Adventure Magazine

Stephen Watts

I'm a bestselling author who has been roaming the world for over a decade. Let me help you plan your trip of a lifetime!

Grand Teton National Park Wildlife Spotting

The Edition of April, 1901 of the USGS 1:125,000 quadrangle map of the area shows “Grand Teton” as the name of the peak. A United...

Grand Teton’s name was first recorded as Mount Hayden by the Washburn-Langford-Doane Expedition of 1870. However, the name “the Grand Teton” had early currency.

The Edition of April, 1901 of the USGS 1:125,000 quadrangle map of the area shows “Grand Teton” as the name of the peak. A United States National Park named “Grand Teton National Park” was established by law in 1929. By 1931, the name Grand Teton Peak was in such common usage that it was recognized by the USGS Board on Geographic Names. Another shift in usage led the Board to shorten the name on maps to Grand Teton in 1970.

The whole bison family is greeting us

The origin of the name is disputed. The most common explanation is that “Grand Teton” means “large teat” or “large nipple” in French, named by either French-Canadian or Iroquois members of an expedition led by Donald McKenzie of the North West Company.

However, other historians disagree, and claim that the mountain was named after the Teton Sioux tribe of Native Americans.

Wikipedia

There is a disagreement over who first climbed Grand Teton. Nathaniel P. Langford and James Stevenson claimed to have reached the summit on July 29, 1872. However, some believe their description and sketches match the summit of The Enclosure, a side peak of Grand Teton. The Enclosure is named after a man-made palisade of rocks on its summit, probably constructed by Native Americans. Mountaineer and author Fred Beckey believes that the two climbed the Enclosure because their description matches it, because their description does not accurately describe the true summit, because their account does not mention the formidable difficulties found just above the Upper Saddle, and finally, because it was traditional with members of the Hayden Geological Survey of 1871 to build a cairn in such a place, but no such cairn was found when William O. Owen reached the summit in 1898. In all likelihood, The Enclosure was first climbed by Native Americans as suggested by Langford in 1873. Supporters of Owen included The Wyoming Legislature and Paul Petzoldt, former pioneer American climber. Ironically among Langford’s supporters was Franklin Spalding, who led the ascent to the summit and tossed the rope that allowed Owen and the others to follow.

Bison is thinking about something

Mountaineer and author Leigh Ortenburger researched the controversy in depth, using original source material, for his 1965 climber’s guidebook.

Wikipedia

Ortenburger concluded: “Since historical ‘proof’ is extremely unlikely to be forthcoming for either side of the argument, perhaps the best way of regarding the problem, short of a detailed analysis of the probabilities, is to state that in 1872 Langford and Stevenson may have climbed the Grand Teton, in 1893 Kieffer, Newell, and Rhyan may have climbed it, and in 1898 Spalding, Owen, Peterson, and Shive definitely did succeed in reaching the summit.”

The Grand Teton has been skied by five routes, each requiring at least one rappel. The first descent on skis was made by Bill Briggs in the spring of 1971 down the East Face and Stettner Couloir, it has since been renamed the Briggs Route. This descent required a free rappel, which was completed with skis on. More casually, skiing is possible from the crest of the saddle between the Grand and the Middle Teton, continuously into the valley floor.

No Comments on Grand Teton National Park Wildlife Spotting

Observing Aurora Borealis in Norway

The resulting ionization and excitation of atmospheric constituents emits light of varying color and complexity. The form of the aurora, occurring within bands around both...

Auroras are produced when the magnetosphere is sufficiently disturbed by the solar wind that the trajectories of charged particles in both solar wind and magnetospheric plasma, mainly in the form of electrons and protons, precipitate them into the upper atmosphere (thermosphere/exosphere) due to Earth’s magnetic field, where their energy is lost.

The resulting ionization and excitation of atmospheric constituents emits light of varying color and complexity. The form of the aurora, occurring within bands around both polar regions, is also dependent on the amount of acceleration imparted to the precipitating particles. Precipitating protons generally produce optical emissions as incident hydrogen atoms after gaining electrons from the atmosphere. Proton auroras are usually observed at lower latitudes.

Tripod is essential if you want to take a great picture

Most auroras occur in a band known as the “auroral zone”, which is typically 3° to 6° wide in latitude and between 10° and 20° from the geomagnetic poles at all local times (or longitudes), most clearly seen at night against a dark sky. A region that currently displays an aurora is called the “auroral oval”, a band displaced towards the night side of the Earth. Early evidence for a geomagnetic connection comes from the statistics of auroral observations. Elias Loomis (1860), and later Hermann Fritz (1881) and S. Tromholt (1882) in more detail, established that the aurora appeared mainly in the auroral zone. Day-to-day positions of the auroral ovals are posted on the Internet.

In northern latitudes, the effect is known as the aurora borealis or the northern lights.

Wikipedia

The former term was coined by Galileo in 1619, from the Roman goddess of the dawn and the Greek name for the north wind. The southern counterpart, the aurora australis or the southern lights, has features almost identical to the aurora borealis and changes simultaneously with changes in the northern auroral zone. The Aurora Australis is visible from high southern latitudes in Antarctica, Chile, Argentina, New Zealand, and Australia.

The view on the Mountains and Aurora

Auroras also occur poleward of the auroral zone as either diffuse patches or arcs, which can be subvisual

Wikipedia

A geomagnetic storm causes the auroral ovals (north and south) to expand, and bring the aurora to lower latitudes. The instantaneous distribution of auroras (“auroral oval”) is slightly different, being centered about 3–5° nightward of the magnetic pole, so that auroral arcs reach furthest toward the equator when the magnetic pole in question is in between the observer and the Sun. The aurora can be seen best at this time, which is called magnetic midnight.

