Adventure Magazine

Month: April 03, 2024

Finland Arctic Circle Expedition

Finland is the eighth-largest country in Europe and the most sparsely populated country in the European Union. It is a parliamentary republic with a central...

Finland’s population is 5.5 million (2017), and the majority of the population is concentrated in the southern region. 88.7% of the population is Finnish and speaks Finnish, a Uralic language unrelated to the Scandinavian languages; next come the Finland-Swedes (5.3%).

Finland is the eighth-largest country in Europe and the most sparsely populated country in the European Union. It is a parliamentary republic with a central government based in the capital city of Helsinki, local governments in 311 municipalities, and one autonomous region, the Åland Islands. Over 1.4 million people live in the Greater Helsinki metropolitan area, which produces one third of the country’s GDP.

Quadcopter did it’s job well in this Expedition

At the time Finland had three main cultural areas–Southwest Finland, Tavastia and Karelia–as reflected in contemporary jewellery

Wikipedia

Finland was inhabited when the last ice age ended, approximately 9000 BCE. The first settlers left behind artifacts that present characteristics shared with those found in Estonia, Russia, and Norway. The earliest people were hunter-gatherers, using stone tools. The first pottery appeared in 5200 BCE, when the Comb Ceramic culture was introduced. The arrival of the Corded Ware culture in southern coastal Finland between 3000 and 2500 BCE may have coincided with the start of agriculture. The Bronze Age and Iron Age were characterised by extensive contacts with other cultures in the Fennoscandian and Baltic regions and the sedentary farming inhabitation increased towards the end of Iron Age. At the time Finland had three main cultural areas–Southwest Finland, Tavastia and Karelia–as reflected in contemporary jewellery.

Nature is beautiful in Finland

Education is compulsory between the ages of 7 and 16. After lower secondary school, graduates may either enter the workforce directly, or apply to trade schools or gymnasiums (upper secondary schools)

Wikipedia

Most pre-tertiary education is arranged at municipal level. Even though many or most schools were started as private schools, today only around 3 percent of students are enrolled in private schools (mostly specialist language and international schools), much less than in Sweden and most other developed countries. Pre-school education is rare compared with other EU countries and formal education is usually started at the age of 7. Primary school takes normally six years and lower secondary school three years. Most schools are managed by municipal officials.

The flexible curriculum is set by the Ministry of Education and the Education Board. Education is compulsory between the ages of 7 and 16. After lower secondary school, graduates may either enter the workforce directly, or apply to trade schools or gymnasiums (upper secondary schools). Trade schools offer a vocational education: approximately 40% of an age group choose this path after the lower secondary school. Academically oriented gymnasiums have higher entrance requirements and specifically prepare for Abitur and tertiary education. Graduation from either formally qualifies for tertiary education.

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Into the Vortex: Science of Storm chasing

A person who chases storms is known as a storm chaser, or simply a chaser. While witnessing a tornado is the single biggest objective for...

Storm chasing is broadly defined as the pursuit of any severe weather condition, regardless of motive, which can be curiosity, adventure, scientific investigation, or for news or media coverage.

A person who chases storms is known as a storm chaser, or simply a chaser. While witnessing a tornado is the single biggest objective for most chasers, many chase thunderstorms and delight in viewing cumulonimbus and related cloud structures, watching a barrage of hail and lightning, and seeing what skyscapes unfold. There are also a smaller number of storm chasers who intercept tropical cyclones and waterspouts.

The superctell has formed

These can include the beauty of views afforded by the sky and land, the mystery of not knowing precisely what will unfold and the quest to undetermined destination on the open road, intangible experiences such as feeling one with a much larger and powerful natural world, the challenge of correctly forecasting and intercepting storms with the optimal vantage points, and pure thrill seeking. Pecuniary interests and competition may also be components; in contrast, camaraderie is common.

Storm chasing is chiefly a recreational endeavor, with motives usually given toward photographing or videoing the storm and for multivariate personal reasons.

Wikipedia

Although scientific work is sometimes cited as a goal, direct participation in such work is almost always impractical except for those collaborating in an organized university or government project. Many chasers also are storm spotters, reporting their observations of hazardous weather to relevant authorities. These reports greatly benefit real-time warnings with ground truth information as well as science by increasing the reliability of severe storm databases used in climatology and other research (which ultimately boosts forecast and warning skill). Additionally, many recreational chasers submit photos and videos to researchers as well as to the National Weather Service (NWS) for spotter training.

