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1

Firehole Canyon Drive

Firehole Canyon Drive is a 2-mile, one-way road off the Grand Loop south of Madison. The drive has a waterfall overlook and swimming area.

2

Norris Geyser Basin

Norris Geyser Basin is the hottest and most changeable thermal area in Yellowstone. We will explore many of the features you would see if you walked the 2 1/4 miles (3.6 km) of trails. Discover the location of the world's tallest active geyser, colorful hot springs, and microscopic life in one of the most extreme environments on earth.

3

Gibbon Falls

Gibbon Falls drops 84 feet (0.3 m) over a remnant of the Yellowstone caldera rim. The caldera was created by a massive volcanic eruption approximately 640,000 years ago. A quick stop on our drive of the lower loop, this is a great opportunity for a photo moment.

4

Old Faithful

Old Faithful is located in Yellowstone’s Upper Geyser Basin in the southwest section of the park. The geyser-viewing area is the most accessible and visitor-friendly in the park with bench seating, a large parking lot, and a ranger station that tracks the time, height and length of an eruption to predict the next eruption.

5

Fountain Paint Pot

Along Fountain Paint Pot Trail you will see various hydrothermal features that are expressions of Yellowstone’s still active volcano. Within this geologic system, each type of thermal feature is represented. They can be grouped into two general categories—those with a great deal of water (hot springs and geysers) and those with limited water (mudpots and fumaroles). Despite their structural similarities, no two features are exactly alike.

6

Grand Prismatic Spring

Grand Prismatic Spring is located in the Midway Geyser Basin. It has the distinction of being the park's largest hot spring. It measures approximately 370 feet (112.8 m) in diameter and is over 121 feet (37 m ) deep. A description of this spring by fur trapper Osborne Russell in 1839 also makes it the earliest described thermal feature in Yellowstone that is definitely identifiable.

7

Yellowstone Lake

Situated at 7,733 feet (2,357 m) above sea level, Yellowstone Lake is the largest high elevation lake (above 7,000 feet / 2,134 m) in North America. It is roughly 20 miles (32.2 km) long and 14 miles (22.5 km) wide, with 141 miles (227 km) of shoreline and a surface area of 132 square miles (342 km2). Yellowstone Lake freezes over completely every winter in late December or early January, with ice thicknesses varying from a few inches to more than two feet. The lake usually thaws in late May or early June. Yellowstone Lake remains cold year-round, with an average water temperature of 41°F (5°C). Because of the extremely cold water, swimming is not recommended. Survival time is estimated to be only 20 to 30 minutes in water at this temperature.

8

Yellowstone Geysers - Mud Volcano Area

Yellowstone itself is a volcano, and one of its most spectacular eruptions occurred 640,000 years ago. During the eruption, the land collapsed and left a large depression in the earth—the Yellowstone Caldera. This caldera filled with lava flows over hundreds and thousands of years creating the volcanic plateau that comprises much of the central part of the park. Here at Mud Volcano you are close to one of the resurgent domes. The hills you see east of here comprise Sour Creek Dome. Resurgent domes are areas of active ground deformation, where the land moves up or down with the fluctuation of the magma chamber below. Scientists monitor these domes closely for information about ongoing volcanic activity. Not surprisingly, many of the park’s geysers, hot springs, mudpots, and fumaroles are also found near or within the caldera.

9

Grand Canyon of the Yellowstone

The Grand Canyon of the Yellowstone River expresses the park's complex geologic history in dramatic colors and shapes. Puffs of steam mark hydrothermal features in the canyon's walls. The Upper and Lower Falls of the Yellowstone River add to the grandeur of the unique natural treasure.

10

Hayden Valley

Hayden Valley is a large, sub-alpine valley in Yellowstone National Park straddling the Yellowstone River between Yellowstone Falls and Yellowstone Lake. The valley floor along the river is an ancient lake bed from a time when Yellowstone Lake was much larger.

11

Firehole Canyon Drive

Firehole Canyon Drive is a 2-mile, one-way road off the Grand Loop south of Madison. The drive has a waterfall overlook and swimming area.

12

Norris Geyser Basin

Norris Geyser Basin is the hottest and most changeable thermal area in Yellowstone. We will explore many of the features you would see if you walked the 2 1/4 miles (3.6 km) of trails. Discover the location of the world's tallest active geyser, colorful hot springs, and microscopic life in one of the most extreme environments on earth.

