Bryce Canyon National Park, Utah, USA in 4K Ultra HD
The stunning, out-of-this-world beauty of Bryce Canyon National Park, seen from the main trails and viewpoints in the park.
In this video: Sunrise Point (0:06), Sunset Point (0:15, 6:25), Navajo trail (0:31), Queens Garden trail (3:01), Peek-a-Boo trail (3:51), Inspiration Point (6:43), Mossy Cave trail (7:11), Fairyland Trail (7:24), Tower Bridge (8:53), Natural Bridge (9:11).
Recorded September 2016 in 4K Ultra HD with Sony AX100.
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Kirsty Hawkshaw - The Ice Castle - 01-Ice Castle; 06-Parallax
Licensed via ilicensemusic.com
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Bryce Canyon National Park - Sunrise to Sunset Point hike through Hoodoos
The Navajo Loop Trail descends from Sunset Point through the slot canyon of Wall Street, where 500 to 700-year-old Douglas Firs reach upward toward the sunlight at the top of the canyon. The Navajo Loop is the most popular trail in the park, and is often combined with the Queen's Garden Trail to form a longer loop that passes through the Queen's Garden and emerges onto the rim at Sunrise Point. From here two very scenic and easy strolls can be taken as part of the Rim Trail. A ½-mile walk to the north on a wheelchair accessible trail which takes you to Sunset Point. Walking ¾ of a mile to the south across gently rolling terrain, you arrive at Inspiration Point.
My exact route:
Start at Sunset Point - known as Queens Garden Trail
Quick stop at Queen Victoria
Continue Queens Garden Trail to Peeakaboo Loop.
Hike Peekaboo Loop counter clockwise
Head up Navajo Loop (known as all street.
Finish up at Sunset Point.
Bryce Canyon National Park (TRAVEL GUIDE) | Beautiful America Series | Episode# 4
Bryce Canyon National Park travel guide in this beautiful America series by Hipfig for visitors to U.S. National Park.
This Bryce Canyon National Park travel guide covers – Main Entrance to Bryce Canyon park on UT-63 HWY, Red Canyon hoodoos on UT-12 Hwy, Bryce Canyon City (also called as Bryce), Bryce Canyon National Park Entrance Fee and Shuttles, Bryce Canyon visitor center, major Bryce Canyon points (like Inspiration point and Sunset Point Hoodoos) to see or hike and much more useful information for people planning visit to this Bryce Canyon Park.
Bryce Canyon National Park is in the southwestern region in the state of Utah on UT HWY 63 near the town of Bryce, UT and is famous for its hoodoos.
Topics covered in detail in this Bryce Canyon National Park travel guide video are below:
1). Introduction to Bryce Canyon National Park to new visitors interested in visiting National parks and famous natural wonders in North America,
2). Information on how to get to Bryce Canyon National Park visitor center by Car or Bryce Canyon Shuttle bus from Bryce (Utah) and information on Red Canyon hoodoos on UT-12 Hwy on the way to Bryce from UT-89 HWY,
3). Detailed information on Bryce Canyon National Park area – like Entrance on HWY UT-63, Shuttle from Bryce, Entrance tickets in Bryce at historic Ruby’s inn, Bryce Canyon National Park visitor Center, major points to visit in Bryce Canyon Park like Sunset Point, Inspiration Point, Bryce Point, Rainbow point etc.
4). Things to see and do at this Bryce Canyon National Park like visit to Bryce Canyon visitor center, Famous points like Rainbow point, Agua Canyon, Natural Bridge, Farview Point, Inspiration Point Hoodoos, Bryce Point amphitheater, Sunset point Silent City, Navajo loop trail, Rim trail etc.
5). After visit to Bryce Canyon National Park, visit and information on Grand Staircase-Escalante National Monument along UT HWY 12,
6). Travel tips for first time visitors visiting Bryce Canyon National Park in Utah.
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Bryce Canyon City, Utah
Bryce Canyon City, Utah. Drive Thru video heading towards Bryce Canyon National Park (South Bound) and a 2nd segment North Bound.