Mushroomhead Supercell Forming

Storm chasers are not generally paid to chase, with the exception of television media crews in certain television market areas, video stringers and photographers, and researchers such as a handful of graduate meteorologists and professors. An increasing number sell storm videos and pictures and manage to make a profit. A few operate “chase tour” services, making storm chasing a recently developed niche tourism. Financial returns usually are relatively meager given the expenses with most chasers spending more than they take in and very few making a living solely from chasing.

Storm chasers come from a wide variety of occupational and socioeconomic backgrounds

Wikipedia

No degree or certification is required to be a storm chaser. Local National Weather Service offices do hold storm spotter training classes, usually early in the spring. Some offices collaborate to produce severe weather workshops oriented toward operational meteorologists.

Storm chasers come from a wide variety of occupational and socioeconomic backgrounds. A fair number are meteorologists, however, most storm chasers may be from any number of occupational fields that have little or nothing to do with meteorology. A large majority of chasers are male and white but a minority are female or of Asian or other descents. The average age is probably around 35 but chasers could theoretically be of any age. A relatively high proportion possess college degrees and a large number live in the central and southern U.S. Many are lovers of nature with interests that also include flora, fauna, volcanoes, aurora, meteors, eclipses, and astronomy.

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The Story: Sands of time

The lack of vegetation exposes the unprotected surface of the ground to the processes of denudation. About one third of the land surface of the...

A desert is a barren area of landscape where little precipitation occurs and consequently living conditions are hostile for plant and animal life.

The lack of vegetation exposes the unprotected surface of the ground to the processes of denudation. About one third of the land surface of the world is arid or semi-arid. This includes much of the polar regions where little precipitation occurs and which are sometimes called polar deserts or “cold deserts”. Deserts can be classified by the amount of precipitation that falls, by the temperature that prevails, by the causes of desertification or by their geographical location.

Walking the hot sand can be challenging

Deserts are formed by weathering processes as large variations in temperature between day and night put strains on the rocks which consequently break in pieces.

Wikipedia

Although rain seldom occurs in deserts, there are occasional downpours that can result in flash floods. Rain falling on hot rocks can cause them to shatter and the resulting fragments and rubble strewn over the desert floor is further eroded by the wind. This picks up particles of sand and dust and wafts them aloft in sand or dust storms. Wind-blown sand grains striking any solid object in their path can abrade the surface. Rocks are smoothed down, and the wind sorts sand into uniform deposits. The grains end up as level sheets of sand or are piled high in billowing sand dunes. Other deserts are flat, stony plains where all the fine material has been blown away and the surface consists of a mosaic of smooth stones. These areas are known as desert pavements and little further erosion takes place. Other desert features include rock outcrops, exposed bedrock and clays once deposited by flowing water. Temporary lakes may form and salt pans may be left when waters evaporate. There may be underground sources of water in the form of springs and seepages from aquifers. Where these are found, oases can occur.

Watching the sunset

Plants and animals living in the desert need special adaptations to survive in the harsh environment

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Plants tend to be tough and wiry with small or no leaves, water-resistant cuticles and often spines to deter herbivory. Some annual plants germinate, bloom and die in the course of a few weeks after rainfall while other long-lived plants survive for years and have deep root systems able to tap underground moisture. Animals need to keep cool and find enough food and water to survive. Many are nocturnal and stay in the shade or underground during the heat of the day. They tend to be efficient at conserving water, extracting most of their needs from their food and concentrating their urine. Some animals remain in a state of dormancy for long periods, ready to become active again when the rare rains fall. They then reproduce rapidly while conditions are favorable before returning to dormancy.

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Spring Mountains National Recreation Area

Most land in the mountains is owned by the United States Forest Service and the Bureau of Land Management and managed as the Spring Mountains...

The Spring Mountains are a mountain range of southern Nevada in the United States, running generally northwest-southeast along the west side of Las Vegas and south to the border with California.

Most land in the mountains is owned by the United States Forest Service and the Bureau of Land Management and managed as the Spring Mountains National Recreation Area within the Humboldt-Toiyabe National Forest and the Red Rock Canyon National Conservation Area.

Our fifth yellow friend

The Spring Mountains range is named for the number of springs to be found, many of them in the recesses of Red Rock Canyon National Conservation Area, which is on the eastern side of the mountains

Wikipedia

The Spring Mountains divide the Pahrump Valley and Amargosa River basins from the Las Vegas Valley watershed, which drains into the Colorado River watershed, by way of Las Vegas Wash into Lake Mead, thus the mountains define part of the boundary of the Great Basin. The Great Basin Divide, (one of the Great Basin region borders) continues north through the Indian Springs Pass region, then turns due east at the perimeter mountain ranges north of Las Vegas.