13

Gibbon Falls

Gibbon Falls drops 84 feet (0.3 m) over a remnant of the Yellowstone caldera rim. The caldera was created by a massive volcanic eruption approximately 640,000 years ago. A quick stop on our drive of the lower loop, this is a great opportunity for a photo moment.

14

Old Faithful

Old Faithful is located in Yellowstone’s Upper Geyser Basin in the southwest section of the park. The geyser-viewing area is the most accessible and visitor-friendly in the park with bench seating, a large parking lot, and a ranger station that tracks the time, height and length of an eruption to predict the next eruption.

15

Fountain Paint Pot

Along Fountain Paint Pot Trail you will see various hydrothermal features that are expressions of Yellowstone’s still active volcano. Within this geologic system, each type of thermal feature is represented. They can be grouped into two general categories—those with a great deal of water (hot springs and geysers) and those with limited water (mudpots and fumaroles). Despite their structural similarities, no two features are exactly alike.

16

Grand Prismatic Spring

Grand Prismatic Spring is located in the Midway Geyser Basin. It has the distinction of being the park's largest hot spring. It measures approximately 370 feet (112.8 m) in diameter and is over 121 feet (37 m ) deep. A description of this spring by fur trapper Osborne Russell in 1839 also makes it the earliest described thermal feature in Yellowstone that is definitely identifiable.

17

Yellowstone Lake

Situated at 7,733 feet (2,357 m) above sea level, Yellowstone Lake is the largest high elevation lake (above 7,000 feet / 2,134 m) in North America. It is roughly 20 miles (32.2 km) long and 14 miles (22.5 km) wide, with 141 miles (227 km) of shoreline and a surface area of 132 square miles (342 km2). Yellowstone Lake freezes over completely every winter in late December or early January, with ice thicknesses varying from a few inches to more than two feet. The lake usually thaws in late May or early June. Yellowstone Lake remains cold year-round, with an average water temperature of 41°F (5°C). Because of the extremely cold water, swimming is not recommended. Survival time is estimated to be only 20 to 30 minutes in water at this temperature.

18

Yellowstone Geysers - Mud Volcano Area

Yellowstone itself is a volcano, and one of its most spectacular eruptions occurred 640,000 years ago. During the eruption, the land collapsed and left a large depression in the earth—the Yellowstone Caldera. This caldera filled with lava flows over hundreds and thousands of years creating the volcanic plateau that comprises much of the central part of the park. Here at Mud Volcano you are close to one of the resurgent domes. The hills you see east of here comprise Sour Creek Dome. Resurgent domes are areas of active ground deformation, where the land moves up or down with the fluctuation of the magma chamber below. Scientists monitor these domes closely for information about ongoing volcanic activity. Not surprisingly, many of the park’s geysers, hot springs, mudpots, and fumaroles are also found near or within the caldera.

19

Grand Canyon of the Yellowstone

The Grand Canyon of the Yellowstone River expresses the park's complex geologic history in dramatic colors and shapes. Puffs of steam mark hydrothermal features in the canyon's walls. The Upper and Lower Falls of the Yellowstone River add to the grandeur of the unique natural treasure.

20

Hayden Valley

Hayden Valley is a large, sub-alpine valley in Yellowstone National Park straddling the Yellowstone River between Yellowstone Falls and Yellowstone Lake. The valley floor along the river is an ancient lake bed from a time when Yellowstone Lake was much larger.

21

Каньон Файрхол Драйв

Firehole Canyon Drive — это дорога с односторонним движением протяженностью 2 мили от Гранд-Луп к югу от Мэдисона. У дороги есть вид на водопад и место для купания.

22

Бассейн Норрис Гейзер

Бассейн Норрис-Гейзер — самая горячая и самая изменчивая термальная зона в Йеллоустоне. Мы рассмотрим многие особенности, которые вы увидите, если пройдете 2 1/4 мили (3,6 км) по тропам. Откройте для себя местонахождение самого высокого в мире активного гейзера, красочных горячих источников и микроскопической жизни в одном из самых экстремальных условий на земле.

23

Гиббон Фолс

Водопад Гиббон падает с высоты 84 фута (0,3 м) над остатком края кальдеры Йеллоустон. Кальдера образовалась в результате мощного извержения вулкана примерно 640 000 лет назад. Быстрая остановка на нашем проезде нижней петли, это отличная возможность для фото.

24

Старый Верный

Old Faithful расположен в Верхнем бассейне гейзеров Йеллоустона в юго-западной части парка. Зона наблюдения за гейзерами является наиболее доступной и удобной для посетителей в парке со скамейками, большой парковкой и станцией рейнджеров, которая отслеживает время, высоту и продолжительность извержения, чтобы предсказать следующее извержение.

