Afrikaans
Akan
Albanian
Amharic
Arabic
Armenian
Azerbaijani
Basque
Belarusian
Bemba
Bengali
Bihari
Bosnian
Breton
Bulgarian
Cambodian
Catalan
Cebuano
Cherokee
Chichewa
Chinese (Simplified)
Chinese (Traditional)
Corsican
Croatian
Czech
Danish
Dutch
English
Esperanto
Estonian
Ewe
Faroese
Filipino
Finnish
French
Frisian
Ga
Galician
Georgian
German
Guarani
Gujarati
Haitian Creole
Hausa
Hawaiian
Hebrew
Hindi
Hmong
Hungarian
Icelandic
Igbo
Indonesian
Interlingua
Irish
Italian
Japanese
Javanese
Kannada
Kazakh
Kinyarwanda
Kirundi
Kongo
Korean
Krio (Sierra Leone)
Kurdish
Kurdish (Soranรฎ)
Kyrgyz
Laothian
Latin
Latvian
Lingala
Lithuanian
Lozi
Luganda
Luo
Luxembourgish
Macedonian
Malagasy
Malay
Malayalam
Maltese
Maori
Marathi
Mauritian Creole
Moldavian
Mongolian
Myanmar (Burmese)
Montenegrin
Nepali
Nigerian Pidgin
Northern Sotho
Norwegian
Norwegian (Nynorsk)
Occitan
Oriya
Oromo
Pashto
Persian
Polish
Portuguese (Brazil)
Portuguese (Portugal)
Punjabi
Quechua
Romanian
Romansh
Runyakitara
Russian
Samoan
Scots Gaelic
Serbian
Serbo-Croatian
Sesotho
Setswana
Seychellois Creole
Shona
Sindhi
Sinhalese
Slovak
Slovenian
Somali
Spanish
Spanish (Latin American)
Sundanese
Swahili
Swedish
Tajik
Tamil
Tatar
Telugu
Thai
Tigrinya
Tonga
Tshiluba
Tumbuka
Turkish
Turkmen
Twi
Uighur
Ukrainian
Urdu
Uzbek
Vietnamese
Welsh
Wolof
Xhosa
Yiddish
Yoruba
Zulu
(wind whirling)
(upbeat music)
(lively music)
(light music)
- Our journey begins at the east entrance
of Yellowstone National Park, exploring Yellowstone Lake.
We continue tracking the Yellowstone River
and catch our first glimpse of the park's
geothermal features in the Mud Volcano area.
As we look north, we discover why the views
of the Upper and Lower Falls had such a dramatic impact
on the park's creation.
Following the Grand Canyon of Yellowstone,
we head to the open planes of Lamar Valley.
At the northwest corner of Wyoming we understand
why the park is a national treasure,
starting with the Mammoth Hot Springs.
Venturing southward, exploring the geothermal basins
of the Yellowstone crater,
we arrive at its most famous feature, Old Faithful
in time for a spectacular finale to our journey.
(tinkling music)
With five entrances to Yellowstone National Park,
we approach from the east, following
along the Shoshone River in the Wapiti Valley,
about 80 kilometers from Cody, Wyoming.
Because of the weather restrictions,
the east entrance to the Yellowstone Park remains open
only from May to November.
On entering the park, there's a glimpse
of the towering peaks of the Absaroka Range
of the Rocky Mountains.
Yellowstone, which became the world's first national park
in 1872, hosts over three million visitors a year.
(light music)
Access to the park from the east is made possible
by the Sylvan Pass, maintained to allow winter travel
by snowmobile or snow coach.
It was named after Sylvan Lake which rests along the route.
As we continue along the pass, we come to Yellowstone Lake,
the largest body of water in the park.
Its basin is part of the massive Yellowstone crater carved
from the volcanic eruptions over 600,000 years ago.
(birds twittering) (summery music)
Yellowstone offers a splendid habitat
for over 60 species of large mammals.
Here we spot a small herd of elk.
The park hosts an estimated 30,000 in total.
The lake's northern tip is where its fed
and drained by Yellowstone River.
A fishing bridge crosses at this meeting point,
a spawning area for the native cutthroat trout.
And nearby is a popular recreational vehicle park.
