Gardiner, Montana and Roosevelt Arch North Entrance of Yellowstone National Park
The town of Gardiner, Montana is nestled at the southern end of Paradise valley and directly at the North Entrance of Yellowstone National Park. Gardiner is a quaint western town that offers a small variety of restaurants, lodging options, and shops.
As we travel along Old Yellowstone Trail road we see many animals including Elk, and antelope. We visit the Roosevelt Arch at the North entrance of Yellowstone National Park.
We also Vist the Iron Horse Bar and Grille in Gardiner for dinner. We try the Bison burger and the ribs. We had a great time in this beautiful town and highly recommend anyone who is thinking about visiting.
Road Trip USA Wyoming, Yellowstone National Park Part 3
Road Trip USA Wyoming, Yellowstone National Park Part 3
Nothing but road scenery over 25,000 + miles of road trip.
Vehicle: RV + Motorcycle.
Camera: Android Nexus 4
Android App: Dashboard Cam by busywww, Google Map
GPS Overlay App: Images From Video (Overlay) by busywww
Video Edit: Corel Video Studio
Yellowstone NP in winter ~ Gardiner, MT to Mammoth Hot Springs (2-15-14)
This is a winter drive from the gateway town of Gardiner, Montana into the North Entrance to Yellowstone National Park (the first U.S. National Park, established in 1872). Only the North and Northeast entrances are kept open in winter (and the 52 miles between them, across the Lamar Valley). From Mammoth, the road to Norris closes at the Upper Terrace in the winter. The Mammoth area is a wintering ground for some of the park's bison and elk, which means wolves can sometimes be seen here.
Music = Cusco: Mexica (album: Apurimac II)
Yellowstone National Park: Grizzlies, Bison, Old Faithful, and More
Footage from my trip to Yellowstone National Park during summer 2019.
Locations
0:00 Hayden Valley
0:08 Mammoth area
0:36 Mammoth Falls
1:10 Gardiner, Montana
1:17 Lamar Valley
2:17 Yellowstone River
2:25 Mount Washburn Summit
2:46 Lower Falls
3:18 Norris Geyser Basin
4:33 Mammoth, Wyoming
4:43 Precise location N/A (along Highway 89/191)
4:50 Old Faithful
5:24 Historic Old Faithful Inn
5:45 Grand Prismatic Spring
5:56 West Yellowstone, Montana
6:06 Precise location N/A (along Highway 89/191)
7:01 Hayden Valley
11:47 Gardiner, Montana
12:23 Petrified Tree & surrounding area
12:38 Mud Volcano area
13:04 Yellowstone Lake area
13:32 Yellowstone Lake
Music
Campfire Song by Chris Haugen
Firefly by Chris Haugen
Tumbleweed Texas by Chris Haugen
Roundup on the Prairie by Aaron Kenny
Horses to Water by Topher Mohr and Alex Elena
Tupelo Train by Chris Haugen
Yellowstone National Park, Sylvan Pass & East Entrance Road.
Film of our entry into Yellowstone National Park from the East Entrance. This was the end of June 2011 but there was still plenty of snow on the Sylvan Pass and Sylvan Lake was still partially frozen. The winter of 2010/11 brought above average snowfall.
Yellowstone National Park Vacation Travel Guide | Expedia
Yellowstone National Park showcases the splendor of North American wilderness from its mountains to its valleys and its streams in between. You won’t want to miss this!
Check out all the places we visited in this video:
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#Yellowstone has long remained in the American imagination as a land little touched by humanity. From the steaming power of erupting geysers, to the thundering might of the Yellowstone River, this magnificent landscape is testament to the power and beauty of Mother Nature.
When European explorers first ventured into these enchanting lands, they returned with stories which most people dismissed as hallucinations. Since then, it has become one of America’s ultimate #adventure #vacation destinations and provides a home for the largest remaining herd of wild bison on the planet. Welcome to Yellowstone, the grandfather of all national parks.
We hope you enjoy watching this #travel #guide as much as we enjoyed making it.