25

Горшок с краской для фонтана

Вдоль тропы Fountain Paint Pot Trail вы увидите различные гидротермальные особенности, которые являются выражением все еще действующего вулкана Йеллоустона. В пределах этой геологической системы представлены все типы термальных особенностей. Их можно разделить на две основные категории — многоводные (горячие источники и гейзеры) и маловодные (грязевые котлы и фумаролы). Несмотря на их структурное сходство, нет двух одинаковых функций.

26

Большая призматическая пружина

Большой призматический источник расположен в бассейне гейзеров Мидуэй. Он отличается тем, что является самым большим горячим источником в парке. Он имеет диаметр около 370 футов (112,8 м) и глубину более 121 фута (37 м). Описание этого источника, сделанное охотником на меха Осборном Расселом в 1839 году, также делает его самым ранним описанным термальным объектом в Йеллоустоне, который определенно можно идентифицировать.

27

Йеллоустонское озеро

Расположенное на высоте 7733 футов (2357 м) над уровнем моря, Йеллоустонское озеро является крупнейшим высокогорным озером (более 7000 футов /2134 м) в Северной Америке. Это примерно 20 миль (32,2 км) в длину и 14 миль (22,5 км) в ширину, с 141 милей (227 км) береговой линии и площадью поверхности 132 квадратных мили (342 км2). Озеро Йеллоустоун полностью замерзает каждую зиму в конце декабря или начале января, при этом толщина льда варьируется от нескольких дюймов до более двух футов. Озеро обычно оттаивает в конце мая или начале июня. Озеро Йеллоустоун остается холодным круглый год со средней температурой воды 41°F (5°C). Из-за очень холодной воды купаться не рекомендуется. По оценкам, время выживания в воде при этой температуре составляет всего 20–30 минут.

28

Йеллоустонские гейзеры - Район грязевого вулкана

Йеллоустоун сам по себе является вулканом, и одно из его самых впечатляющих извержений произошло 640 000 лет назад. Во время извержения земля обрушилась, оставив в земле большую впадину — Йеллоустонскую кальдеру. Эта кальдера, заполненная потоками лавы на протяжении сотен и тысяч лет, создала вулканическое плато, составляющее большую часть центральной части парка. Здесь, в Грязевом вулкане, вы находитесь рядом с одним из возрождающихся куполов. Холмы, которые вы видите к востоку отсюда, составляют Купол Сур-Крик. Возрождающиеся купола представляют собой области активной деформации грунта, где земля перемещается вверх или вниз при колебаниях магматического очага внизу. Ученые внимательно следят за этими куполами, чтобы получить информацию о продолжающейся вулканической активности. Неудивительно, что многие из гейзеров, горячих источников, грязевых котлов и фумарол парка также находятся рядом с кальдерой или внутри нее.

29

Гранд-Каньон Йеллоустона

Гранд-Каньон реки Йеллоустоун выражает сложную геологическую историю парка в драматических цветах и формах. Клубы пара отмечают гидротермальные образования на стенах каньона. Верхний и Нижний водопады реки Йеллоустоун дополняют величие уникального природного сокровища.

30

Хейден Вэлли

Хейден-Вэлли — большая субальпийская долина в Йеллоустонском национальном парке, расположенная по обе стороны реки Йеллоустон между Йеллоустонским водопадом и Йеллоустонским озером. Дно долины вдоль реки представляет собой древнее дно озера тех времен, когда Йеллоустонское озеро было намного больше.

31

Firehole Canyon Drive

Firehole Canyon Drive is a 2-mile, one-way road off the Grand Loop south of Madison. The drive has a waterfall overlook and swimming area.

32

Norris Geyser Basin

Norris Geyser Basin is the hottest and most changeable thermal area in Yellowstone. We will explore many of the features you would see if you walked the 2 1/4 miles (3.6 km) of trails. Discover the location of the world's tallest active geyser, colorful hot springs, and microscopic life in one of the most extreme environments on earth.

33

Gibbon Falls

Gibbon Falls drops 84 feet (0.3 m) over a remnant of the Yellowstone caldera rim. The caldera was created by a massive volcanic eruption approximately 640,000 years ago. A quick stop on our drive of the lower loop, this is a great opportunity for a photo moment.

