soon form most of Eastern Sabah, in which the Semporna Peninsula will emerge from the thick clouds of volcanic ashes.

Remains of ancient volcanoes in Tawau, west of Semporna.

Volcanic rocks of Tawau indicates the region was once highly active in volcanic activity.

Low tides exposes ancient volcanic pumice and rock deposits (dark brown areas) along mainland Semporna and Pulau Bum Bum.

Across the 100m tall developing volcanic cones along Semporna Peninsula, ashes spews and radiate out into the ocean and the ancient floodplains of Central Sabah, joining nearby islands and expanding its landmass. However, further out in the deep ocean off the edge of Eurasian Plate, an undersea volcano far removed from the bustling volcanic activity miles from it, silently build in height. Forwarding the frame in a year per second, one would see steam rising out from the deep Celebes Sea and then, a dark mass of rock and pumice pops out of the surface and extends in width and height. Pulau Sipadan is born. Since it is separated from mainland Semporna by deep waters, the lowland sediments of Semporna never made it to Sipadan.

Volcanic rocks exposed on Pulau Menampilik off Semporna.

The chain of islands off Southeastern Semporna with prominent exposed volcanic rocks.

Sometime later, the lava flows and plumes disappeared and volcanoes silenced. Clumps of greenery previously existed only in areas of least volcanic activity flourished and spreaded across the landscape. Gradually, the dark rocks of past ages got smothered in rainforests and mangroves, only occasionally protruding as hardened lava cones at higher peaks. Ashes not covered by vegetation end up being washed away by rains and wave action of the sea. As time progresses, the ice age of the Holocene (approximately 12000 years ago) arrives. As if a plug in a basin of seawater is being pulled, sea levels bordering the peninsula dramatically retreated 120m below sea level. Thus, "raising" the badly worn volcanic peaks of Semporna some 100m above that era's shoreline. Across the narrow band of water, Sipadan stood as a lonely, weathered and extinct volcano draped in lush forests on its slopes and coastal grasslands along it's coasts. During this time, some ancient fauna and flora might have migrated to the island through the deep but short passage of sea. There may be corals fringing the ancient coast as well.

Fertile soils encourage rapid growth of rainforests across the volcanic slopes of the mountains on mainland Semporna.

Manado Tua of North Sulawesi, Indonesia. Pulau Sipadan was once similar in appearance to this island when it was a volcanic mountain island many millenia ago.

Bukit Tengkorak with a volcanic outcrop, near Semporna town. The sign of an ancient volcanic land.

Fertile lands on the southeastern tip of Semporna Peninsula is the testimony of the volcanoes around the area.

Corals are the building blocks of Sipadan's limestone.

Approaching 6000 years before present day, the ending of ice age marked another dramatic event- the increase in sea level or mass-flooding. Once again, lowlands shrinked and forests of the past disappeared below the waves. The seawater soon reached present day levels at 6070 years before present, only to exceed another tenths of metres of height for the following millenia. Thus, the cone became completely submerged. Corals started to form at the top most part of the seamount, growing outwards slightly below sea level. Before long, the sea levels retreated again, exposing the limestone reefs to the atmosphere and creating habitat for forest recolonisation. During this period of emergence, parts of the limestone eroded to form a complex cave system complete with stalactites and stalagmites which will be known as the Turtles' Tomb or Cave due to the high numbers of unfortunate turtles trapped and died in the labyrinths of this cave. What happens next will define Sipadan's present day characteristics.

Coral-fringe islands is now part of Semporna's modern feature after the sea level rise.

The island chain in the foreground used to be high and dry with grasslands dominating valleys between them and the sea as well as mainland Semporna (background).

During the exposure of limestone, this may be what Sipadan looked like. Picture taken in Nusa Penida, Bali, Indonesia, an island made of raised coral limestone.

The submerged cave entrance to Turtle's Tomb.

Crevices like these may be the access routes to caves lying deep inside Sipadan limestone.

Being on a mobile, active edge of the Philippine plate, it so happened that Sipadan slides along the growing tectonic plate and the limestone forest began to submerged again, probably eliminating the terrestrial ecosystem all together. Then, polyps of modern corals settled on the ready-made reefs of craggy limestone to expand as a reef and form the strange shape of a "mushroom" along the top perimeter of the seamount. Up above water, the reefs slowly give way to a sand bank which accumulates and grows as time passes. Birds and storms bring driftwood, sea beans, plants and animals to colonise the sandy island. Finally, the ecosystem of coastal forests and coral reefs reached their climax that is Pulau Sipadan today.

The sand bar formed near Semporna show what modern Sipadan was like in the initial stages of development.

As sand accumulates, the land mass increases and vegetation flourishes as shown here in Pulau Mabul, near Sipadan.

Driftwood washed up by storms brings in many flora and fauna from nearby terrestrial ecosystems.

The product of millenia of colonisation by terrestrial flora and fauna- the dense coastal forest of Pulau Sipadan.

The famous vertical drop off of Sipadan. Could this be the upper part of the "mushroom" structure?

Diving along the ancient limestone cliff.

Sipadan today as seen from above (Google Earth).

Indeed, Pulau Sipadan has gone a long way since becoming a little lava-spewing bump at the edge of the Philippine Shelf and Eurasian Plate to the grandeur of today. Not surprisingly, the story of this tiny island in the Celebes Sea does not end here. Maybe Sipadan is going to expand its landmass? Or rather swept below the waves by climate change induced sea level rise? Or, as some joked, topple over into the abyss of the Celebes due to excessive pressure on the seamount by the "mushroom" coral limestone? (Note: The last theory is mend to be, well, a joke!)

Reference:
1.Charles S. Hutchison, 2006 The Unique Geology of Sabah (North Borneo). University of Malaya, Kuala Lumpur. (click here)

2. JED Fox. General Geology of Sabah (excerpt). Sabah Forestry Department. (click here)

3.Intercoastal Zone Management Project, 1998. Sabah Coastal Zone Profile. Town & Regional Planning Department Sabah. (click here)

4.Allagu Ballaguru and Gary Nichols, 2003. Tertiary stratigraphy and basin evolution, southern Sabah (Malaysian Borneo). Journal of Asian Earth Sciences V. 23, Iss. 4: 537-554

5.Mohd Harun Abdullah, Mazlin B. Mokhtar, Sanudin Hj. Tahir and Almah Bt.
Awaluddin, 1997. Do Tides Affect Water Quality in the Upper Phreatic Zone of a Small Oceanic Island – Sipadan Island, Malaysia? Environmental Geology 29(1/2):112-117

6.Ahmad Zaharin Aris, Mohd Harun Abdullah, Kim Kyoung Woong, 2006. Hydrochemical Analysis on seawater intrusion of small carbonate islands: Manukan and Sipadan, Sabah. Proceedings of the 2nd Southeast Asian Natural resources and Environmental Management Conference, kota Kinabalu, Nov. 21-23, 2006, pp.40-44