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Canary Spring, Mammoth Hot Spring, Yellowstone National Park, Wyoming, United States, North America
Mammoth Hot Springs is a large complex of hot springs on a hill of travertine in Yellowstone National Park adjacent to Fort Yellowstone and the Mammoth Hot Springs Historic District. It was created over thousands of years as hot water from the spring cooled and deposited calcium carbonate. Although these springs lie outside the caldera boundary, their energy has been attributed to the same magmatic system that fuels other Yellowstone geothermal areas. Dead trees in an area of intense deposition of calcium carbonate. The hot water that feeds Mammoth comes from Norris Geyser Basin after traveling underground via a fault line that runs through limestone and roughly parallel to the Norris-to-Mammoth road. The limestone from rock formations along the fault is the source of the calcium carbonate. Shallow circulation along this corridor allows Norris' superheated water to slightly cool before surfacing at Mammoth, generally at about 170 °F (80 °C). Algae living in the warm pools have tinted the travertine shades of brown, orange, red, and green. Thermal activity here is extensive both over time and distance. The thermal flows show much variability with some variations taking place over periods ranging from decades to days. Terrace Mountain at Mammoth Hot Springs is the largest known carbonate-depositing spring in the world. The most famous feature at the springs is the Minerva Terrace, a series of travertine terraces. The terraces have been deposited by the spring over many years but, due to recent minor earthquake activity, the spring vent has shifted, rendering the terraces dry. The Mammoth Terraces extend all the way from the hillside, across the Parade Ground, and down to Boiling River. The Mammoth Hotel, as well as all of Fort Yellowstone, is built upon an old terrace formation known as Hotel Terrace. There was some concern when construction began in 1891 on the fort site that the hollow ground would not support the weight of the buildings. Several large sink holes (fenced off) can be seen out on the Parade Ground. This area has been thermally active for several thousand years. The Mammoth area exhibits much evidence of glacial activity from the Pinedale Glaciation. The summit of Terrace Mountain is covered with glacial till, thereby dating the travertine formation there to earlier than the end of the Pinedale Glaciation. Several thermal kames, including Capitol Hill and Dude Hill, are major features of the Mammoth Village area. Ice-marginal stream beds are in evidence in the small, narrow valleys where Floating Island Lake and Phantom Lake are found. In Gardner Canyon one can see the old, sorted gravel bed of the Gardner River covered by unsorted glacial till. The geothermal areas of Yellowstone include several geyser basins in Yellowstone National Park as well as other geothermal features such as hot springs, mud pots, and fumaroles. The number of thermal features in Yellowstone is estimated at 10,000. A study that was completed in 2011 found that a total of 1283 geysers have erupted in Yellowstone, 465 of which are active during an average year. These are distributed among nine geyser basins, with a few geysers found in smaller thermal areas throughout the Park. The number of geysers in each geyser basin are as follows: Upper Geyser Basin (410), Midway Geyser Basin (59), Lower Geyser Basin (283), Norris Geyser Basin (193), West Thumb Geyser Basin (84), Gibbon Geyser Basin (24), Lone Star Geyser Basin (21), Shoshone Geyser Basin (107), Heart Lake Geyser Basin (69), other areas (33). Although famous large geysers like Old Faithful are part of the total, most of Yellowstone's geysers are small, erupting to only a foot or two. The hydrothermal system that supplies the geysers with hot water sits within an ancient active caldera. Many of the thermal features in Yellowstone build up sinter, geyserite, or travertine deposits around and within them. The various geyser basins are located where rainwater and snowmelt can percolate into the ground, get indirectly superheated by the underlying Yellowstone hotspot, and then erupt at the surface as geysers, hot springs, and fumaroles. Thus flat-bottomed valleys between ancient lava flows and glacial moraines are where most of the large geothermal areas are located. Smaller geothermal areas can be found where fault lines reach the surface, in places along the circular fracture zone around the caldera, and at the base of slopes that collect excess groundwater.
Drive from Gardiner, MT to Eagle Creek Campground
OLD FAITHFUL & Mammoth Hot Springs | Yellowstone National Park & Red Lodge, Montana Roadtrip
Visit Red Lodge! It is a beautiful town, right on the way to Beartooth pass in Yellowstone National Park, in Montana.