34

Old Faithful

Old Faithful is located in Yellowstone’s Upper Geyser Basin in the southwest section of the park. The geyser-viewing area is the most accessible and visitor-friendly in the park with bench seating, a large parking lot, and a ranger station that tracks the time, height and length of an eruption to predict the next eruption.

35

Fountain Paint Pot

Along Fountain Paint Pot Trail you will see various hydrothermal features that are expressions of Yellowstone’s still active volcano. Within this geologic system, each type of thermal feature is represented. They can be grouped into two general categories—those with a great deal of water (hot springs and geysers) and those with limited water (mudpots and fumaroles). Despite their structural similarities, no two features are exactly alike.

36

Grand Prismatic Spring

Grand Prismatic Spring is located in the Midway Geyser Basin. It has the distinction of being the park's largest hot spring. It measures approximately 370 feet (112.8 m) in diameter and is over 121 feet (37 m ) deep. A description of this spring by fur trapper Osborne Russell in 1839 also makes it the earliest described thermal feature in Yellowstone that is definitely identifiable.

37

Yellowstone Lake

Situated at 7,733 feet (2,357 m) above sea level, Yellowstone Lake is the largest high elevation lake (above 7,000 feet / 2,134 m) in North America. It is roughly 20 miles (32.2 km) long and 14 miles (22.5 km) wide, with 141 miles (227 km) of shoreline and a surface area of 132 square miles (342 km2). Yellowstone Lake freezes over completely every winter in late December or early January, with ice thicknesses varying from a few inches to more than two feet. The lake usually thaws in late May or early June. Yellowstone Lake remains cold year-round, with an average water temperature of 41°F (5°C). Because of the extremely cold water, swimming is not recommended. Survival time is estimated to be only 20 to 30 minutes in water at this temperature.

38

Yellowstone Geysers - Mud Volcano Area

Yellowstone itself is a volcano, and one of its most spectacular eruptions occurred 640,000 years ago. During the eruption, the land collapsed and left a large depression in the earth—the Yellowstone Caldera. This caldera filled with lava flows over hundreds and thousands of years creating the volcanic plateau that comprises much of the central part of the park. Here at Mud Volcano you are close to one of the resurgent domes. The hills you see east of here comprise Sour Creek Dome. Resurgent domes are areas of active ground deformation, where the land moves up or down with the fluctuation of the magma chamber below. Scientists monitor these domes closely for information about ongoing volcanic activity. Not surprisingly, many of the park’s geysers, hot springs, mudpots, and fumaroles are also found near or within the caldera.

39

Grand Canyon of the Yellowstone

The Grand Canyon of the Yellowstone River expresses the park's complex geologic history in dramatic colors and shapes. Puffs of steam mark hydrothermal features in the canyon's walls. The Upper and Lower Falls of the Yellowstone River add to the grandeur of the unique natural treasure.

40

Hayden Valley

Hayden Valley is a large, sub-alpine valley in Yellowstone National Park straddling the Yellowstone River between Yellowstone Falls and Yellowstone Lake. The valley floor along the river is an ancient lake bed from a time when Yellowstone Lake was much larger.

41

Firehole Canyon Drive

Firehole Canyon Drive is a 2-mile, one-way road off the Grand Loop south of Madison. The drive has a waterfall overlook and swimming area.

42

Norris Geyser Basin

Norris Geyser Basin is the hottest and most changeable thermal area in Yellowstone. We will explore many of the features you would see if you walked the 2 1/4 miles (3.6 km) of trails. Discover the location of the world's tallest active geyser, colorful hot springs, and microscopic life in one of the most extreme environments on earth.

43

Gibbon Falls

Gibbon Falls drops 84 feet (0.3 m) over a remnant of the Yellowstone caldera rim. The caldera was created by a massive volcanic eruption approximately 640,000 years ago. A quick stop on our drive of the lower loop, this is a great opportunity for a photo moment.

44

Old Faithful

Old Faithful is located in Yellowstone’s Upper Geyser Basin in the southwest section of the park. The geyser-viewing area is the most accessible and visitor-friendly in the park with bench seating, a large parking lot, and a ranger station that tracks the time, height and length of an eruption to predict the next eruption.

45

Fountain Paint Pot

Along Fountain Paint Pot Trail you will see various hydrothermal features that are expressions of Yellowstone’s still active volcano. Within this geologic system, each type of thermal feature is represented. They can be grouped into two general categories—those with a great deal of water (hot springs and geysers) and those with limited water (mudpots and fumaroles). Despite their structural similarities, no two features are exactly alike.

