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June 2016 ~ World Eyes Travel

Saturday, June 25, 2016

Uluru/Ayers Rock, Australia

Ayers Rock is also known by its Aboriginal name 'Uluru'. It is a sacred part of Aboriginal creation mythology, or dreamtime - reality being a dream. Uluru is considered one of the great wonders of the world and one of Australia's most recognizable natural icons. Uluru is a large magnetic mound large not unlike Silbury Hill in England. It is located on a major planetary grid point much like the Great Pyramid in Egypt.

Ayers Rock is a large sandstone rock formation in central Australia, in the Northern Territory. It is located in Uluru-Kata Tjuta National Park, 350 km southwest of Alice Springs at 25 degrees 20' 41" S 131 degrees 01' 57" E. It is the second-largest monolith in the world (after Mount Augustus, also in Australia), more than 318 m (986 ft) high and 8 km (5 miles) around. It also extends 2.5 km (1.5 miles) into the ground. It was described by explorer Ernest Giles in 1872 as "the remarkable pebble".'

Uluru is an inselberg, literally "island mountain", an isolated remnant left after the slow erosion of an original mountain range. Uluru is also often referred to as a monolith, although this is a somewhat ambiguous term because of its multiple meanings, and thus a word generally avoided by geologists. The remarkable feature of Uluru is its homogeneity and lack of jointing and parting at bedding surfaces, leading to the lack of development of scree slopes and soil. These characteristics led to its survival, while the surrounding rocks were eroded. For the purpose of mapping and describing the geological history of the area, geologists refer to the rock strata making up Uluru as the Mutitjulu Arkose, and it is one of many sedimentary formations filling the Amadeus Basin.

Age and Origin

The Mutitjulu Arkose is believed to be of about the same age as the conglomerate at Kata Tjuta, and to have a similar origin despite the rock type being different, but it is younger than the rocks exposed to the east at Mount Conner, and unrelated to them. The strata at Uluru are nearly vertical, dipping to the south west at 85 degrees, and have an exposed thickness of at least 2,400 m (7,900 ft).

The strata dip below the surrounding plain and no doubt extend well beyond Uluru in the subsurface, but the extent is not known. The rock was originally sand, deposited as part of an extensive alluvial fan that extended out from the ancestors of the Musgrave, Mann and Petermann Ranges to the south and west, but separate from a nearby fan that deposited the sand, pebbles and cobbles that now make up Kata Tjuta.


The similar mineral composition of the Mutitjulu Arkose and the granite ranges to the south is now explained. The ancestors of the ranges to the south were once much larger than the eroded remnants we see today. They were thrust up during a mountain building episode referred to as the Petermann Orogeny that took place in late Neoproterozoic to early Cambrian times (550-530 Ma), and thus the Mutitjulu Arkose is believed to have been deposited at about the same time.
The arkose sandstone which makes up the formation is composed of grains that show little sorting based on grain size, exhibit very little rounding and the feldspars in the rock are relatively fresh in appearance. This lack of sorting and grain rounding is typical of arkosic sandstones and is indicative of relatively rapid erosion from the granites of the growing mountains to the south. The layers of sand were nearly horizontal when deposited, but were later tilted to their near vertical position during a later episode of mountain building, possibly the Alice Springs Orogeny of Palaeozoic age (400-300 Ma).

Despite current estimates of the age of the geological formations that comprise Uluru, however, the arkose sandstone which makes up the formation is composed of grains that are many different sizes and are jagged, and the feldspars in the rock are fresh and shiny. Flood geologists argue that this indicates a comparatively fast deposit, on the order of only a few years or less. They state that if the arkose grains had been transported more slowly they would be more rounded and evenly sorted, and the feldspars would have turned to clay in the intervening years.

History

Archaeological findings to the east and west indicate that humans settled in the area more than 10,000 years ago. Europeans arrived in the Australian Western Desert in the 1870s. Uluru and Kata Tjuta were first mapped by Europeans in 1872 during the expeditionary period made possible by the construction of the Australian Overland Telegraph Line. In separate expeditions, Ernest Giles and William Gosse were the first European explorers to this area.