Visitors wanting less rustic accommodation stay
at the historic Lake Hotel.
Originally built in the late 19th century,
the hotel was restored to its 1920s grandeur in 1990.
The Yellowstone River is a main tributary
of the Missouri River, and drains nearly
a 1100 kilometer stretch of the Rockies.
Within the park, the river is used recreationally
for flatboat fishing.
The words, "Yellow stone" were recorded
by Lewis and Clark during their famous expedition
after meeting with the Minitari Indians
near the river in 1805.
North along the river we enter the mud volcano area.
These formations are created from a geo-excretion
of iron and hydrogen sulfide, which results
in a dark gray color and rotten egg smell.
(majestic music)
Flowing north out of Hayden Valley,
the first signs of rapids are present
as the Yellowstone River begins its decent
toward the park's Grand Canyon.
(water rushing)
The river first cascades at the Upper Falls,
dropping about 33 meters.
Spectacular viewing points along the trails
on either side of the canyon, makes this one
of the favorite places in the park among visitors.
And it's yet another example
of how Yellowstone's landscape was shaped
from volcanic events 600,000 years ago.
The Upper Falls marks a junction
where a hard lava flow met with a softer altered flow.
In 1871, Dr. Ferdinand Hayden, whose name was given
to the valley, led a US geological survey
into the unexplored Yellowstone region.
Joining the expedition were photographer
William Henry Jackson and artist, Thomas Moran.
Their photographs and paintings of the falls captured
the nation's attention and inspired congress
to establish the national park a year later.
The Yellowstone River continues to flow
another half kilometer before taking a much bigger plunge
that will take it to the mouth of the Grand Canyon.
The Lower Falls drop 94 meters and is the tallest waterfall
in the park, nearly twice the height of Niagara Falls.
It's also the largest volume
of falling water in the Rocky Mountains.
And this is the famous vantage point along the canyon
that was immortalized in the famous painting
by Thomas Moran, which now hangs in the White House.
It was these majestic falls that were the subject
of the almost mythic accounts composed
by prospectors venturing into the Montana territory
in the mid 19th century.
Frontier newspapers printed claims
that the falls were thousands of feet high,
and referred to it as the most sublime spot on earth.
(light music)
Two scenic routes of Grand Loop Road offer breathtaking
views of the canyon such as Point Sublime on the south rim.
The other viewpoints take visitors to the absolute brink
of the Upper and Lower Falls,
offering them a riveting encounter
with the powerful cascades.
Some 10,000 years after the volcanic eruptions
in Yellowstone, lava flow filled the region.
One of these was a canyon lava flow,
leaving a thermal basin shaped from the hot steam
and gasses that altered and weakened the lava.
Other flows blocked lakes and created overflowing lakes
that further molded the Yellowstone canyon.
(light upbeat music)
The park contains several broad, open valleys,
such as the Lamar Valley in the park's northeast corner.
Packhorse treks are very popular for guided camping tours.
Organized trips can last as long as 10 days
as visitors venture into the heart
of Yellowstone's tranquil wilderness.
Lamar Valley and the river stretches
for almost 10 kilometers from its confluence
with the Yellowstone River,
just below the Grand Canyon to its junction
with the Soda Butte Creek tributary.
A true treasure of Yellowstone,
the valley is remarkable in its scenery.
But it was also the stage for one
of the most significant wildlife conservation projects,
the recovery of the American bison.
(somber music)
In 1903, there were less than 50 bison in the park.
A century later, the population was nearly 5,000.
The Yellowstone Park bison herd is one of four
in North America that are free roaming and genetically pure.
27 kilometers north of the canyon,
the small creek shoots off the Yellowstone River
and flows south to the park's third notable cascade,
Tower Fall, which stands 40 meters tall.
Named for the volcanic formations that surround it,
the park offers a breathtaking view
from an overlook that draws visitors in droves.
Flying northwest, we pass
over the Roosevelt Lodge history district.
Originally built in 1919 as an education center,
the lodge offers guests rustic accommodation
and horseback tours, exploring the area's wildlife.
The area was named in honor of President Teddy Roosevelt
who camped near the site prior to its construction.
Here we witness another popular tourist attraction.