My mother, Carla, and I are road tripping through beautiful Montana. We stayed for a night in Red Lodge, since we heard it is so picturesque and beautiful.
When we woke up at the Lupine Inn, we drank some free hotel coffee, and had a quick swim in the pool. Hungry for food, we then went for lunch at Bogart's Restaurant downtown. We ordered fried pickles, jalapeno poppers and Mexican enchiladas. The food is extremely delicious here, and good value.
After lunch, we decided to work off some calories, so we walked the whole length of the main street of Red Lodge.
We were anxious to see animals. Yellowstone Wildlife Sanctuary, all rescued animals who need care, is also in downtown Red Lodge and welcomes guests to see their bears, foxes and other animals. Community funded, the animals here are deemed unable to survive in the wild. They try to provide the best life for the animals. There are many signs to be quiet, so as not to scare the animals.
Before traveling out of town to drive up Beartooth Pass Highway, we first stopped at the old train station, where the art takes over the indoors, from floor to ceiling. Admission is all free, but the art is for sale.
It was our time to target on the road to Yellowstone, by way of Beartooth Pass. We headed into the mountains to Beartooth Highway Pass, up to the state line where Montana meets Wyoming. Unfortunately, there was too much ice and snow on the roads to continue -- the road was closed off for the rest of the winter already.
We had no other choice but to drive up to the North gate at Gardiner, Montana, entrance to Yellowstone to enter. Along the way, we saw moose and deer along the road. Once we entered Yellowstone National Park, we enjoyed the sighs of Mammoth hot springs and Old Faithful Geyser.
We left Yellowstone from the south gate entrance at Wyoming, that goes through the Grand Teton Park. The sunsets were incredible in the wide open Montana and Wyoning skies.
Where we ate:
Bogart's Restaurant
11 Broadway Ave S, Red Lodge, MT 59068
(406) 446-1784
Where we saw the animals:
Yellowstone Wildlife Sanctuary
615 2nd St E, Red Lodge, MT 59068
(406) 446-1133
Where to go see art:
Carbon County Arts Guild & Depot Gallery
11 8th St W, Red Lodge, MT 59068
(406) 446-1370
Where we slept (cheapest in town):
Lupine Inn Red Lodge
702 Hauser Ave S, Red Lodge, MT 59068
(406) 445-3301
Bellagio Hotel and Casino in Las Vegas is better, but if you want to see the geyser (joking):
Old Faithful
Yellowstone National Park, WY 82190
(307) 344-7381
Music used in this video:
Emma Jensen - Closer
Marilyn Manson cover song - We Are The Nobodies
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This video is co-produced by Carla Marie Rupp.
Thank you! ❤
Jason Rupp
Mammoth Hot Springs, Yellowstone National Park, Wyoming/Montana/Idaho, United States, North America
Mammoth Hot Springs is a large complex of hot springs on a hill of travertine in Yellowstone National Park adjacent to Fort Yellowstone and the Mammoth Hot Springs Historic District. It was created over thousands of years as hot water from the spring cooled and deposited calcium carbonate. Because of the huge amount of geothermal vents, travertine flourishes. Although these springs lie outside the caldera boundary, their energy has been attributed to the same magmatic system that fuels other Yellowstone geothermal areas. The hot water that feeds Mammoth comes from Norris Geyser Basin after traveling underground via a fault line that runs through limestone and roughly parallel to the Norris-to-Mammoth road. The limestone from rock formations along the fault is the source of the calcium carbonate. Shallow circulation along this corridor allows Norris' superheated water to slightly cool before surfacing at Mammoth, generally at about 170 °F (80 °C). Algae living in the warm pools have tinted the travertine shades of brown, orange, red, and green. Thermal activity here is extensive both over time and distance. The thermal flows show much variability with some variations taking place over periods ranging from decades to days. Terrace Mountain at Mammoth Hot Springs is the largest known carbonate-depositing spring in the world. The most famous feature at the springs is the Minerva Terrace, a series of travertine terraces. The terraces have been deposited by the spring over many years but, due to recent minor earthquake activity, the spring vent has shifted, rendering the terraces dry. The Mammoth Terraces extend all the way from the hillside, across the Parade Ground, and down to Boiling River. The Mammoth Hotel, as well as all of Fort Yellowstone, is built upon an old terrace formation known as Hotel Terrace. There was some concern when construction began in 1891 on the fort site that the hollow ground would not support the weight of the buildings. Several large sink holes can be seen out on the Parade Ground. This area has been thermally active for several thousand years. The Mammoth area exhibits much evidence of glacial activity from the Pinedale Glaciation. The summit of Terrace Mountain is covered with glacial till, thereby dating the travertine formation there to earlier than the end of the Pinedale Glaciation. Several thermal kames, including Capitol Hill and Dude Hill, are major features of the Mammoth Village area. Ice-marginal stream beds are in evidence in the small, narrow valleys where Floating Island Lake and Phantom Lake are found. In Gardner Canyon one can see the old, sorted gravel bed of the Gardner River covered by unsorted glacial till.