While exploring the area in 1872, Giles sighted Kata Tjuta from a location near Kings Canyon and called it Mount Olga, while the following year Gosse observed Uluru and named it Ayers Rock. Further explorations followed with the aim of establishing the possibilities of the area for pastoralism. In the late 1800s, pastoralists attempted to establish themselves in areas adjoining the South western/Petermann Reserve and interaction between Anangu and white people became more frequent and more violent. Due to the effects of grazing and drought, bush food stores became depleted. Competition for these resources created conflict between the two groups, resulting in more frequent police patrols. Later, during the depression in the 1930s, Anangu became involved in dingo scalping with 'doggers' who introduced Anangu to European foods and ways.

Between 1918 and 1921, large adjoining areas of South Australia, Western Australia and Northern Territory were declared as Aboriginal reserves, sanctuaries for nomadic people who had virtually no contact with European settlers. In 1920, part of Uluru - Kata Tjuta National Park was declared an Aboriginal Reserve (commonly known as the South-Western or Petermann Reserve) by the Australian government under the Aboriginals Ordinance.

The first tourists arrived in the Uluru area in 1936. Beginning in the 1940s, permanent European settlement of the area for reasons of the Aboriginal welfare policy and to help promote tourism of Uluru. This increased tourism prompted the formation of the first vehicular tracks in 1948 and tour bus services began early in the following decade.

In 1958, the area that would become the Uluru - Kata Tjuta National Park was excised from the Petermann Reserve; it was placed under the management of the Northern Territory Reserves Board and named the Ayers Rock - Mount Olga National Park. The first ranger was Bill Harney, a well-recognised central Australian figure. By 1959, the first motel leases had been granted and Eddie Connellan had constructed an airstrip close to the northern side of Uluru.

On 26 October 1985, the Australian government returned ownership of Uluru to the local Pitjantjatjara Aborigines, with one of the conditions being that the Anangu would lease it back to the National Parks and Wildlife agency for 99 years and that it would be jointly managed. The Aboriginal community of Mutitjulu, population of approximately 300, is located near the western end of Uluru. From Uluru it is 17 km (11 mi) by road to the tourist town of Yulara, population 3,000, which is situated just outside of the national park.
Kata Tjuta National Park is owned and run by the local Aboriginals. The Australian government handed ownership of the land back to the Aboriginals some years ago.

The Caves

The caves in Uluru can be both engaging and enlightening. To truly experience the power of Ayers Rock, your journey should be more than a few hours. Take your time to absorb the history of the springs, caves, and ancient paintings throughout the formation and don't worry about running your business. The first Aboriginal settlers arrived there more than 10,000 years ago and created a historical journey that would be difficult to transverse overnight so the recommendation for any tourists traveling to the formation has always been to allow more time to absorb the area without being distracted.

Ayers Rock was named for the Premier of South Australia, Sir Henry Ayers. It extends down over 3 and a half miles beneath the surface. Approximately 500 million years ago it was part of the ocean floor at the center of Australia. Some report that there is a light source emanating at various times of the year. Most likely this can be explained scientifically.

The Aborigines believe that there it is hollow below ground, and that there is an energy source that they call 'Tjukurpa' the dream time. The term Tjukurpa is also used to refer to the record of all activities of a particular ancestral being from the very beginning of his or her travels to their end. Anangu know that the area around

Ayers Rock (Mount Uluru) is inhabited by dozens of ancestral 'beings' whose activities are recorded at many other sites. At each site, the events that took place can be recounted, whether those events were of significance or whether the ancestral being just rested at a certain place before going on.

Usually, there is a physical feature of some form at each ancestral site which represents both the activities of the ancestral being at the time of its formation and the living presence of Tjukurpa within that physical feature today. For the Australian Aboriginal people, that physical feature, whatever its form or appearance, animate or inanimate, is the Tjukurpa. It may be a rock, a sand hill, a grove of trees, a cave. For all of these, the creative essence remains forever within the physical form or appearance.

Around Mount Uluru there are many examples of ancestral sites. The Anangu explanations of these sites and of the formation of Mount Uluru itself derive from the Tjukurpa. Most of these explanations are in the realm of secret information and are not disclosed to Piranypa, the non-Aborigines.

'The Dreaming' is not a creation myth, per se, but a myth of formation. The world existed, but was featureless. Giant semi-human beings, resembling plants or animals, rose up from the plains where they had been slumbering for countless ages.

These ancient heroes roamed the land aimlessly. As they wandered around, they carried out the tasks that the present Aborigines do today including camping, making fires, digging for water, fighting each other, and performing ceremonies. When the heroes became tired of doing these things, Dreamtime came to an end.

