WORLD TOP 10 UN IDENTIFIED SECRETS.
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10.cano crystals in Colombia
Caño Crystals is a river located in the Serrenia de la
Macerana region of Columbia. This isn’t just any river, it has been referred to
as and “The Most Beautiful River in the World.” For much of the year it
looks just the same as any other river, but for a short amount of time between
September and November – in the transition period between wet and dry seasons –
it transforms into a wash of color. The reds, pinks, blues, greens and yellows
that adorn the river are actually unique types of flora growing on the
riverbed.
Caño
Cristales
|
|
liquid
rainbow, river of five colours
|
|
River
|
|
Caño
Cristales
|
|
Country
|
Colombia
|
Region
|
Meta
|
Source
|
Serranía de la
Macarena
|
Mouth
|
Guayabero River
|
Length
|
100 km (62 mi)
|
8. Fly Geyser, United States
Fly
Geyser, located in the Nevada Desert, is a collection of three large, colorful
mounds which continually shoot five feet of water straight up into the air. It
was accidentally created in 1916, during a routine well-drilling. It worked
normally until the 1960s, when heated geothermal water started spurting out
through the well. Dissolved minerals began to accumulate and gradually built up
into the large, colored mounds we see today. Fly Geyser is amongst the most
secret places on
Earth, as it’s located on private property and
no tourists or sightseers are allowed in.
Name origin
|
 |
Location
|
Fly Ranch, Washoe County, Nevada
|
Coordinates
|
 40°51′34″N 119°19′55″WCoordinates: 40°51′34″N 119°19′55″W |
Elevation
|
4,014 feet (1,223 m)
|
Type
|
Cone-type Geyser
|
Eruption height
|
5 feet (1.5 m) and growing
|
Frequency
|
Constant
|
Duration
|
Consta
|
History
The source of the Fly
Geyser field's heat is attributed to a very deep pool of hot rock where
tectonic rifting and faulting are common. Fly Geyser was accidentally created
during well drilling in
1964 while exploring for sources of geothermal energy. The well may not have been capped correctly,
or left unplugged, but either way, dissolved minerals started rising and
accumulating, creating the travertine mound
on which the geyser sits and continues growing. Water
is constantly released, reaching 5 feet (1.5 m) in the air. The geyser
contains several terraces discharging water into 30 to 40 pools over an area of
74 acres (30 ha). The
geyser is made up of a series of different minerals, but its brilliant colors are due to thermophilic algae.
In June 2016, the Burning Man Project announced that they had purchased the
Fly Ranch - which includes the geyser. The ranch (and geyser) are still closed
to the public, but some access is planned for the future.
Other local geysers
A prior
well-drilling attempt in 1917 resulted in the creation of a geyser close to the
currently active Fly Geyser; it created a pillar of calcium
carbonate about
12 feet (3.7 m) tall, but ceased when the Fly Geyser began releasing water
in 1964.
Two
additional geysers in the area were created in a similar way and continue to
grow.The first geyser is approximately 3 feet (0.91 m) and is shaped like
a miniature volcano; the second is cone-shaped and is about 5 feet (1.5 m)
7. Aokighara, Japan
Found at the
base of Mount Fuji, Aokighara is probably the most renowned forest in all of
Japan. This 3,500 hectare wide forest is thick with gnarled and twisted trees.
It’s reportedly haunted, with legends of ghosts, demons and spirits surrounding
the area. Sadly, it’s also the second most popular suicide spot in the world.
More than 500 people have committed suicide there since the 1950s. The forest has a historical reputation as a home to
"yūrei" or ghosts of the dead in Japanese
mythology. In recent
years, Aokigahara has become internationally known as arguably the world's most
popular destination for suicide, and signs at the head of some trails urges
suicidal visitors to think of their families and contact a suicide
prevention association. In
an exhaustive 2017 feature story on Mount Fuji, Smithsonian
magazine columnist Franz Lidz wrote: "Distraught teens and other troubled
souls straggle through the 7,680-acre confusion of pine, boxwood and white
cedar. In the eerie quiet, it’s easy to lose your way and those with second
thoughts might struggle to retrace their steps. According to local legend,
during the 1800s the Japanese custom of ubasute, in which elderly or infirm
relatives were left to die in a remote location, was widely practiced in the
Aokigahara.”