46

Grand Prismatic Spring

Grand Prismatic Spring is located in the Midway Geyser Basin. It has the distinction of being the park's largest hot spring. It measures approximately 370 feet (112.8 m) in diameter and is over 121 feet (37 m ) deep. A description of this spring by fur trapper Osborne Russell in 1839 also makes it the earliest described thermal feature in Yellowstone that is definitely identifiable.

47

Yellowstone Lake

Situated at 7,733 feet (2,357 m) above sea level, Yellowstone Lake is the largest high elevation lake (above 7,000 feet / 2,134 m) in North America. It is roughly 20 miles (32.2 km) long and 14 miles (22.5 km) wide, with 141 miles (227 km) of shoreline and a surface area of 132 square miles (342 km2). Yellowstone Lake freezes over completely every winter in late December or early January, with ice thicknesses varying from a few inches to more than two feet. The lake usually thaws in late May or early June. Yellowstone Lake remains cold year-round, with an average water temperature of 41°F (5°C). Because of the extremely cold water, swimming is not recommended. Survival time is estimated to be only 20 to 30 minutes in water at this temperature.

48

Yellowstone Geysers - Mud Volcano Area

Yellowstone itself is a volcano, and one of its most spectacular eruptions occurred 640,000 years ago. During the eruption, the land collapsed and left a large depression in the earth—the Yellowstone Caldera. This caldera filled with lava flows over hundreds and thousands of years creating the volcanic plateau that comprises much of the central part of the park. Here at Mud Volcano you are close to one of the resurgent domes. The hills you see east of here comprise Sour Creek Dome. Resurgent domes are areas of active ground deformation, where the land moves up or down with the fluctuation of the magma chamber below. Scientists monitor these domes closely for information about ongoing volcanic activity. Not surprisingly, many of the park’s geysers, hot springs, mudpots, and fumaroles are also found near or within the caldera.

49

Grand Canyon of the Yellowstone

The Grand Canyon of the Yellowstone River expresses the park's complex geologic history in dramatic colors and shapes. Puffs of steam mark hydrothermal features in the canyon's walls. The Upper and Lower Falls of the Yellowstone River add to the grandeur of the unique natural treasure.

50

Hayden Valley

Hayden Valley is a large, sub-alpine valley in Yellowstone National Park straddling the Yellowstone River between Yellowstone Falls and Yellowstone Lake. The valley floor along the river is an ancient lake bed from a time when Yellowstone Lake was much larger.

51

Firehole Canyon Drive

Firehole Canyon Drive is a 2-mile, one-way road off the Grand Loop south of Madison. The drive has a waterfall overlook and swimming area.

52

Norris Geyser Basin

Norris Geyser Basin is the hottest and most changeable thermal area in Yellowstone. We will explore many of the features you would see if you walked the 2 1/4 miles (3.6 km) of trails. Discover the location of the world's tallest active geyser, colorful hot springs, and microscopic life in one of the most extreme environments on earth.

53

Gibbon Falls

Gibbon Falls drops 84 feet (0.3 m) over a remnant of the Yellowstone caldera rim. The caldera was created by a massive volcanic eruption approximately 640,000 years ago. A quick stop on our drive of the lower loop, this is a great opportunity for a photo moment.

54

Old Faithful

Old Faithful is located in Yellowstone’s Upper Geyser Basin in the southwest section of the park. The geyser-viewing area is the most accessible and visitor-friendly in the park with bench seating, a large parking lot, and a ranger station that tracks the time, height and length of an eruption to predict the next eruption.

55

Fountain Paint Pot

Along Fountain Paint Pot Trail you will see various hydrothermal features that are expressions of Yellowstone’s still active volcano. Within this geologic system, each type of thermal feature is represented. They can be grouped into two general categories—those with a great deal of water (hot springs and geysers) and those with limited water (mudpots and fumaroles). Despite their structural similarities, no two features are exactly alike.

56

Grand Prismatic Spring

Grand Prismatic Spring is located in the Midway Geyser Basin. It has the distinction of being the park's largest hot spring. It measures approximately 370 feet (112.8 m) in diameter and is over 121 feet (37 m ) deep. A description of this spring by fur trapper Osborne Russell in 1839 also makes it the earliest described thermal feature in Yellowstone that is definitely identifiable.