Wherever the creators had been active, some form of natural feature now marks the place. The creators made everything with which the aborigines are in daily contact and from which they gain their living. The heroes also established laws that govern all aspects, both secular and sacred, of the tribes.

Dreamtime was in the past, but it is the Aborigines present religion and culture. The saying, 'As it was done in the Dreamtime, so it must be done today,' dominates all aspects of aboriginal behavior. Because of their beliefs in 'the dreaming,' ceremonies and rituals are held, stories are told, pictures are drawn, and daily life is defined.

In order to understand the religion of the Aborigines, one must have a basic understanding of the organization of the tribes. All men and women belong to small groups, called clans. Each clan posses a distinct body of spiritual properties, or sacred sites. A clan may have several sacred sites that they claim, and the area surrounded by the connection of these sites forms the clan's estate. Clans are linked by common religious traditions, intermarriage, shared dialects, and overlapping foraging rights.

Each clan has a totem. 'Totemism is a view of nature and life, of the universe and man, which colors and influences the Aborigines' social groupings and mythologies, inspires their rituals and links them to the past. It unites them with nature's activities and species in a bond of mutual life-giving, and imparts confidence amidst the vicissitudes of life'. The totem provides a tangible expression of a man's relationship to his deities. Everything in the Aboriginal world contains an essence or spirit that had its beginnings in the Dreamtime. Each person descended from one of these spirits and possessed some of its life force. The spirit it descended from is the person's totem. Images of totems make-up a large part of Aboriginal art. They were painted on cave walls, which we title rock art, drawn on the interiors of their huts, drawn on their bodies, and carved in wood. Totemic spirits are celebrated in ceremonies and rituals, and played a prominent part in Aboriginal myth.

Myths, Legends and Aboriginal Traditions

According to the Anangu traditional landowners of Uluru:
"The world was once a featureless place. None of the places we know existed until creator beings, in the forms of people, plants and animals, traveled widely across the land. Then, in a process of creation and destruction, they formed the landscape as we know it today. Anangu land is still inhabited by the spirits of dozens of these ancestral creator beings which are referred to as Tjukuritja or Waparitja."

There are a number of unauthenticated accounts of the Aboriginal ancestral stories for the origins of Uluru and its many cracks and fissures. One such account, taken from Robert Layton's (1989) ULURU: An Aboriginal history of Ayers Rock, reads as follows:
"Uluru (Ayers Rock) was built up during the creation period by two boys who played in the mud after rain. When they had finished their game they travelled south to Wiputa ..Fighting together, the two boys made their way to the table topped Mount Conner, on top of which their bodies are preserved as boulders" (Page 5)

Two other accounts are given in Norbert Brockman's (1997) Encyclopedia of Sacred Places. The first tells of serpent beings who waged many wars around Uluru, scarring the rock. The second tells of two tribes of ancestral spirits who were invited to a feast, but were distracted by the beautiful Sleepy Lizard Women and did not show up. In response, the angry hosts sang evil into a mud sculpture that came to life as the dingo. There followed a great battle, which ended in the deaths of the leaders of both tribes. The earth itself rose up in grief at the bloodshed, becoming Uluru.

The Commwealth Department of Environment's webpage advises:
"Many .. Tjukurpa such as Kalaya (Emu), Liru (poisonous snake), Lungkata (blue tongue lizard), Luunpa (kingfisher) and Tjintir-tjintirpa (willie wagtail) travel through Uluru-Kata Tjuta National Park. Other Tjukurpa affect only one specific area.
"Kuniya, the woma python, lived in the rocks at Uluru where she fought the Liru, the poisonous snake."


It is sometimes reported that those who take rocks from the formation will be cursed and suffer misfortune. There have been many instances where people who removed such rocks attempted to mail them back to various agencies in an attempt to remove the perceived curse.

Friday, June 24, 2016

Punalu'u, Hawaii, United States

Punaluʻu (pronounced [punəluʔu]) is a census-designated place and rural community in the Koʻolauloa District on the island ofOʻahu, City & County of Honolulu, Hawaii, United States. In Hawaiian, punaluʻu means "coral dived for", or in the case of the fishpond once located here, possibly "spring dived for". There is a very small commercial center located beside Punaluʻu Stream, and several condominium projects, including a high-rise building, located at Haleaha Beach and Kaluanui Beach. At the 2010 Census, the CDP had a population of 1,164.
A fringing reef extends off the shoreline. There are several beaches and a beach park in Punaluʻu, including Punaluʻu Beach Park, Punaluʻu Beach, Haleaha Beach, and Kaluanui Beach. Sugar cane was once grown on the narrow coastal plain inland from the highway.
The U.S. postal code for Punaluʻu is 96717.

