Kaimanawa Mountains & Kaimanawa wall in NZ

2024. 12. 30. 04:08Wonderful World

아직까지 풀리지 않는

뉴질랜드의 미스터리, 거석 유적

https://www.youtube.com/watch?v=L78qXIuHSxM

 

 

전통적인 역사관에 따르면 뉴질랜드는 인간이 정착한 지구상의 마지막 주요 대륙입니다.

 

태평양 남서부에 위치한 이 섬은 서기 1300년 경, 최초의 폴리네시아인 마오리족이 도착할 때까지 사람이 살지 않았습니다.

 

그러나 최근 뉴질랜드 북섬에서 놀라운 발견이 이뤄졌는데요. 이는 이 지역의 고대 역사에 대한 우리의 이해를 완전히 바꾸는 것이었습니다.

 

카이마나와 산맥의 빽빽한 초목 속에는 카이마나와 벽으로 알려진 거대한 거석 구조물이 자리잡고 있습니다.

이 벽은 돌들이 너무도 정밀하게 서로 맞춰져 형성되어 있기 때문에 그 기원에 대한 뜨거운 논쟁을 불러일으키고 있는데요.

이는 뉴질랜드의 선사 시대에 대한 우리의 이해에 커다란 도전을 하고 있습니다.

 

벽은 일련의 촘촘하게 박힌 돌들이 특징이며, 언뜻 보기에는 정밀하게 배치된 것처럼 보입니다.

 

 

 

Kaimanawa Mountains

Kaimanawa Range

Elevation 1,727 m (5,666 ft)

summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. The topographic terms acmeapexpeak (mountain peak), and zenith are synonymous.

Sunset_over_Kaimanawas

Kaimanawa Ranges in the Taupo District of New Zealand

 

The Kaimanawa Range, officially called the Kaimanawa Mountains since 16 July 2020, is a range of mountains in the central North Island of New Zealand.  They extend for 50 kilometres in a northeast–southwest direction through largely uninhabited country to the south of Lake Taupō, east of the "Desert Road". Their slopes form part of the North Island Volcanic Plateau.

 

The New Zealand Ministry for Culture and Heritage gives a translation of "breath for food" for Kaimanawa.

 

The lands around the mountains are scrubby. To the west, where the Rangipo Desert is located, the soils are poor quality. To the east, the soils are more fertile, but the land is very rough. A population of feral horses, the Kaimanawa horses, roam free on the ranges.

 

Unlike the majority of mountain ranges in New Zealand, the Kaimanawa Range is divided into private land. Considerable areas of the Rangipo Desert are used by the New Zealand Army for training.

 

 

Wilderness  Kaimanawa – Heart of the North Island

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    Looking south from Thunderbolt (1638m) along Middle Range with Makomiko Stream and Rangitikei REZ to left.

Looking from Middle Range across upper Rangitikei to Makorako (1727m) at the north-eastern edge of the Rangitikei Remote Experience Zone. 

 

Mount Urchin Track

 

Urchin Campsite to Pillars of Hercules

 

Pillars of Hercule

 

Oamaru Hut via Taharua Road

 

Te Iringa Track to Tiki Tiki Stream

 

Kaimanawa Forest Loop Walk

 

Mount Urchin Track

 

Oamaru Hut to Boyd Hut Track

 

Clements Road End Campsite Waterfall Walk

 

Te Iringa Track to Tiki Tiki Stream

 

Mt Urchin. Kaimanawa Forest Park

 

 

 Kaimanawa Horses

Kaimanawa Heritage Horses 

 

 

Access to Needle Block, Kaimanawa Mountains

 

 

 

Kaimanawa wall

The Kaimanawa wall. A Rock formation on Clements Mill Road in Kaimanawa Forest Park, New Zealand. It has distinctive straight edges.

 

 

The Kaimanawa Wall is a geological feature in the Kaimanawa State Forest.  The Tuwharetoa tangata whenua claim an “oral tradition” of the place as a kōhatu (rock).  A popular theory is that the wall is a pre-Māori civilization artifact.

 

The wall formation was inspected by an archaeologist and a geologist; neither saw evidence of a human origin. In a preliminary investigation, archaeologist Neville Ritchie of the New Zealand Department of Conservation observed "matching micro-irregularities along the joints." This indicated that the blocks in the wall were too perfectly matched. He also observed the joints were neither straight nor truly horizontal nor perpendicular, indicating the joint alignments were too poorly constructed. Ritchie concluded the blocks are a natural formation based on the presence of matching micro-irregularities in blocks and imperfect joint alignment.

 

Peter Wood, a geologist of the Institute of Geological and Nuclear Sciences at Wairakei, inspected the blocks for an afternoon and concluded they are natural fractures in "jointed Rangitaiki ignimbrite, a 330,000 year old volcanic rock that is common in the Taupō Volcanic Zone."  Both vertical and horizontal joints are common.

 

Fractures in the Rangitaiki ignimbrite formed when it cooled and contracted after flowing into place during an eruption.