Canary Spring, Mammoth Hot Spring, Yellowstone National Park, Wyoming, United States, North America
Mammoth Hot Springs is a large complex of hot springs on a hill of travertine in Yellowstone National Park adjacent to Fort Yellowstone and the Mammoth Hot Springs Historic District. It was created over thousands of years as hot water from the spring cooled and deposited calcium carbonate. Although these springs lie outside the caldera boundary, their energy has been attributed to the same magmatic system that fuels other Yellowstone geothermal areas. Dead trees in an area of intense deposition of calcium carbonate. The hot water that feeds Mammoth comes from Norris Geyser Basin after traveling underground via a fault line that runs through limestone and roughly parallel to the Norris-to-Mammoth road. The limestone from rock formations along the fault is the source of the calcium carbonate. Shallow circulation along this corridor allows Norris' superheated water to slightly cool before surfacing at Mammoth, generally at about 170 °F (80 °C). Algae living in the warm pools have tinted the travertine shades of brown, orange, red, and green. Thermal activity here is extensive both over time and distance. The thermal flows show much variability with some variations taking place over periods ranging from decades to days. Terrace Mountain at Mammoth Hot Springs is the largest known carbonate-depositing spring in the world. The most famous feature at the springs is the Minerva Terrace, a series of travertine terraces. The terraces have been deposited by the spring over many years but, due to recent minor earthquake activity, the spring vent has shifted, rendering the terraces dry. The Mammoth Terraces extend all the way from the hillside, across the Parade Ground, and down to Boiling River. The Mammoth Hotel, as well as all of Fort Yellowstone, is built upon an old terrace formation known as Hotel Terrace. There was some concern when construction began in 1891 on the fort site that the hollow ground would not support the weight of the buildings. Several large sink holes (fenced off) can be seen out on the Parade Ground. This area has been thermally active for several thousand years. The Mammoth area exhibits much evidence of glacial activity from the Pinedale Glaciation. The summit of Terrace Mountain is covered with glacial till, thereby dating the travertine formation there to earlier than the end of the Pinedale Glaciation. Several thermal kames, including Capitol Hill and Dude Hill, are major features of the Mammoth Village area. Ice-marginal stream beds are in evidence in the small, narrow valleys where Floating Island Lake and Phantom Lake are found. In Gardner Canyon one can see the old, sorted gravel bed of the Gardner River covered by unsorted glacial till. The geothermal areas of Yellowstone include several geyser basins in Yellowstone National Park as well as other geothermal features such as hot springs, mud pots, and fumaroles. The number of thermal features in Yellowstone is estimated at 10,000. A study that was completed in 2011 found that a total of 1283 geysers have erupted in Yellowstone, 465 of which are active during an average year. These are distributed among nine geyser basins, with a few geysers found in smaller thermal areas throughout the Park. The number of geysers in each geyser basin are as follows: Upper Geyser Basin (410), Midway Geyser Basin (59), Lower Geyser Basin (283), Norris Geyser Basin (193), West Thumb Geyser Basin (84), Gibbon Geyser Basin (24), Lone Star Geyser Basin (21), Shoshone Geyser Basin (107), Heart Lake Geyser Basin (69), other areas (33). Although famous large geysers like Old Faithful are part of the total, most of Yellowstone's geysers are small, erupting to only a foot or two. The hydrothermal system that supplies the geysers with hot water sits within an ancient active caldera. Many of the thermal features in Yellowstone build up sinter, geyserite, or travertine deposits around and within them. The various geyser basins are located where rainwater and snowmelt can percolate into the ground, get indirectly superheated by the underlying Yellowstone hotspot, and then erupt at the surface as geysers, hot springs, and fumaroles. Thus flat-bottomed valleys between ancient lava flows and glacial moraines are where most of the large geothermal areas are located. Smaller geothermal areas can be found where fault lines reach the surface, in places along the circular fracture zone around the caldera, and at the base of slopes that collect excess groundwater.