Bryce Canyon National Park - Utah - United States
Bryce Canyon National Park is a national park located in southwestern Utah in the United States. The major feature of the park is Bryce Canyon which, despite its name, is not a canyon but a giant natural amphitheater created by erosion along the eastern side of the Paunsaugunt Plateau. Bryce is distinctive due to geological structures called hoodoos, formed by wind, water, and ice erosion of the river and lake bed sedimentary rocks. The red, orange, and white colors of the rocks provide spectacular views for park visitors. Bryce sits at a much higher elevation than nearby Zion National Park. The rim at Bryce varies from 8,000 to 9,000 feet (2,400 to 2,700 m).
The Bryce area was settled by Mormon pioneers in the 1850s and was named after Ebenezer Bryce, who homesteaded in the area in 1874. The area around Bryce Canyon became a U.S. National Monument in 1923 and was designated as a national park in 1928. The park covers 35,835 acres (55.99 sq mi; 145.02 km2) and receives relatively few visitors compared to Zion National Park and the Grand Canyon, largely due to its remote location. The town of Kanab, Utah, is situated at a central point between these three parks. ( source Wikipedia )
The 'hoodoos' of Bryce Canyon National Park
The 'hoodoos' of Bryce Canyon National Park
USA Utah der wunderschöne Bryce Canyon Nationalpark Thors Hammer Bryce Point Hoodoos
didiaurich Bryce-Canyon-Nationalpark Utahs Vereinigten Staaten beautiful Bryce Canyon National Park hermoso Parque Nacional Bryce Canyon Bryce Point
The beautiful Bryce Canyon National Park is located in southwestern Utah in the United States
El hermoso Parque Nacional Bryce Canyon está situado en el suroeste de Utah en los Estados Unidos
Bryce Canyon National Park - Sunset Visit
Recorded June 2, 2010.
Video covers my visits to Inspiration Point, Bryce Point, Paria View and Sunset Point as the sun was setting in Utah's Bryce Canyon National Park.
Watch my complete video of this 2010 western roadtrip @
From:
Bryce Canyon, Bryce Canyon National Park, Utah, United States, North America
Bryce Canyon National Park is a national park located in southwestern Utah in the United States. The major feature of the park is Bryce Canyon which, despite its name, is not a canyon but a collection of giant natural amphitheaters along the eastern side of the Paunsaugunt Plateau. Bryce is distinctive due to geological structures called hoodoos, formed by frost weathering and stream erosion of the river and lake bed sedimentary rocks. The red, orange, and white colors of the rocks provide spectacular views for park visitors. Bryce sits at a much higher elevation than nearby Zion National Park. The rim at Bryce varies from 8,000 to 9,000 feet (2,400 to 2,700 m). The Bryce Canyon area was settled by Mormon pioneers in the 1850s and was named after Ebenezer Bryce, who homesteaded in the area in 1874. The area around Bryce Canyon became a U.S. National Monument in 1923 and was designated as a national park in 1928. The park covers 35,835 acres (55.99 sq mi; 145.02 km2) and receives relatively few visitors compared to Zion National Park and the Grand Canyon, largely due to its remote location. Bryce Canyon National Park is located in southwestern Utah about 50 miles (80 km) northeast of and 1,000 feet (300 m) higher than Zion National Park. The weather in Bryce Canyon is therefore cooler, and the park receives more precipitation: a total of 15 to 18 inches (38 to 46 cm) per year. Yearly temperatures vary from an average minimum of 9 °F (−13 °C) in January to an average maximum of 83 °F (28 °C) in July, but extreme temperatures can range from −30 °F to 97 °F (−34 °C to 36 °C). The record high temperature in the park was 98 °F (37 °C) on July 14, 2002. The record low temperature was −28 °F (−33 °C) on December 10, 1972. The national park lies within the Colorado Plateau geographic province of North America and straddles the southeastern edge of the Paunsagunt Plateau west of the Paunsagunt Fault. Park visitors arrive from the plateau part of the park and look over the plateau's edge toward a valley containing the fault and the Paria River just beyond it. The edge of the Kaiparowits Plateau bounds the opposite side of the valley. Bryce Canyon was not formed from erosion initiated from a central stream, meaning it technically is not a canyon. Instead