Flora and Fauna
While
clickbait articles on the Internet promoting Aokigahara as "creepy" claim that there are no animals in the
Aokigahara this is not true. The animals are just cautious and shy of human
presence as in many popular tourist destinations. Many are nocturnal. The
mammals include Asian Black
bear, Small
Japanese mole, bats, mice, deer, fox, boar, wild rabbit, Japanese
mink and squirrel. Birds include
great tit, willow tit, long-tailed tit, magerahigara, higera, great spotted
woodpecker, pygmy woodpecker, bush warbler, Eurasian jay, Japanese white-eye,
Japanese thrush, brown-headed thrush, Siberian thrush, Hodgson’s hawk-cuckoo,
Japanese grosbeak, lesser cuckoo, black-faced bunting, Oriental turtle dove, and
common cuckoo.
There
are ground beetles and other insects, including
many species of butterflies, even in the forest interior Argynnis paphia, Chrysozephyrus smaragdinus, Celastrina argiolus, Celastrina
sugitanii, Curetis acuta, Favonius
jezoensis, Neptis sappho,Parantica sita and Polygonia c-album are found.
The
forest has a wide variety of conifers and broadleaf trees and shrubs including:Chamaecyparis obtusa, Cryptomeria japonica, Pinus densiflora, Pinus parviflora,Tsuga sieboldii, Acer
distylum, Acer micranthum, Acer sieboldianum, Acer
tschonoskii,Betula grossa, Chengiopanax
sciadophylloides (as Acanthopanax sciadophylloides a.k.a.Eleutherococcus sciadophylloides), Clethra barbinervis, Enkianthus campanulatus,Euonymus
macropterus, Ilex
pedunculosa, Ilex
macropoda, Pieris japonica, Prunus jamasakura, Quercus mongolica var. crispula, Rhododendron
dilatatum, Skimmia japonica f. repens, Sorbus
commixta (as Sorbus
americana ssp. japonica)
andToxicodendron trichocarpum (as Rhus trichocarpa). The dominant tree species between 1000
and 1800 metres of altitude is Tsuga diversifolia and from 1800 to 2200 metres is Abies veitchii.
Even
deep in the forest there are many herbaceous flowering plants including Artemisia princeps, Cirsium nipponicum var. incomptum, Corydalis
incisa], Erigeron
annuus, Geranium nepalense, Kalimeris
pinnatifida], Maianthemum dilatatum,Oplismenus
undulatifolius] and Polygonum cuspidatum]. There are also the myco-heterotrophic Monotropastrum humile] frequent liverworts, many mosses and many ferns. The
forest edges have many more species.
Suicides
Aokigahara
is sometimes referred to as the most popular site for suicide
in Japan.
Statistics vary, but there were around up to 105 documented suicides a year.
In
2003, 105 bodies were found in the forest, exceeding the previous record of 78
in 2002. In 2010, the police
recorded more than 200 people having attempted
suicide in the
forest, of whom 54 completed the act. Suicides
are said to increase during March, the end of the fiscal
year in
Japan. As of 2011, the most
common means of suicide in the forest were hanging or drug overdose. In recent years, local officials have
stopped publicizing the numbers in an attempt to decrease Aokigahara's
association with suicide.
The
rate of suicide has led officials to place a sign at the forest's entry,
written in Japanese, urging suicidal visitors to seek help and not take their
own lives. Annual body searches have been conducted by police, volunteers, and
attendant journalists since 1970.
The
site's popularity has been attributed to Seichō Matsumoto's 1960 novel Kuroi Jukai(Black Sea of Trees). However,
the history of suicide in Aokigahara predates the novel's publication, and the
place has long been associated with death; ubasute may have been practiced there into the
nineteenth century, and the forest is reputedly haunted by the yūrei of
those left to die
6. The Bermuda Triangle, Atlantic Ocean
What would a
list of mysterious places be without a mention of the Bermuda Triangle? For
anyone who doesn’t know, it’s a triangular area in the Atlantic ocean, between
Miami, Bermuda and San Juan. Over the years, the area has captured our
imaginations, with reports of seemingly unexplainable disappearances of planes,
ships and people. No one can say for sure what happened in these cases, but
theories are as far ranging as sea monsters, alien abduction and simple weather
conditions.
Triangle area
In 1964, Vincent Gaddis wrote in the pulp magazine Argosy of the boundaries of the Bermuda Triangle three vertices, in Miami, Florida peninsula, in San Juan, Puerto Rico, and in the
mid-Atlantic island of Bermuda. Subsequent
writers did not necessarily follow this definition. Some writers gave different boundaries
and vertices to the triangle, with the total area varying from 1,300,000 to
3,900,000 km2 (500,000 to 1,510,000 sq mi). Consequently, the determination of
which accidents occurred inside the triangle depends on which writer reported
them.The United States
Board on Geographic Names does not recognize the Bermuda Triangle.