57

Yellowstone Lake

Situated at 7,733 feet (2,357 m) above sea level, Yellowstone Lake is the largest high elevation lake (above 7,000 feet / 2,134 m) in North America. It is roughly 20 miles (32.2 km) long and 14 miles (22.5 km) wide, with 141 miles (227 km) of shoreline and a surface area of 132 square miles (342 km2). Yellowstone Lake freezes over completely every winter in late December or early January, with ice thicknesses varying from a few inches to more than two feet. The lake usually thaws in late May or early June. Yellowstone Lake remains cold year-round, with an average water temperature of 41°F (5°C). Because of the extremely cold water, swimming is not recommended. Survival time is estimated to be only 20 to 30 minutes in water at this temperature.

58

Yellowstone Geysers - Mud Volcano Area

Yellowstone itself is a volcano, and one of its most spectacular eruptions occurred 640,000 years ago. During the eruption, the land collapsed and left a large depression in the earth—the Yellowstone Caldera. This caldera filled with lava flows over hundreds and thousands of years creating the volcanic plateau that comprises much of the central part of the park. Here at Mud Volcano you are close to one of the resurgent domes. The hills you see east of here comprise Sour Creek Dome. Resurgent domes are areas of active ground deformation, where the land moves up or down with the fluctuation of the magma chamber below. Scientists monitor these domes closely for information about ongoing volcanic activity. Not surprisingly, many of the park’s geysers, hot springs, mudpots, and fumaroles are also found near or within the caldera.

59

Grand Canyon of the Yellowstone

The Grand Canyon of the Yellowstone River expresses the park's complex geologic history in dramatic colors and shapes. Puffs of steam mark hydrothermal features in the canyon's walls. The Upper and Lower Falls of the Yellowstone River add to the grandeur of the unique natural treasure.

60

Hayden Valley

Hayden Valley is a large, sub-alpine valley in Yellowstone National Park straddling the Yellowstone River between Yellowstone Falls and Yellowstone Lake. The valley floor along the river is an ancient lake bed from a time when Yellowstone Lake was much larger.

61

Firehole Canyon Drive

Firehole Canyon Drive is a 2-mile, one-way road off the Grand Loop south of Madison. The drive has a waterfall overlook and swimming area.

62

Norris Geyser Basin

Norris Geyser Basin is the hottest and most changeable thermal area in Yellowstone. We will explore many of the features you would see if you walked the 2 1/4 miles (3.6 km) of trails. Discover the location of the world's tallest active geyser, colorful hot springs, and microscopic life in one of the most extreme environments on earth.

63

Gibbon Falls

Gibbon Falls drops 84 feet (0.3 m) over a remnant of the Yellowstone caldera rim. The caldera was created by a massive volcanic eruption approximately 640,000 years ago. A quick stop on our drive of the lower loop, this is a great opportunity for a photo moment.

64

Old Faithful

Old Faithful is located in Yellowstone’s Upper Geyser Basin in the southwest section of the park. The geyser-viewing area is the most accessible and visitor-friendly in the park with bench seating, a large parking lot, and a ranger station that tracks the time, height and length of an eruption to predict the next eruption.

65

Fountain Paint Pot

Along Fountain Paint Pot Trail you will see various hydrothermal features that are expressions of Yellowstone’s still active volcano. Within this geologic system, each type of thermal feature is represented. They can be grouped into two general categories—those with a great deal of water (hot springs and geysers) and those with limited water (mudpots and fumaroles). Despite their structural similarities, no two features are exactly alike.

66

Grand Prismatic Spring

Grand Prismatic Spring is located in the Midway Geyser Basin. It has the distinction of being the park's largest hot spring. It measures approximately 370 feet (112.8 m) in diameter and is over 121 feet (37 m ) deep. A description of this spring by fur trapper Osborne Russell in 1839 also makes it the earliest described thermal feature in Yellowstone that is definitely identifiable.

67

Yellowstone Lake

Situated at 7,733 feet (2,357 m) above sea level, Yellowstone Lake is the largest high elevation lake (above 7,000 feet / 2,134 m) in North America. It is roughly 20 miles (32.2 km) long and 14 miles (22.5 km) wide, with 141 miles (227 km) of shoreline and a surface area of 132 square miles (342 km2). Yellowstone Lake freezes over completely every winter in late December or early January, with ice thicknesses varying from a few inches to more than two feet. The lake usually thaws in late May or early June. Yellowstone Lake remains cold year-round, with an average water temperature of 41°F (5°C). Because of the extremely cold water, swimming is not recommended. Survival time is estimated to be only 20 to 30 minutes in water at this temperature.