Auroras seen within the auroral oval may be directly overhead, but from farther away, they illuminate the poleward horizon as a greenish glow, or sometimes a faint red, as if the Sun were rising from an unusual direction. Auroras also occur poleward of the auroral zone as either diffuse patches or arcs, which can be subvisual.

No Comments on Observing Aurora Borealis in Norway

How to properly Research and Plan your next Adventure

Adventurous experiences create psychological arousal, which can be interpreted as negative (e.g. fear) or positive (e.g. flow). For some people, adventure becomes a major pursuit...

An adventure is an exciting experience that is typically a bold, sometimes risky, undertaking. Adventures may be activities with some potential for physical danger such as traveling, exploring, skydiving, mountain climbing, scuba diving, river rafting or participating in extreme sports.

Adventurous experiences create psychological arousal, which can be interpreted as negative (e.g. fear) or positive (e.g. flow). For some people, adventure becomes a major pursuit in and of itself. According to adventurer André Malraux, in his La Condition Humaine (1933), “If a man is not ready to risk his life, where is his dignity?”. Similarly, Helen Keller stated that “Life is either a daring adventure or nothing.”

Friends can help too

Some of the oldest and most widespread stories in the world are stories of adventure such as Homer’s The Odyssey

Wikipedia

Outdoor adventurous activities are typically undertaken for the purposes of recreation or excitement: examples are adventure racing and adventure tourism. Adventurous activities can also lead to gains in knowledge, such as those undertaken by explorers and pioneers – the British adventurer Jason Lewis, for example, uses adventures to draw global sustainability lessons from living within finite environmental constraints on expeditions to share with schoolchildren. Adventure education intentionally uses challenging experiences for learning.

The knight errant was the form the “adventure seeker” character took in the late Middle Ages.

Mapping the directions for trip to Norway

The adventure novel exhibits these “protagonist on adventurous journey” characteristics as do many popular feature films, such as Star Wars and Raiders of the Lost Ark.

Wikipedia

Adventure books may have the theme of the hero or main character going to face the wilderness or Mother Nature. Examples include books such as Hatchet or My Side of the Mountain. These books are less about “questing”, such as in mythology or other adventure novels, but more about surviving on their own, living off the land, gaining new experiences, and becoming closer to the natural world.

Many adventures are based on the idea of a quest: the hero goes off in pursuit of a reward, whether it be a skill, prize, or perhaps the safety of a person. On the way, the hero must overcome various obstacles. Mythologist Joseph Campbell discussed his notion of the monomyth in his book, The Hero with a Thousand Faces. Campbell proposed that the heroic mythological stories from culture to culture followed a similar underlying pattern, starting with the “call to adventure”, followed by a hazardous journey, and eventual triumph.

No Comments on How to properly Research and Plan your next Adventure

Monument Valley: Forgotten & Untold Stories

The area is part of the Colorado Plateau. The elevation of the valley floor ranges from 5,000 to 6,000 feet (1,500 to 1,800 m) above sea...

Monument Valley has been featured in many forms of media since the 1930s. Director John Ford used the location for a number of his best-known films and thus, in the words of critic Keith Phipps, “its five square miles have defined what decades of moviegoers think of when they imagine the American West.”

The area is part of the Colorado Plateau. The elevation of the valley floor ranges from 5,000 to 6,000 feet (1,500 to 1,800 m) above sea level. The floor is largely siltstone of the Cutler Group, or sand derived from it, deposited by the meandering rivers that carved the valley. The valley’s vivid red color comes from iron oxide exposed in the weathered siltstone. The darker, blue-gray rocks in the valley get their color from manganese oxide.

Road to gorgeous stone giants

The buttes are clearly stratified, with three principal layers. The lowest layer is the Organ Rock Shale, the middle is de Chelly Sandstone, and the top layer is the Moenkopi Formation capped by Shinarump Conglomerate

Wikipedia

Between 1945 and 1967, the southern extent of the Monument Upwarp was mined for uranium, which occurs in scattered areas of the Shinarump Conglomerate; vanadium and copper are associated with uranium in some deposits.

Monument Valley is officially a large area that includes much of the area surrounding Monument Valley Navajo Tribal Park, a Navajo Nation equivalent to a national park. Oljato, for example, is also within the area designated as Monument Valley.

Do you know the Monument Valley prophecy?

Visitors may pay an access fee and drive through the park on a 17-mile (27 km) dirt road (a 2-3 hour trip). Parts of Monument Valley, such as Mystery Valley and Hunts Mesa, are accessible only by guided tour.

Wikipedia

Monument Valley experiences a desert climate with cold winters and hot summers. While the summers may be hot, the heat is tempered by the region’s high altitude. Although the valley experiences an average of 54 days above 90 °F (32 °C) annually, summer highs rarely exceed 100 °F (38 °C). Summer nights are comfortably cool, and temperatures drop quickly after sunset. Winters are cold, but daytime highs are usually above freezing. Even in the winter, temperatures below 0 °F (−18 °C) are uncommon, though possible. Monument Valley receives an occasional light snowfall in the winter; however, it usually melts within a day or two.

No Comments on Monument Valley: Forgotten & Untold Stories

Type on the field below and hit Enter/Return to search