Paranormal explanations
Triangle
writers have used a number of supernatural concepts to explain the events. One
explanation pins the blame on leftover technology from the mythical lost
continent ofAtlantis.
Sometimes connected to the Atlantis story is the submerged rock formation known
as the Bimini Road off
the island of Bimini in
the Bahamas, which is in the Triangle by some definitions. Followers of the
purported psychic Edgar
Cayce take
his prediction that evidence of Atlantis would be found in 1968 as referring to
the discovery of the Bimini Road. Believers describe the formation as a road,
wall, or other structure, but the Bimini Road is of natural origin.
Other
writers attribute the events to UFOs. This
idea was used by Steven
Spielbergfor his science fiction film Close
Encounters of the Third Kind, which
features the lost Flight 19 aircrews as alien
abductees.
Charles
Berlitz,
author of various books on anomalous phenomena, lists several theories
attributing the losses in the Triangle to anomalous or unexplained forces.
Natural explanations
Compass variations
Compass problems are one of the cited phrases in
many Triangle incidents. While some have theorized that unusual local magnetic
anomalies may exist in the area such
anomalies have not been found. Compasses have natural magnetic variations in relation to the magnetic poles, a fact which navigators have known for
centuries. Magnetic (compass) north and geographic
(true) north are only exactly the same for a small
number of places – for example, as of 2000, in the United States, only those
places on a line running from Wisconsin to the Gulf of
Mexico. But
the public may not be as informed, and think there is something mysterious
about a compass "changing" across an area as large as the Triangle,
which it naturally will.
Gulf Stream
The Gulf
Stream is a
major surface current, primarily driven by thermohaline
circulation that
originates in the Gulf of Mexico and then flows through the Straits of Florida into the North Atlantic. In essence, it is
a river within an ocean, and, like a river, it can and does carry floating
objects. It has a surface velocity of up to about 2.5 metres per second
(5.6 mi/h). A small plane
making a water
landing or a
boat having engine trouble can be carried away from its reported position by
the current.
Human error
One of
the most cited explanations in official inquiries as to the loss of any
aircraft or vessel is human error. Human
stubbornness may have caused businessman Harvey Conover to lose his sailing
yacht, the Revonoc, as he sailed into the teeth
of a storm south of Florida on January 1, 1958.
Violent weather
Tropical
cyclones are
powerful storms, which form in tropical waters and have historically cost
thousands of lives and caused billions of dollars in damage. The sinking ofFrancisco de Bobadilla's Spanish fleet in 1502 was the first recorded instance of a
destructive hurricane. These storms have in the past caused a number of
incidents related to the Triangle.
A
powerful downdraft
of cold air was suspected to be a cause in the sinking
of the Pride of Baltimore on May 14, 1986. The crew of the sunken
vessel noted the wind suddenly shifted and increased velocity from 32 km/h
(20 mph) to 97–145 km/h (60–90 mph). A National Hurricane Center
satellite specialist, James Lushine, stated "during very unstable weather
conditions the downburst of cold air from aloft can hit the surface like a
bomb, exploding outward like a giant squall line of wind and water." A similar event occurred to the Concordia in 2010 off the coast of Brazil. Scientists
are currently investigating whether "hexagonal" clouds may be the source of these
up-to-170 mph "air bombs".
Methane hydrates
An
explanation for some of the disappearances has focused on the presence of large
fields ofmethane hydrates (a form of natural gas) on thecontinental shelves. Laboratory experiments carried out in Australia have proven
that bubbles can, indeed, sink a scale model ship by decreasing the density of
the water; any wreckage
consequently rising to the surface would be rapidly dispersed by the Gulf Stream.
It has been hypothesized that periodic methaneeruptions (sometimes called "mud
volcanoes")
may produce regions of frothy water that are no longer capable of providing
adequatebuoyancy for ships. If this were the case, such an
area forming around a ship could cause it to sink very rapidly and without warning.
Publications
by the USGS describe large stores of undersea hydrates
worldwide, including the Blake
Ridge area,
off the coast of the southeastern United States.However, according to the USGS,
no large releases of gas hydrates are believed to have occurred in the Bermuda
Triangle for the past 15,000 years.[18]
5. Moguicheng, China
Moguicheng
is a desert in the Xinjiang region of China. The name literally translates to
City of Satan or Devil’s City. Walking through the desert toward an old
abandoned city, people have reported some extremely strange occurrences.