68

Yellowstone Geysers - Mud Volcano Area

Yellowstone itself is a volcano, and one of its most spectacular eruptions occurred 640,000 years ago. During the eruption, the land collapsed and left a large depression in the earth—the Yellowstone Caldera. This caldera filled with lava flows over hundreds and thousands of years creating the volcanic plateau that comprises much of the central part of the park. Here at Mud Volcano you are close to one of the resurgent domes. The hills you see east of here comprise Sour Creek Dome. Resurgent domes are areas of active ground deformation, where the land moves up or down with the fluctuation of the magma chamber below. Scientists monitor these domes closely for information about ongoing volcanic activity. Not surprisingly, many of the park’s geysers, hot springs, mudpots, and fumaroles are also found near or within the caldera.

69

Grand Canyon of the Yellowstone

The Grand Canyon of the Yellowstone River expresses the park's complex geologic history in dramatic colors and shapes. Puffs of steam mark hydrothermal features in the canyon's walls. The Upper and Lower Falls of the Yellowstone River add to the grandeur of the unique natural treasure.

70

Hayden Valley

Hayden Valley is a large, sub-alpine valley in Yellowstone National Park straddling the Yellowstone River between Yellowstone Falls and Yellowstone Lake. The valley floor along the river is an ancient lake bed from a time when Yellowstone Lake was much larger.

71

Firehole Canyon Drive

Firehole Canyon Drive is a 2-mile, one-way road off the Grand Loop south of Madison. The drive has a waterfall overlook and swimming area.

72

Norris Geyser Basin

Norris Geyser Basin is the hottest and most changeable thermal area in Yellowstone. We will explore many of the features you would see if you walked the 2 1/4 miles (3.6 km) of trails. Discover the location of the world's tallest active geyser, colorful hot springs, and microscopic life in one of the most extreme environments on earth.

73

Gibbon Falls

Gibbon Falls drops 84 feet (0.3 m) over a remnant of the Yellowstone caldera rim. The caldera was created by a massive volcanic eruption approximately 640,000 years ago. A quick stop on our drive of the lower loop, this is a great opportunity for a photo moment.

74

Old Faithful

Old Faithful is located in Yellowstone’s Upper Geyser Basin in the southwest section of the park. The geyser-viewing area is the most accessible and visitor-friendly in the park with bench seating, a large parking lot, and a ranger station that tracks the time, height and length of an eruption to predict the next eruption.

75

Fountain Paint Pot

Along Fountain Paint Pot Trail you will see various hydrothermal features that are expressions of Yellowstone’s still active volcano. Within this geologic system, each type of thermal feature is represented. They can be grouped into two general categories—those with a great deal of water (hot springs and geysers) and those with limited water (mudpots and fumaroles). Despite their structural similarities, no two features are exactly alike.

76

Grand Prismatic Spring

Grand Prismatic Spring is located in the Midway Geyser Basin. It has the distinction of being the park's largest hot spring. It measures approximately 370 feet (112.8 m) in diameter and is over 121 feet (37 m ) deep. A description of this spring by fur trapper Osborne Russell in 1839 also makes it the earliest described thermal feature in Yellowstone that is definitely identifiable.

77

Yellowstone Lake

Situated at 7,733 feet (2,357 m) above sea level, Yellowstone Lake is the largest high elevation lake (above 7,000 feet / 2,134 m) in North America. It is roughly 20 miles (32.2 km) long and 14 miles (22.5 km) wide, with 141 miles (227 km) of shoreline and a surface area of 132 square miles (342 km2). Yellowstone Lake freezes over completely every winter in late December or early January, with ice thicknesses varying from a few inches to more than two feet. The lake usually thaws in late May or early June. Yellowstone Lake remains cold year-round, with an average water temperature of 41°F (5°C). Because of the extremely cold water, swimming is not recommended. Survival time is estimated to be only 20 to 30 minutes in water at this temperature.

78

Yellowstone Geysers - Mud Volcano Area

Yellowstone itself is a volcano, and one of its most spectacular eruptions occurred 640,000 years ago. During the eruption, the land collapsed and left a large depression in the earth—the Yellowstone Caldera. This caldera filled with lava flows over hundreds and thousands of years creating the volcanic plateau that comprises much of the central part of the park. Here at Mud Volcano you are close to one of the resurgent domes. The hills you see east of here comprise Sour Creek Dome. Resurgent domes are areas of active ground deformation, where the land moves up or down with the fluctuation of the magma chamber below. Scientists monitor these domes closely for information about ongoing volcanic activity. Not surprisingly, many of the park’s geysers, hot springs, mudpots, and fumaroles are also found near or within the caldera.