Stagecoach rides. (coach rattling)
Once the primary mode of transportation for guests,
who'd traverse the parks for days along dusty roads,
stagecoaches offer a nostalgic adventure
through the sage-covered fields of Pleasant Valley.
We are fortunate to capture a rarely seen resident
of Yellowstone, the black bear.
The park actually has a sizable population
as opposed to the estimated mere 300 grizzlies
that take residence in the park.
Although this bear is seen in the open meadow,
black bears are usually found in timber areas.
In our journey across the northern valleys of Yellowstone,
we observe a playful bison.
These animals are quite nomadic, migrating high
to these grassy plateaus in the summer to mate.
They are vegetarians, grazing on the grasslands
and the meadows and foothills
as well as during the colder seasons.
Bison are the biggest of the park's animals,
and it is believed that the Yellowstone bison habitat is the
only one in America to have existed since prehistoric times.
Elk are high elevation mammals,
and are more often seen in the early morning
or late afternoon in the summers,
grazing on the grasses of the meadows.
In 1988, wildfires damaged 36 percent of the park.
These areas eventually became a habitat
for the elk as lush vegetation developed.
For this reason, they also graze in areas recently logged.
The elk bulls are symbolized by their beautiful antlers.
The rack may have six to eight branches on each side,
and weigh more than 13 kilos.
By March or April of each year the bull
completely sheds its antlers then begins
to regrow them starting in May until August.
And nearby the Gardner River cuts
through the rugged Sheepeater Canyon,
named after the Sheepeater Indians,
who are believed to have used these cliff edges
to herd and trap game.
Today a spectacular trail along the canyon brings hikers
to one of Yellowstone's best kept secrets, the Osprey Falls.
Nestled in the narrow gorge, the spray created
by the waterfall provides a welcome cooling mist
for visitors on a hot summer's day.
(majestic music)
The park sits on a plateau
at an average height of 2400 meters.
Bound by mountains that soar as high as 3300 meters.
Often the plateau fills with clouds,
setting a very enchanting tone for the visitors.
(flowery music)
Nestled between Mount Everts and the Mammoth area,
about eight kilometers from the north entrance,
is Yellowstone Park's headquarters.
A series of red roof buildings constructed
in the late 1800s and early 1900s.
For most of its early existence as a national park,
Yellowstone was operated by the US cavalry,
with this area serving as an Army post for 32 years.
The stone buildings house 400 occupants.
In 1918 the Army turned over control of the park
to civilians who have maintained Fort Yellowstone
as the park's headquarters ever since.
The historic Army buildings now serve
as offices and resident housing.
Additionally, there is a medical clinic,
and the Albright museum which chronicles a history
of the park's residents.
Adjacent to the Fort Yellowstone district lies a magical
white hillside, blanketed in calcium carbonate.
(soothing music)
This geothermal wonder of nature,
the Mammoth Hot Springs, is a large complex
of limestone terraces, appearing in white,
tan and cream colored varieties.
A circuit a boardwalks and stairs allow explorers
to navigate through the impressive displays
of step-like sedimentary rock.
Each of these formations exhibits individual character,
such as the now extinct Liberty Cap,
a 14 meter cone formed from hot water emanating
from a single source.
(water gushing)
As heated water from the Norris Geyser Basin moves
through a fault line and escapes the earth's surface
through cracks and fissures,
dissolved limestone is deposited onto the terraces.
Over 1800 kilos of calcium carbonate flow
into Mammoth each day.
The yellow, orange and brown terraces get their color
from bacteria that are able to grow in the waters.
We exit the northwest region of Yellowstone
and continue our journey moving south,
back towards the crater rim.
It's here that we'll explore a basin
that boasts the park's highest temperatures.
The extreme thermal conditions
of the Norris Geyser Basin result
from the junction of two major fault lines,
and the ring of the fracture zone of the Yellowstone crater.
For this reason, the basin boasts the hottest,
most acidic and most dynamic thermal features in the park.
Clear pools become violently bubbly and muddy,
even temporarily transforming into geysers.
Within this basin, we see a hot spring
with prismatic characteristics,
developed from the pigmentation of the bacteria
that grows in this mineral-rich water.