Visitors are adamant that they’ve heard a range of mysterious sounds floating
on the breeze, from weird melodies and the sound of guitar strings gently being
plucked to babies crying and tigers roaring. These sounds are apparently
inexplicable, nobody has yet been able to find any sort of source.
4. Richat Structure, Mauritania
The
Richat Structure is also known as the Eye of the Sahara. It’s a distinct and
prominent circular geographical feature in the Sahara Desert. At roughly 30
miles wide, you probably wouldn’t notice that you were within it, but from an
aerial view – and even from space – it is highly visible. Originally, it was
thought to be the product of an asteroid impact and later people thought it
could have been created by a volcanic eruption. The main school, of thought
today says that it was once a circular rock formation that has gradually been
eroded. Several mysteries still surround the areas, such as why the structure
is nearly a perfect circle and why the rings are equidistant from each other
Geology
Exposed
within the interior of the Richat Structure are a variety of intrusive and extrusiveigneous rocks. They include rhyolitic volcanic
rocks, gabbros, carbonatites andkimberlites. The rhyolitic rocks consist of lava flows and hydrothermally alteredtuffaceous rocks that are part of two distinct
eruptive centers, which are interpreted to be the eroded remains of two maars.
According to field mapping and aeromagnetic data, the gabbroic rocks form two
concentric ring dikes. The inner ring dike is about 20 m
in width and lies about 3 km from the center of Richat Structure. The
outer ring dike is about 50 m in width and lies about 7 to 8 km from
the center of this structure. Thirty-two carbonatite dikes and sills have
been mapped within the Richat Structure. The dikes are generally about
300 m long and typically 1 to 4 m wide. They consist of massive
carbonatites that are mostly devoid of vesicles. The carbonatite rocks have been
dated as having cooled between 94 and 104 million years ago. A kimberlitic
plug and several sills have been found within the northern part of the Richat
Structure. The kimberlite plug has been dated to around 99 million years
old. These intrusive igneous rocks are interpreted as indicating the presence
of a large alkaline igneous intrusion that currently underlies the Richat
Structure and created it by uplifting the overlying rock.
Spectacular
hydrothermal features are a part of the Richat Structure. They include the
extensive hydrothermal
alteration of
rhyolites and gabbros and a central megabrecciacreated by hydrothermal dissolution
and collapse. The siliceous megabreccia is at least 40 m thick in its
center to only a few meters thick along its edges. The breccia consists of
fragments of white to dark gray cherty material, quartz-rich sandstone, diagenetic cherty
nodules, and stromatolitic limestone and
is intensively silicified. The hydrothermal alteration, which created this
breccia, has been dated to have occurred about 98.2 ± 2.6 million years
ago using the 40Ar/39Ar method.
Origins
Initially
interpreted as an asteroid impact structure because of its high degree of
circularity, the Richat Structure is now regarded by geologists as a highly
symmetrical and deeply eroded geologic dome. After extensive field and
laboratory studies, no credible evidence has been found for shock metamorphism or any type of deformation indicative
of a hypervelocity extraterrestrial impact. While coesite, an indicator of shock metamorphism,
had initially been reported as being present in rock samples collected from the
Richat Structure, further analysis of rock samples concluded that barite had
been misidentified as coesite. In
addition, the Richat Structure lacks the annular depression that characterizes
large extraterrestrial impact structures of this size. Also, it is quite
different from large extraterrestrial impact structures in that the sedimentary
strata comprising this structure is remarkably intact and "orderly"
and lacking in overturned, steeply dipping strata or disoriented blocks. A more recent multianalytical study on
the Richat megabreccias concluded that carbonates within the silica-rich
megabreccias were created by low-temperature hydrothermal waters, and that the
structure requires special protection and further investigation of its origin.
3. Travertine Pools of Pamukkale, Turkey
The Travertine Pools of Pamukkale are as wonderful to behold as they are ethereal-looking. Over the years, white travertine mineral deposits have built up in this area of hot springs, creating a series of white terraces. These natural pools are blindingly white and filled with clear blue waters. These strange terraced pools have been appreciated for at least 2,000 years, and they’re sure to last for many more. Pamukkale, meaning "cotton castle" in Turkish, is a natural site in Denizli Province in southwestern Turkey. The city contains hot springs andtravertines, terraces of carbonate minerals left by the flowing water. It is located in Turkey's Inner Aegeanregion, in the River Menderes valley, which has a temperate climate for most of the year.