79

Grand Canyon of the Yellowstone

The Grand Canyon of the Yellowstone River expresses the park's complex geologic history in dramatic colors and shapes. Puffs of steam mark hydrothermal features in the canyon's walls. The Upper and Lower Falls of the Yellowstone River add to the grandeur of the unique natural treasure.

80

Hayden Valley

Hayden Valley is a large, sub-alpine valley in Yellowstone National Park straddling the Yellowstone River between Yellowstone Falls and Yellowstone Lake. The valley floor along the river is an ancient lake bed from a time when Yellowstone Lake was much larger.

81

Firehole Canyon Drive

Firehole Canyon Drive is a 2-mile, one-way road off the Grand Loop south of Madison. The drive has a waterfall overlook and swimming area.

82

Norris Geyser Basin

Norris Geyser Basin is the hottest and most changeable thermal area in Yellowstone. We will explore many of the features you would see if you walked the 2 1/4 miles (3.6 km) of trails. Discover the location of the world's tallest active geyser, colorful hot springs, and microscopic life in one of the most extreme environments on earth.

83

Gibbon Falls

Gibbon Falls drops 84 feet (0.3 m) over a remnant of the Yellowstone caldera rim. The caldera was created by a massive volcanic eruption approximately 640,000 years ago. A quick stop on our drive of the lower loop, this is a great opportunity for a photo moment.

84

Old Faithful

Old Faithful is located in Yellowstone’s Upper Geyser Basin in the southwest section of the park. The geyser-viewing area is the most accessible and visitor-friendly in the park with bench seating, a large parking lot, and a ranger station that tracks the time, height and length of an eruption to predict the next eruption.

85

Fountain Paint Pot

Along Fountain Paint Pot Trail you will see various hydrothermal features that are expressions of Yellowstone’s still active volcano. Within this geologic system, each type of thermal feature is represented. They can be grouped into two general categories—those with a great deal of water (hot springs and geysers) and those with limited water (mudpots and fumaroles). Despite their structural similarities, no two features are exactly alike.

86

Grand Prismatic Spring

Grand Prismatic Spring is located in the Midway Geyser Basin. It has the distinction of being the park's largest hot spring. It measures approximately 370 feet (112.8 m) in diameter and is over 121 feet (37 m ) deep. A description of this spring by fur trapper Osborne Russell in 1839 also makes it the earliest described thermal feature in Yellowstone that is definitely identifiable.

87

Yellowstone Lake

Situated at 7,733 feet (2,357 m) above sea level, Yellowstone Lake is the largest high elevation lake (above 7,000 feet / 2,134 m) in North America. It is roughly 20 miles (32.2 km) long and 14 miles (22.5 km) wide, with 141 miles (227 km) of shoreline and a surface area of 132 square miles (342 km2). Yellowstone Lake freezes over completely every winter in late December or early January, with ice thicknesses varying from a few inches to more than two feet. The lake usually thaws in late May or early June. Yellowstone Lake remains cold year-round, with an average water temperature of 41°F (5°C). Because of the extremely cold water, swimming is not recommended. Survival time is estimated to be only 20 to 30 minutes in water at this temperature.

88

Yellowstone Geysers - Mud Volcano Area

Yellowstone itself is a volcano, and one of its most spectacular eruptions occurred 640,000 years ago. During the eruption, the land collapsed and left a large depression in the earth—the Yellowstone Caldera. This caldera filled with lava flows over hundreds and thousands of years creating the volcanic plateau that comprises much of the central part of the park. Here at Mud Volcano you are close to one of the resurgent domes. The hills you see east of here comprise Sour Creek Dome. Resurgent domes are areas of active ground deformation, where the land moves up or down with the fluctuation of the magma chamber below. Scientists monitor these domes closely for information about ongoing volcanic activity. Not surprisingly, many of the park’s geysers, hot springs, mudpots, and fumaroles are also found near or within the caldera.

89

Grand Canyon of the Yellowstone

The Grand Canyon of the Yellowstone River expresses the park's complex geologic history in dramatic colors and shapes. Puffs of steam mark hydrothermal features in the canyon's walls. The Upper and Lower Falls of the Yellowstone River add to the grandeur of the unique natural treasure.

90

Hayden Valley

Hayden Valley is a large, sub-alpine valley in Yellowstone National Park straddling the Yellowstone River between Yellowstone Falls and Yellowstone Lake. The valley floor along the river is an ancient lake bed from a time when Yellowstone Lake was much larger.

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