Skip to main content

Antelope Canyon, Arizon USA

Antelope Canyon is a slot canyon in the American Southwest, on Navajo land east of Page, Arizona. It includes two separate, scenic slot canyon sections, referred to as Upper Antelope Canyon (or The Crack), and Lower Antelope Canyon (or The Corkscrew).

The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means 'the place where water runs through rocks'. Lower Antelope Canyon is Hazdistazí (called "Hasdestwazi" by the Navajo Parks and Recreation Department), or 'spiral rock arches'. 

Antelope Canyon lights and rocks Arizona USA © Andrea Izzotti/Shutterstock

Antelope Canyon’s undulating sandstone walls have been smoothed and polished to perfection by years of rainwater and flooding. The slot canyon is still prone to flash floods on occasion, but visit on a fair weather day and you’ll be in for a treat, as the walls turn burning shades of amber, bronze and gold in the shafts of sunlight that peek through from above.

Geology

Antelope Canyon was formed by the erosion of Navajo Sandstone due to flash flooding and other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways eroded away, deepening the corridors and smoothing hard edges to form characteristic "flowing" shapes.

Upper Antelope Canyon

Upper Antelope Canyon is called Tsé bighánílíní, 'the place where water runs through rocks' by the Navajo. It's entrance and entire length are at ground level, requiring no climbing; and because beams of direct sunlight radiating down from openings at the top of the canyon are much more common. Light beams start to peek into the canyon March 20 and disappear by October 7.

Lower Antelope Canyon

Lower Antelope Canyon, called Hazdistazí, or 'spiral rock arches' by the Navajo, is located several miles from Upper Antelope Canyon. 

It is longer, narrower in places, and even footing is not available in all areas. Five flights of stairs of varying widths are currently available to aid in descent and ascent. At the end, the climb out requires flights of stairs. Additionally, sand continually falls from the crack above and can make the stairs slippery.

The lower canyon is in the shape of a "V" and shallower than the Upper Antelope. Lighting is better in the early hours and late morning.


Note: Taken help from google and image credit is given.

For any copyright issues mail us at: geologylearn123@gmail.com


Comments

Popular posts from this blog

HOW TO MAKE A GEOLOGICAL REPORT?

What is a GEOLOGICAL REPORT? Geological reports are concise, informative and well documented reports used to present, analyse and summarise field data for both industry and research purposes. They should be accompanied by geological maps, figures, stratigraphic columns, tables, graphs etc. PREPARATION First plan the layout, section by section; then draft each section using all your notes, maps, laboratory results and references gathered from other sources. Then list the illustrations needed to support the text. Finally, lay sections out in your choosen order, before gathering them together to edit  them. Does not spare the paper, allow plenty of room between the lines and at the margins for corrections, alterations and additions. REVISION AND EDITING First, a rough draft gets the essential facts and information in order. The next stage is to revise it and re-edit. The order of some paragraphs may need changing, spelling mistakes corrected, grammar improved. Indicate where illustratio

Stishovite

Origin Of Name Named after S.M. Stishov, an early investigator of high-pressure Silicon dioxide polymorphs     Copyright: Geology.today Stishovite, a rare, high-pressure polymorphs of Silicon dioxide, is known only from meteor impact craters Physical Properties . Hardness- 7 to 8 . Specific Gravity- 4.30 . Clevage- (110) . Fracture- Conchoidal . Luster- Vitreous . Transparency- Transparent to translucent . Colour- Colourless . Streak- White Crystal System- Tetragonal

The 10 Most Toxic Minerals

1. Cinnabar- Cinnabar is the main ore of mercury, the most toxic mineral on Earth. The name itself means dragons bloods. Form near volcanoes and sulphur deposits, the bright red colour signals danger.                    Copyright: Courtesy of Ted Boente; John H. Gerard/Encyclopedia Brittanica, Inc.  2. Orpiment- Originate from Latin auri , " golden "; pigmentum , " paint ". Composed of Arsenic Sulfide, the lethal and chemically reactive orpiment crystals are found growing below the surface in mineral formations, often near hydrothermal veins. It may crumble into dangerous powder when exposed to light. Holding crystals in your hands may release carcinogenic , neurotoxic powder.   Copyright:   U.S. Geological Survey 3. Stibnite- Antimony Sulphide, the principle ore of antimony. It is used in manufacturing of  matches and fireworks. Mines near Oksaku, Japan produce the best stibnite crystals in the world.