headward erosion has excavated large amphitheater-shaped features in the Cenozoic-aged rocks of the Paunsagunt Plateau. This erosion exposed delicate and colorful pinnacles called hoodoos that are up to 200 feet (61 m) high. A series of amphitheaters extends more than 20 miles (32 km) north-to-south within the park. The largest is Bryce Amphitheater, which is 12 miles (19 km) long, 3 miles (4.8 km) wide and 800 feet (240 m) deep. A nearby example of amphitheaters with hoodoos in the same formation but at a higher elevation, is in Cedar Breaks National Monument, which is 25 miles (40 km) to the west on the Markagunt Plateau. Rainbow Point, the highest part of the park at 9,105 feet (2,775 m), is at the end of the 18-mile (29 km) scenic drive. From there, Aquarius Plateau, Bryce Amphitheater, the Henry Mountains, the Vermilion Cliffs and the White Cliffs can be seen. Yellow Creek, where it exits the park in the north-east section, is the lowest part of the park at 6,620 feet (2,020 m). The Bryce Canyon area shows a record of deposition that spans from the last part of the Cretaceous period and the first half of the Cenozoic era. The ancient depositional environment of the region around what is now the park varied. The Dakota Sandstone and the Tropic Shale were deposited in the warm, shallow waters of the advancing and retreating Cretaceous Seaway (outcrops of these rocks are found just outside park borders). The colorful Claron Formation, from which the park's delicate hoodoos are carved, was laid down as sediments in a system of cool streams and lakes that existed from 63 to about 40 million years ago (from the Paleocene to the Eocene epochs). Different sediment types were laid down as the lakes deepened and became shallow and as the shoreline and river deltas migrated.
Several other formations were also created but were mostly eroded away following two major periods of uplift.
Bryce Canyon, Bryce Canyon National Park, Utah, United States, North America
Bryce Canyon National Park is a national park located in southwestern Utah in the United States. The major feature of the park is Bryce Canyon which, despite its name, is not a canyon but a collection of giant natural amphitheaters along the eastern side of the Paunsaugunt Plateau. Bryce is distinctive due to geological structures called hoodoos, formed by frost weathering and stream erosion of the river and lake bed sedimentary rocks. The red, orange, and white colors of the rocks provide spectacular views for park visitors. Bryce sits at a much higher elevation than nearby Zion National Park. The rim at Bryce varies from 8,000 to 9,000 feet (2,400 to 2,700 m). The Bryce Canyon area was settled by Mormon pioneers in the 1850s and was named after Ebenezer Bryce, who homesteaded in the area in 1874. The area around Bryce Canyon became a U.S. National Monument in 1923 and was designated as a national park in 1928. The park covers 35,835 acres (55.99 sq mi; 145.02 km2) and receives relatively few visitors compared to Zion National Park and the Grand Canyon, largely due to its remote location. Bryce Canyon National Park is located in southwestern Utah about 50 miles (80 km) northeast of and 1,000 feet (300 m) higher than Zion National Park. The weather in Bryce Canyon is therefore cooler, and the park receives more precipitation: a total of 15 to 18 inches (38 to 46 cm) per year. Yearly temperatures vary from an average minimum of 9 °F (−13 °C) in January to an average maximum of 83 °F (28 °C) in July, but extreme temperatures can range from −30 °F to 97 °F (−34 °C to 36 °C). The record high temperature in the park was 98 °F (37 °C) on July 14, 2002. The record low temperature was −28 °F (−33 °C) on December 10, 1972. The national park lies within the Colorado Plateau geographic province of North America and straddles the southeastern edge of the Paunsagunt Plateau west of the Paunsagunt Fault. Park visitors arrive from the plateau part of the park and look over the plateau's edge toward a valley containing the fault and the Paria River just beyond it. The edge of the Kaiparowits Plateau bounds the opposite side of the valley. Bryce Canyon was not formed from erosion initiated from a central stream, meaning it technically is not a canyon. Instead headward erosion has excavated large amphitheater-shaped features in the Cenozoic-aged rocks of the Paunsagunt Plateau. This