Geography

Punaluu is located at 21°35'33" North, 157°53'49" West (21.592600, -157.896989). According to the U.S. Census Bureau, the CDP has a total area of 2.1 square miles (5.4 km2), of which 1.6 square miles (4.1 km2) is land and 0.46 square miles (1.2 km2), or 22.97%, is water. The town is north of Kahana Bay and Kaʻaʻawa and south of Hauʻula along Kamehameha Highway (State Rte. 83). Kaluanui Stream and Sacred Falls are located between Punaluʻu and Hauʻula.

Demographics


As of the census of 2000, there were 881 people, 305 households, and 196 families residing in the CDP. The population densitywas 1,106.0 people per square mile (425.2/km²). There were 439 housing units at an average density of 551.1 per square mile (211.9/km²). The racial makeup of the CDP was 32.69% White, 0.57% Black or African American, 0.23% Native American, 10.22%Asian, 24.06% Pacific Islander, 0.23% from other races, and 32.01% from two or more races. 6.02% of the population wereHispanic or Latino of any race.

There were 305 households out of which 34.1% had children under the age of 18 living with them, 44.3% were married couplesliving together, 13.4% had a female householder with no husband present, and 35.7% were non-families. 29.8% of all households were made up of individuals and 5.2% had someone living alone who was 65 years of age or older. The average household size was 2.66 and the average family size was 3.32.

In the CDP the population was spread out with 26.0% under the age of 18, 8.7% from 18 to 24, 24.3% from 25 to 44, 25.0% from 45 to 64, and 16.0% who were 65 years of age or older. The median age was 38 years. For every 100 females there were 94.5 males. For every 100 females age 18 and over, there were 88.4 males.


The median income for a household in the CDP was $32,143, and the median income for a family was $32,500. Males have a median income of $32,188 versus $21,719 for females. The per capita income for the CDP was $19,067. About 15.8% of families and 19.9% of the population were below the poverty line, including 24.5% of those under the age of 18 and 0.8% of those ages 65 and older.

Sunday, June 12, 2016

Moraine Lake, Banff National Park, Alberta, Canada

Moraine Lake is a glacially-fed lake in Banff National Park, 14 kilometres (8.7 mi) outside the Village of Lake Louise, Alberta,Canada. It is situated in the Valley of the Ten Peaks, at an elevation of approximately 6,183 feet (1,885 m). The lake has a surface area of .5 square kilometres (0.19 sq mi).

The lake, being glacially fed, does not reach its crest until mid to late June. When it is full, it reflects a distinct shade of blue. The colour is due to the refraction of light off the rock flour deposited in the lake on a continual basis.

The area around the lake has several walking/hiking trails which are, from time to time, restricted. This is the one most commonly taken by tourists. The Rockpile Trail along the actual moraine is approximately 300 metres long, with an elevation change of 24 metres (79 ft). The view of the lake from the top of the rockpile is one of the most photographed locations in all of Canada.[1] That view of the mountains behind the lake in Valley of the Ten Peaks is known as the Twenty Dollar View, as Moraine Lake was featured on the reverse side of the 1969 and 1979 issues of theCanadian twenty dollar bill.
 
Along the same trailhead, the Consolation Lakes trail starts, which is approximately 3 kilometres (1.9 mi) long, with an elevation change of 90 metres (300 ft). Upon reaching Consolation Lakes hikers may continue along to the upper lake, which is not visible from the end of the lower lake. There is, however, no clearly marked trail, and can often be a scramble over large rocky areas.

Near the canoe docks of Moraine Lake Lodge there is another trailhead. This trailhead is the start of two trails, one of which branches out into four different trails - so there are in total, five trails starting at that trailhead (Moraine Lake Lakeshore Trail, Eiffel Lake, Wenkchemna Pass, Larch Valley, and Sentinel Pass). The Lake Louise & Yoho Map provides information on these trails.

 

Mountaineering routes

The Neil Colgan Hut can be reached in 8 to 12 hours climbing the Perren Route from Moraine Lake.