Yellowstone Road Trip (1/3): Idaho, Montana, & Hot Springs
A trip in and around Yellowstone National Park viewing some hot springs, waterfalls in Idaho, and caves and towns in Montana.
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I have always wanted to see Yellowstone National Park for myself ever since I was a seven year old boy. Fortunately, I had three others with me who desired to see the park and it's surrounding areas with me. We set off for Idaho Falls and shortly after taking off with our rental we reached our first stop at Targhee National Forest in southeastern Idaho to see upper and lower Mesa Falls.
From there we crossed the Idaho Montana border and entered into West Yellowstone where we stayed, at Wyndham Worldmark. Next day was a fairly cloudy and snowy day limiting our travel plans to almost none. Fortunately we got a taste of winter in the park checking out some Hot Springs. First stop was the Painting Pot Nature Trail, then The Midway Geyser Basin for the Grand Prismatic hot spring and several geysers. Snow eventually came in real hard and we eventually headed back to town for dinner and some local beer.
Third day, we did a large loop around southwest Montana passing through Hebgen Lake and Earthquake Lake. Passing through Ennis and up to the Lewis and Clark Caverns where we took a two hour tour through some beautiful caves. From there we drove through the large towns of Bozeman and Livingston before heading back south through the Roosevelt Arch in Gardiner to Mammoth for some more Hot Springs and back to our place of stay.
Footage captured with with an iPhone 4s and GoPro3
Compiled with Final Cut Pro
Music Credit goes to the artists but more so to these talented individuals:
-Phillip Phillips - Home (Cover by Hartley Road ft. Ashley Serena)
-Buck Norris - She'll Be Comin Round The Mountain
-Buffalo Springfield - For What It's Worth (Guitar Cover)
-Willie Nelson - On the Road again (Country Cover by Karen Muenchen)
-Gene Quaw - Going Home to Montana
-Miranda Lambert - House That Built Me (cover by Hannah Mulholland)
Yellowstone National Park de Gardiner à West Yellowstone # 2
Yellowstone National Park road trip de Gardiner à West Yellowstone
Grand Prismatic spring - Geyser old Faithful et de nombreuses merveilles de la nature.