erosion exposed delicate and colorful pinnacles called hoodoos that are up to 200 feet (61 m) high. A series of amphitheaters extends more than 20 miles (32 km) north-to-south within the park. The largest is Bryce Amphitheater, which is 12 miles (19 km) long, 3 miles (4.8 km) wide and 800 feet (240 m) deep. A nearby example of amphitheaters with hoodoos in the same formation but at a higher elevation, is in Cedar Breaks National Monument, which is 25 miles (40 km) to the west on the Markagunt Plateau. Rainbow Point, the highest part of the park at 9,105 feet (2,775 m), is at the end of the 18-mile (29 km) scenic drive. From there, Aquarius Plateau, Bryce Amphitheater, the Henry Mountains, the Vermilion Cliffs and the White Cliffs can be seen. Yellow Creek, where it exits the park in the north-east section, is the lowest part of the park at 6,620 feet (2,020 m). The Bryce Canyon area shows a record of deposition that spans from the last part of the Cretaceous period and the first half of the Cenozoic era. The ancient depositional environment of the region around what is now the park varied. The Dakota Sandstone and the Tropic Shale were deposited in the warm, shallow waters of the advancing and retreating Cretaceous Seaway (outcrops of these rocks are found just outside park borders). The colorful Claron Formation, from which the park's delicate hoodoos are carved, was laid down as sediments in a system of cool streams and lakes that existed from 63 to about 40 million years ago (from the Paleocene to the Eocene epochs). Different sediment types were laid down as the lakes deepened and became shallow and as the shoreline and river deltas migrated. Several other formations were also created but were mostly eroded away following two major periods of uplift.
Bryce Canyon, Bryce Canyon National Park, Utah, United States, North America
Bryce Canyon National Park is a national park located in southwestern Utah in the United States. The major feature of the park is Bryce Canyon which, despite its name, is not a canyon but a collection of giant natural amphitheaters along the eastern side of the Paunsaugunt Plateau. Bryce is distinctive due to geological structures called hoodoos, formed by frost weathering and stream erosion of the river and lake bed sedimentary rocks. The red, orange, and white colors of the rocks provide spectacular views for park visitors. Bryce sits at a much higher elevation than nearby Zion National Park. The rim at Bryce varies from 8,000 to 9,000 feet (2,400 to 2,700 m). The Bryce Canyon area was settled by Mormon pioneers in the 1850s and was named after Ebenezer Bryce, who homesteaded in the area in 1874. The area around Bryce Canyon became a U.S. National Monument in 1923 and was designated as a national park in 1928. The park covers 35,835 acres (55.99 sq mi; 145.02 km2) and receives relatively few visitors compared to Zion National Park and the Grand Canyon, largely due to its remote location. Bryce Canyon National Park is located in southwestern Utah about 50 miles (80 km) northeast of and 1,000 feet (300 m) higher than Zion National Park. The weather in Bryce Canyon is therefore cooler, and the park receives more precipitation: a total of 15 to 18 inches (38 to 46 cm) per year. Yearly temperatures vary from an average minimum of 9 °F (−13 °C) in January to an average maximum of 83 °F (28 °C) in July, but extreme temperatures can range from −30 °F to 97 °F (−34 °C to 36 °C). The record high temperature in the park was 98 °F (37 °C) on July 14, 2002. The record low temperature was −28 °F (−33 °C) on December 10, 1972. The national park lies within the Colorado Plateau geographic province of North America and straddles the southeastern edge of the Paunsagunt Plateau west of the Paunsagunt Fault. Park visitors arrive from the plateau part of the park and look over the plateau's edge toward a valley containing the fault and the Paria River just beyond it. The edge of the Kaiparowits Plateau bounds the opposite side of the valley. Bryce Canyon was not formed from erosion initiated from a central stream, meaning it technically is not a canyon. Instead headward erosion has excavated large amphitheater-shaped features in the Cenozoic-aged rocks of the Paunsagunt Plateau. This erosion exposed delicate and colorful pinnacles called hoodoos that are up to 200 feet (61 m) high. A series of amphitheaters