Near the western entrance is the origin
of the Madison River at the confluence
of Gibbon's and Firehole Rivers,
overlooked by National Park Mountain.
(flowery music)
This place is known as Madison Junction,
and legend has it that this is the site
where leaders of the 1870 Washburn Expedition
first conceived the idea of creating a national park
while sat around a campfire.
Continuing south we examine the Lower Geyser Basin
with thermal features that are scattered in small clusters,
spread out mostly on open meadows along the Firehole River.
We concentrate on the fire lake
and the fountain groups known for its multicolored mud pots.
The basin also delights spectators
with its fumaroles and geysers,
as well as bubbling pools and hot springs.
(lively music)
The white dome ejects water and steam
through a six meter high pinkish-white cone.
The lower basin geyser has many areas of high activity,
such as the Firehole and Hot Lakes
which drain from a tributary of the Firehole River.
The aptly named Steady Geyser is the largest,
constantly erupting geyser in Yellowstone and the world.
The Fountain Paint Pot Group is the most diverse cluster
of thermal features in the lower basin,
with hot springs, mud pots, geysers and fumaroles.
The Clepsydra Geyser, a name derived
from the Greek word for water clock,
has four vents spewing water in two different phases.
Clepsydra's wild phase can last three to six hours.
The other notable feature of
this group is the Fountain Paint Pots
which derive their name from their red,
yellow and brown colors.
In the spring these mut pots are most active
when an abundance source of water
from melted snow creates a dancing effect in the bubbles.
During the warmer summer months
the mud gets drier and thicker.
In between the Upper and Lower Geyser Basins is the
appropriately named Midway Geyser Basin,
nicknamed Hells Half Acre, by the writer, Rudyard Kipling.
This is Excelsior Geyser, once the largest in the world,
which releases 22 million liters
of water per day into Firehole River.
Excelsior is flanked by the Grand Prismatic Spring,
the largest hot spring in the park
and third largest in the world.
The spring discharges over 2,000 liters of water per minute.
The color varies at times depending on the pigment ratio
of the bacteria growing in the water
as well as the water temperature.
The deep blue color is so intense due to the high purity
and depth of the water in the middle.
The Grand Prismatic Spring is yet
another famous Yellowstone subject of artist, Thomas Moran.
Moving along to the Upper Geysers,
we focus on an isolated group called The Black Sand Basin,
highlighted by its colorful hot springs
such as emerald and rainbow pools.
The basin got its name from the black volcanic glass
that covers much of the area.
Another famous feature of the Upper Geysers is the
most unusually shaped Grotto Geyser.
The gusher formed around stumps
of dead pine trees destroyed
by an earthquake thousands of years ago.
With a clear view of the Old Faithful Geyser,
the inn of the same name has operated
as a hotel in the park since 1904.
Constructed of locally grown pine,
it is the largest log hotel in the world.
The foundation and the massive fireplace
inside were made from a volcanic stone
that is dominant in the park.
A short walk from the historic
inn is the Old Faithful Geyser.
Because of its predictability, it is quite possibly the
most calculable geothermal feature on the planet.
Thus, the cone-shaped geyser is also the most visited
and anticipated attraction.
Like most visitors to the park,
the famous US Army expedition that named Yellowstone
in 1870 count Old Faithful
as the first geyser they set eyes on.
Thus, she was also the first in the park
to receive a name.
The best indicator among locals
of the next eruption is to watch
for the benches around Old Faithful to fill and overflow.
(exciting music)
Old Faithful begins each performance
with a prologue of splashing and small-jetting
for a period of up to 20 minutes.
The jetting usually grows over two to three steps
before reaching its maximum height.
Ranging 32 to 56 meters in height,
it shoots out between 14 and 32 thousand liters of water.
Predictions of Old Faithful's next eruption are based
on the duration of its previous blast,
which average two to four minutes.
The intervals between eruptions average about 90 minutes,
and times are estimated one eruption in advance.
Old Faithful is indeed both a symbol of Yellowstone Park
and an American icon.
A perfect place to end this journey.
(upbeat music)
(letters blasting)
Can't find what you're looking for?
Get subtitles in any language from opensubtitles.com, and translate them here.