The
ancient Greco-Roman city ofHierapolis was built on top of the white
"castle" which is in total about 2,700 metres (8,860 ft) long,
600 m (1,970 ft) wide and 160 m (525 ft) high. It can be
seen from the hills on the opposite side of the valley in the town of Denizli, 20 km away.
Known as Pamukkale (Cotton Castle) or ancient Hierapolis (Holy
City), this village has been drawing the weary to its thermal springs for more
than 23 centuries. The Turkish name refers to the surface of the shimmering,
snow-white limestone, shaped over millennia by calcium-rich springs. Dripping
slowly down the vast mountainside, mineral-rich waters foam and collect in
terraces, spilling over cascades of stalactites into milky pools below. Legend
has it that the formations are solidified cotton (the area’s principal crop)
that giants left out to dry.
Overshadowed by natural wonder, Pamukkale’s well-preserved Roman
ruins and museum have been remarkably underestimated and unadvertised; tourist
brochures over the past 20 years have mainly featured photos of people bathing
in the calcium pools. Aside from a small footpath running up the mountain face,
the terraces are all currently off-limits, having suffered erosion and water
pollution at the feet of tourists. While it is not open for bathing, the site
is still worth a visit. Although many travelers come to Pamukkale only as a
hasty day trip from Kuşadası or Selçuk.
Tourism is and has been a major industry. People have bathed in
its pools for thousands of years. As recently as the mid-20th century, hotels
were built over the ruins of Hierapolis, causing considerable damage. An
approach road was built from the valley over the terraces, and motor bikes were
allowed to go up and down the slopes. When the area was declared a World Heritage Site,
the hotels were demolished and the road removed and replaced with artificial
pools. Wearing shoes in the water is prohibited to protect the deposits.
UNESCO World Heritage
Site
|
|
Location
|
Denizli, Turkey
|
Criteria
|
iii,
iv, vii
|
Reference
|
485
|
Coordinates
|
37°55′23″N 29°07′26″E |
Inscription
|
1988 (12th Session)
|
Website
| |
2. McMurdo Dry Valleys, Antarctica
The McMurdo Dry
Valleys could be the most secret place on Earth. This little-known area is one
of the most extreme deserts and perhaps the driest place in the world –
receiving just 4 inches of precipitation each year – but strangely it’s located
slap bang in the middle of the usual ice and snow of Antarctica. Rather than
being covered in snow, this bleak and barren landscape is completely bare. The
area even lacks any terrestrial vegetation, although some lichens, mosses and
nematodes live there. Scientists have said that the Dry Valley area is probably
the place on this planet that is most similar to the environment on Mars
Climate
The Dry
Valleys are so named because of their extremely low humidity and
their lack of snow or ice cover. They are also dry because, in this location,
the mountains are sufficiently high that they block seaward flowing ice from
the East Antarctic ice
sheet from reaching
the Ross Sea. At 4,800 square kilometres
(1,900 sq mi), the valleys constitute around 0.03% of the continent,
and form the largest ice-free region in Antarctica. The valley floors are
covered with loose gravel, in which ice wedge polygonal patterned ground may be observed.
The unique conditions in the Dry Valleys are caused, in part, by katabatic winds; these occur when cold, dense
air is pulled downhill by the force of gravity. The winds can reach speeds of
320 kilometres per hour (200 mph), heating as they descend, and
evaporating all water, ice and snow.
Geology
The
valleys cut through the Beacon Supergroup, as well as older granites
and gneisses of the Ross Orogeny. Deposited directly from ice, tillsdot
this bedrock landscape. These are relatively thin and patchy, and differ
markedly from the extensive, mud-rich tills of the Laurentide ice sheet in the Northern Hemisphere. One reason
for the difference is that most of the tills in the Dry Valleys were deposited
from cold-based ice (ice with basal temperatures below 0 °C (32 °F)),
whereas the Laurentide ice sheet was largely wet-based, with significant
melting at the base and at the glacier surface.
Life
Endolithic photosynthetic bacteria have
been found living in the Dry Valleys, sheltered from the dry air in the
relatively moist interior of rocks. Summer meltwater from
the glaciers provides the primary source of soil nutrients. Scientists consider the Dry
Valleys perhaps the closest of any terrestrial environment to the planet Mars,
and thus an important source of insights into possible extraterrestrial life.