extends more than 20 miles (32 km) north-to-south within the park. The largest is Bryce Amphitheater, which is 12 miles (19 km) long, 3 miles (4.8 km) wide and 800 feet (240 m) deep. A nearby example of amphitheaters with hoodoos in the same formation but at a higher elevation, is in Cedar Breaks National Monument, which is 25 miles (40 km) to the west on the Markagunt Plateau. Rainbow Point, the highest part of the park at 9,105 feet (2,775 m), is at the end of the 18-mile (29 km) scenic drive. From there, Aquarius Plateau, Bryce Amphitheater, the Henry Mountains, the Vermilion Cliffs and the White Cliffs can be seen. Yellow Creek, where it exits the park in the north-east section, is the lowest part of the park at 6,620 feet (2,020 m). The Bryce Canyon area shows a record of deposition that spans from the last part of the Cretaceous period and the first half of the Cenozoic era. The ancient depositional environment of the region around what is now the park varied. The Dakota Sandstone and the Tropic Shale were deposited in the warm, shallow waters of the advancing and retreating Cretaceous Seaway (outcrops of these rocks are found just outside park borders). The colorful Claron Formation, from which the park's delicate hoodoos are carved, was laid down as sediments in a system of cool streams and lakes that existed from 63 to about 40 million years ago (from the Paleocene to the Eocene epochs). Different sediment types were laid down as the lakes deepened and became shallow and as the shoreline and river deltas migrated. Several other formations were also created but were mostly eroded away following two major periods of uplift.
The Bryce Canyon National Park, Utah, United States.
One of the feature locations during my 2018 road trip and in a word, 'stunning'. I really, really recommend going and not as a secondary sight but a highlight.
Looking back I regret not planning enough time to walk down into the 'canyon' a bit to get up close with some of the features (this was partly a time-to-get-there issue but also bad luck as the weather was to say the least 'wet' over my 2 days in the area).
Bryce Canyon isn't technically a canyon but a series of amphitheatres along a ridge. This is nit-picking to say the least but if you see the view from Rainbow Point (3 mins 20 sec) you can see the various amphitheatres curling into the distance. Inspiration Point is spectacular! It is quite difficult to take it all in because the views from each stop have something different to marvel over. If you are in the area or even passing within 50 miles I highly recommend a visit.
If you're interested, the hoodoo features (tall pinnacles or columns) are the result of acidic rain slowly eroding the calcium carbonate rock. Initially the rain erodes down through fissures which sees the development of walls of rock. These walls gradually crumble (under further acid rain erosion) into arches and finally, when the arch thins and collapses, hoodoos.
Bryce Canyon National Park, Utah - Bryce Point HD (2013)
Bryce Canyon National Park is a national park located in southwestern Utah in the United States. The major feature of the park is Bryce Canyon, which despite its name, is not a canyon but a collection of giant natural amphitheaters along the eastern side of the Paunsaugunt Plateau. Bryce is distinctive due to geological structures called hoodoos, formed by frost weathering and stream erosion of the river and lake bed sedimentary rocks. The red, orange, and white colors of the rocks provide spectacular views for park visitors. Bryce sits at a much higher elevation than nearby Zion National Park. The rim at Bryce varies from 8,000 to 9,000 feet (2,400 to 2,700 m).
The Bryce Canyon area was settled by Mormon pioneers in the 1850s and was named after Ebenezer Bryce, who homesteaded in the area in 1874. The area around Bryce Canyon became a National Monument in 1923 and was designated as a National Park in 1928. The park covers 35,835 acres (55.99 sq mi; 145.02 km2) and receives relatively few visitors compared to Zion National Park and the Grand Canyon, largely due to its remote location.
Bryce Canyon National Park - 4K UHD Nature Documentary Film - 1 HR
A visit to Bryce Canyon National Park can be really overwhelming and full of wonders! Bryce Canyon offers the best American West's spectacular scenery that won’t leave anyone indifferent.