Main Terrace, Mammoth Hot Spring, Yellowstone National Park, Wyoming, United States, North America
Mammoth Hot Springs is a large complex of hot springs on a hill of travertine in Yellowstone National Park adjacent to Fort Yellowstone and the Mammoth Hot Springs Historic District. It was created over thousands of years as hot water from the spring cooled and deposited calcium carbonate. Although these springs lie outside the caldera boundary, their energy has been attributed to the same magmatic system that fuels other Yellowstone geothermal areas. Dead trees in an area of intense deposition of calcium carbonate. The hot water that feeds Mammoth comes from Norris Geyser Basin after traveling underground via a fault line that runs through limestone and roughly parallel to the Norris-to-Mammoth road. The limestone from rock formations along the fault is the source of the calcium carbonate. Shallow circulation along this corridor allows Norris' superheated water to slightly cool before surfacing at Mammoth, generally at about 170 °F (80 °C). Algae living in the warm pools have tinted the travertine shades of brown, orange, red, and green. Thermal activity here is extensive both over time and distance. The thermal flows show much variability with some variations taking place over periods ranging from decades to days. Terrace Mountain at Mammoth Hot Springs is the largest known carbonate-depositing spring in the world. The most famous feature at the springs is the Minerva Terrace, a series of travertine terraces. The terraces have been deposited by the spring over many years but, due to recent minor earthquake activity, the spring vent has shifted, rendering the terraces dry. The Mammoth Terraces extend all the way from the hillside, across the Parade Ground, and down to Boiling River. The Mammoth Hotel, as well as all of Fort Yellowstone, is built upon an old terrace formation known as Hotel Terrace. There was some concern when construction began in 1891 on the fort site that the hollow ground would not support the weight of the buildings. Several large sink holes (fenced off) can be seen out on the Parade Ground. This area has been thermally active for several thousand years. The Mammoth area exhibits much evidence of glacial activity from the Pinedale Glaciation. The summit of Terrace Mountain is covered with glacial till, thereby dating the travertine formation there to earlier than the end of the Pinedale Glaciation. Several thermal kames, including Capitol Hill and Dude Hill, are major features of the Mammoth Village area. Ice-marginal stream beds are in evidence in the small, narrow valleys where Floating Island Lake and Phantom Lake are found. In Gardner Canyon one can see the old, sorted gravel bed of the Gardner River covered by unsorted glacial till. The geothermal areas of Yellowstone include several geyser basins in Yellowstone National Park as well as other geothermal features such as hot springs, mud pots, and fumaroles. The number of thermal features in Yellowstone is estimated at 10,000. A study that was completed in 2011 found that a total of 1283 geysers have erupted in Yellowstone, 465 of which are active during an average year. These are distributed among nine geyser basins, with a few geysers found in smaller thermal areas throughout the Park. The number of geysers in each geyser basin are as follows: Upper Geyser Basin (410), Midway Geyser Basin (59), Lower Geyser Basin (283), Norris Geyser Basin (193), West Thumb Geyser Basin (84), Gibbon Geyser Basin (24), Lone Star Geyser Basin (21), Shoshone Geyser Basin (107), Heart Lake Geyser Basin (69), other areas (33). Although famous large geysers like Old Faithful are part of the total, most of Yellowstone's geysers are small, erupting to only a foot or two. The hydrothermal system that supplies the geysers with hot water sits within an ancient active caldera. Many of the thermal features in Yellowstone build up sinter, geyserite, or travertine deposits around and within them. The various geyser basins are located where rainwater and snowmelt can percolate into the ground, get indirectly superheated by the underlying Yellowstone hotspot, and then erupt at the surface as geysers, hot springs, and fumaroles. Thus flat-bottomed valleys between ancient lava flows and glacial moraines are where most of the large geothermal areas are located. Smaller geothermal areas can be found where fault lines reach the surface, in places along the circular fracture zone around the caldera, and at the base of slopes that collect excess groundwater.
Yellowstone National Park en Gardiner, Montana
RV Road Trip Yellowstone National Park - South to North Entrance - 28ft Motorhome
Family RV Road Trip USA - Day 9 of 90: Yellowstone
Drive our rented 28ft motorhome from Colter Bay campground in Grand Teton National Park, from the south to the north entrance to camp in Gardiner, Montana
Join us in the RV and we'll take you to Yellowstone, road trip music and noisy kids all the way.
BMW K1600GTL - Yellowstone West Entrance (Montana) to Biscuit Basin (geysers)
The last of our 08/09/2016 ride. We left out of the South entrance, visited the Grand Tetons, lunched in Jackson, WY, headed south and west around the Grand Tetons to ride the Idaho side. Then back into Yellowstone through the west entrance.
The sun was to are back and the weather was perfect. At the end we stopped at Biscuit Basin to check out some of the geysers at dusk.
From here we headed back to Grant Village.