Anaerobic bacteria whose metabolism is based on
iron and sulfur live in sub-freezing temperatures under the Taylor Glacier. It was previously thought that
the algae was staining red the ice emerging at Blood Falls but
it is now known that the staining is caused by high levels of iron oxide.
Canadian and American researchers conducted a field expedition
in 2013 to University Valley in order to examine the microbial population and
to test a drill designed for sampling on Mars in the permafrost of the driest
parts of the valleys, the areas most analogous to the Martian surface. They
found no living organisms in the permafrost, the first location on the planet
visited by humans with no active microbial life.
Part of the Valleys was designated an environmentally protected
area in 2004.
.
1.Mount Roraima, Brazil
Mount Roraima is
particularly unusual to look at because, rather than finishing in a peak like
most mountains, its top is a large plateau. It’s thought to be amongst the
world’s oldest geological formations, and its plateau was most likely created
by winds and rains. The plateau is often cloaked with clouds, which are more
often than not near the top of the mountain. It has a particularly large number
of endemic species of flora and fauna – species that can can be found nowhere
else on Earth. There’s no explanation as to why it has such an unusually large
amount.
Flora and fauna
Many of
the species found on Roraima are unique to the tepui plateaus with 2 local
endemic plants found on Roraima summit. Plants such aspitcher plants (Heliamphora), Campanula (a bellflower), and the rare Rapatea heather are commonly found on the
escarpment and summit. It rains
almost every day of the year. Almost the entire surface of the summit is bare sandstone, with only a few bushes (Bonnetia roraimœ) and algae present. Low scanty and bristling
vegetation is also found in the small, sandy marshes that intersperse the rocky
summit.Most of the nutrients that
are present in the soil are washed away by torrents that cascade over the edge,
forming some of the highest waterfalls in the world.
There are multiple examples of unique fauna atop Mount Roraima. Oreophrynella
quelchii, commonly called the Roraima Bush Toad, is a diurnal toad
usually found on open rock surfaces and shrubland. It is a species of toad in
the family Bufonidae and
breeds by direct development. The species is currently listed as vulnerable and there is a need for increased
education among tourists to make them aware of the importance of not handling
these animals in the wild. Close population monitoring is also required,
particularly since this species is known only from a single location. The
species is protected in Monumento Natural Los Tepuyes in Venezuela, and Parque Nacional Monte Roraima in Brazil.
Culture
Since long before the arrival of European explorers, the
mountain has held a special significance for the indigenous people of the
region, and it is central to many of their myths and legends. The Pemon and Kapon natives of the Gran Sabana see
Mount Roraima as the stump of a mighty tree that once held all the fruits and
tuberous vegetables in the world. Felled by Makunaima, their mythical
trickster, the tree crashed to the ground, unleashing a terrible flood. Roroi in the Pemon language means blue-green
and ma means great.
Ascents
Although
the steep sides of the plateau make it difficult to access, it was the first
recorded major tepui to be climbed: SirEverard im Thurn walked up a forested ramp in December
1884 to scale the plateau. This is the same route hikers take today.The only
non-technical route to the top is the Paraitepui route from Venezuela; any
other approach will involve climbing gear. Mount Roraima has been climbed on a
few occasions from the Guyana and Brazil sides, but as the mountain is entirely
bordered on both these sides by enormous sheer cliffs that include high
overhanging (negative-inclination) stretches, these are extremely difficult and
technical rock climbing routes. Such climbs would also require
difficult authorizations for entering restricted-access national parks in the
respective countries.
In
Brazil the Monte Roraima
National Park lies
within the Raposa Serra do Sol Indigenous Territory, and is not open
to the public without permission.
The 2013 Austrian documentary Jäger des Augenblicks - Ein Abenteuer am
Mount Roraima (Moment Hunters - An Adventure on Mount Roraima) shows rock climbers Kurt Albert,
Holger Heuber, and Stefan Glowacz climbing to the top of Mount Roraima
from the Guyana side. Similarly, in 2010 Brazilian climbers Eliseu Frechou,
Fernando Leal and Márcio Bruno opened a new route on the Guyanese side,
climbing to the top in 12 days of a very difficult vertical wall climb. They called the new route Guerra
de Luz e Trevas(Portuguese for "War of Light and Darkness")
and classed it as 6° VIIa A3 J4. A 28-minute Vimeo video called Dias
de Tempestade (Days of Storm) is
available documenting their climb (English subtitles, audio in Portuguese).
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