A new 4K Ultra HD amazing nature documentary film from and won’t leave you indifferent either.
Bryce canyon is known for magnificent limestone sculptures, for its’ river and water reservoirs, for its’ diversity of animals and plants. Many tourists consider Bryce Canyon even more beautiful and tourist friendly than Zion or Grand Canyon National Parks.
The best way to explore and take in the beauty and grandeur of Bryce Canyon is from numerous viewpoints that are found along an 18-mile scenic road. The famous road runs along the plateau rim offering magnificent views. Don’t forget about sunsets here, they are gorgeous in the area!
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Bryce point at Bryce Canyon National Park, Utah, USA
Bryce point at Bryce Canyon National Park, Utah, USA
Bryce canyon national park, Utah, United States 3
Bryce Canyon National Park, Utah, USA 1999
Another video Bryce canyon, part 1
Bryce Canyon National Park /ˈbraɪs/ is a National Park located in southwestern Utah in the United States. The major feature of the park is Bryce Canyon, which despite its name, is not a canyon, but a collection of giant natural amphitheaters along the eastern side of the Paunsaugunt Plateau. Bryce is distinctive due to geological structures called hoodoos, formed by frost weathering and stream erosion of the river and lake bed sedimentary rocks. The red, orange, and white colors of the rocks provide spectacular views for park visitors. Bryce sits at a much higher elevation than nearby Zion National Park. The rim at Bryce varies from 8,000 to 9,000 feet (2,400 to 2,700 m).
The Bryce Canyon area was settled by Mormon pioneers in the 1850s and was named after Ebenezer Bryce, who homesteaded in the area in 1874. The area around Bryce Canyon became a National Monument in 1923 and was designated as a National Park in 1928. The park covers 35,835 acres (55.992 sq mi; 14,502 ha; 145.02 km2) and receives relatively few visitors compared to Zion National Park and the Grand Canyon, largely due to its remote location.
Bryce Canyon National Park
Bryce Canyon National Park USA ① ✈ HD 1080p50
Bryce Canyon National Park - Utah, USA
Bryce Canyon National Park - Utah, USA
July 2012
Hiking Bryce Canyon National Park. Utah USA
Bryce Canyon National Park is an American national park located in southwestern Utah. The major feature of the park is Bryce Canyon, which despite its name, is not a canyon, but a collection of giant natural amphitheaters along the eastern side of the Paunsaugunt Plateau. Bryce is distinctive due to geological structures called hoodoos, formed by frost weathering and stream erosion of the river and lake bed sedimentary rocks. The red, orange, and white colors of the rocks provide spectacular views for park visitors. Bryce sits at a much higher elevation than nearby Zion National Park. The rim at Bryce varies from 8,000 to 9,000 feet
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Utah By Drone - Zion, Moab, Bryce Canyon, Devil's Garden & Arches National Park
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It's hard to believe some of the amazing places that exist in Utah! Red rock towers, amazing stone arches, mysterious desert canyons, and more.
Here are some places you might see in the video:
- Hurrah Pass (Moab, UT)
- Fisher Towers (Moab, UT)
- Corona Arch (Moab, UT)
- Delicate Arch (Moab, UT)
- Goosenecks State Park
- Devil's Garden (Boulder, UT)
- Dead Horse Canyon (Moab, UT)
- Kodachrome Basin State Park
- Red Canyon (Bryce, UT)
- Hell's Canyon (Kayenta, UT)
- Grosvenor Arch (Cannonville, UT)
- Zion National Park (Springdale, UT)
- Lower Calf Creek Falls (Boulder, UT)
- Devil's Golf Ball (Moab, UT)
- Mexican Hat Rock (Mexican Hat, UT)
- Bryce Canyon National Park
- Stewart Falls (Provo, UT)
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*** Any national/state parks or restricted areas in this video were filmed from outside the boundaries, flying in public airspace. As of the time of filming, this means no park rules were broken making this video (NPS has confirmed). ***