Safe riding - James
A september in the Rocky Mountains, 2018 USA road trip
Our road trip through the Rockies took us to Colorado, Wyoming, Montana, South Dakota and Nebraska from September 8th to September 29th. Shot with iphone 8s and some shots with GH4. Music from Kacey Musgraves' Golden hour album, go buy it! Our itinerary was :
Day 1 - Saturday 08th
- Flight from Paris
- Denver
- Night in Denver - Airbnb
Day 2 - Sunday 09th
- Georgetown
- Steamboat Springs
- Night in Steamboat Springs - Steamboat Mountain Lodge
Day 3 - Monday 10th
- Dinosaur National Monument (Colorado and Utah parts)
- Flaming Gorge National Recreation Area (Red Canyon)
- Night in Rock Springs - Quality Inn
Day 4 - Tuesday 11th
- Jackson
- Grand Teton National Park
- Night in Grand Teton - Colter Bay campground
Day 5 - Wednesday 12th
- Grand Teton National Park
- Night in Grand Teton - Headwater's Lodge & Cabins at Flagg Ranch
Day 6 - Thursday 13th
- Yellowstone National Park
- Night in Yellowstone - Madison Campground
Day 7 - Friday 14th
- Yellowstone
- Night in Yellowstone - Old Faithful Inn
Day 8 - Saturday 15th
- Yellowstone
- West Yellowstone
- Earthquake lake
- Ennis
- Virginia City
- Nevada City
- Butte
- Night in Butte - Copper King Mansion
Day 9 - Sunday 16th
- Missoula
- Ronan
- Night in Whitefish - Baymont Inn
Day 10 - Monday 17th
- Glacier National Park
- Night in Glacier - Many Glacier campground
Day 11 - Tuesday 18th
- Glacier National Park
- Night in East Glacier - Whistling Swan Motel
Day 12 - Wednesday 19th
- Helena
- Bozeman
- Night in Bozeman - Royal 7 Budget Inn Motel
Day 13 - Thursday 20th
- Gardiner
- Yellowstone National Park
- Chief Joseph Scenic Byway
- Cody
- Night in Cody - Rodeway Inn
Day 14 - Friday 21st
- Greybull
- Big Horn Scenic Byway
- Sheridan
- Gillette
- Devils Tower
- Night at Devils Tower KOA
Day 15 - Saturday 22nd
- Hulett
- Belle Fourche
- Spearfish
- Deadwood
- Night in Deadwood - 1899 Inn
Day 16 - Sunday 23rd
- Mount Rushmore National Memorial
- Black Hills National Forest
- Custer State Park
- Black Elk Peak
- Needle highway
- Norbeck Byway
- Night in Keystone - Roosevelt Inn
Day 17 - Monday 24th
- Wind Cave National Park
- Hot Springs
- Rapid City
- Night in Rapid City - Americas Best Value Inn
Day 18 - Tuesday 25th
- Wall Drugstore
- Badlands National Park
- Night in Badlands - Cedar Pass campground
Day 19 - Wednesday 26th
- Badlands National Park
- Scenic
- Chadron
- Carhenge
- Alliance
- Chimney Rock National Historic Site
- Night in Scotts Bluff - Super 8
Day 20 - Thursday 27th
- Scottsbluff National Monument
- Cheyenne
- Fort Collins
- Night in Fort Collins - Americas Best Value East
Day 21 - Friday 28th
- Golden
- Denver
- Night in Denver - Comfort Inn Denver East
Day 22 - Saturday 29th
- Flight to Paris
Driving from Jackson Hole, WY to Yellowstone National Park
Today I drove from Jackson Hole, Wyoming to Butte, Montana. The first leg of today's journey takes us to the south entrance to Yellowstone National Park.
My Sony HXR-NX100 rode shotgun on a tripod shooting at 4 fps. The tripod was held in place using bungee cords giving it I nice smooth feel, even on bumpy roads. I also used this same camera to shoot various scenes around the country, and to interview folks.
Original music by Nim Portakey and/or created by Pinnacle Studio ScoreFitter.
Driving Yellowstone National Park
From the Northwest (Gardiner) entrance to Mammoth Hot Springs - 9/6/2013