The highest point is Mount Charleston (officially Charleston Peak), at 11,918 ft (3,633 m). The area around Mt. Charleston is protected in the Mount Charleston Wilderness. The area is typically 20-30°F (11-17°C) cooler than the valleys below, and it is a popular getaway for Las Vegas residents and visitors. The Lee Canyon (Ski and Snowboard Resort) lies in Lee Canyon on State Highway 156.

Spring mountains are breathtaking

In addition to Mount Charleston, other major summits in the Spring Mountains range include Bonanza Peak, McFarland Peak, Mummy Mountain, Griffith Peak, Bridge Mountain, Mount Wilson, and Mount Potosi.

Wikipedia

The Spring Mountains are a sky island ecosystem. With an area around 860 square miles (2,200 km2), and a vertical range of nearly 2 miles (3.2 km), the mountains encompass a wide variety of habitats, and the biological diversity is probably greater than anywhere else in Nevada; 37 species of trees are known (more than any other Nevadan range), and 600 species of vascular plants have been reported from the Red Rock Canyon National Conservation Area alone.

The bases of the mountains are part of the Mojave zone dominated by creosote bush and white bursage, then rising to a blackbush scrub zone, followed by a pygmy conifer zone with juniper, pinyon pine, and mountain mahogany, and topped by a montane zone with many species of conifers around Mt. Charleston and its connecting ridges.

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You Want to Climb Mount Everest? Here’s What It Takes

The current official elevation of 8,848 m (29,029 ft), recognised by China and Nepal, was established by a 1955 Indian survey and subsequently confirmed by a Chinese...

Mount Everest, known in Nepali as Sagarmāthā and in Tibetan as Chomolungma, is Earth’s highest mountain above sea level, located in the Mahalangur Himal sub-range of the Himalayas. The international border between China (Tibet Autonomous Region) and Nepal (Province No. 1) runs across its summit point.

The current official elevation of 8,848 m (29,029 ft), recognised by China and Nepal, was established by a 1955 Indian survey and subsequently confirmed by a Chinese survey in 1975. In 2005, China remeasured the rock height of the mountain, with a result of 8844.43 m. There followed an argument between China and Nepal as to whether the official height should be the rock height (8,844 m., China) or the snow height (8,848 m., Nepal). In 2010, an agreement was reached by both sides that the height of Everest is 8,848 m, and Nepal recognises China’s claim that the rock height of Everest is 8,844 m.

Pointer showed us the direction to mt. Everest

In 1865, Everest was given its official English name by the Royal Geographical Society, upon a recommendation by Andrew Waugh, the British Surveyor General of India

Wikipedia

As there appeared to be several different local names, Waugh chose to name the mountain after his predecessor in the post, Sir George Everest, despite George Everest’s objections.

Mount Everest attracts many climbers, some of them highly experienced mountaineers. There are two main climbing routes, one approaching the summit from the southeast in Nepal (known as the “standard route”) and the other from the north in Tibet. While not posing substantial technical climbing challenges on the standard route, Everest presents dangers such as altitude sickness, weather, and wind, as well as significant hazards from avalanches and the Khumbu Icefall. As of 2017, nearly 300 people have died on Everest, many of whose bodies remain on the mountain.

Melting glacier near mt. Everest

The first recorded efforts to reach Everest’s summit were made by British mountaineers. As Nepal did not allow foreigners into the country at the time, the British made several attempts on the north ridge route from the Tibetan side

Wikipedia

After the first reconnaissance expedition by the British in 1921 reached 7,000 m (22,970 ft) on the North Col, the 1922 expedition pushed the north ridge route up to 8,320 m (27,300 ft), marking the first time a human had climbed above 8,000 m (26,247 ft). Seven porters were killed in an avalanche on the descent from the North Col. The 1924 expedition resulted in one of the greatest mysteries on Everest to this day: George Mallory and Andrew Irvine made a final summit attempt on 8 June but never returned, sparking debate as to whether or not they were the first to reach the top. They had been spotted high on the mountain that day but disappeared in the clouds, never to be seen again, until Mallory’s body was found in 1999 at 8,155 m (26,755 ft) on the north face. Tenzing Norgay and Edmund Hillary made the first official ascent of Everest in 1953, using the southeast ridge route. Norgay had reached 8,595 m (28,199 ft) the previous year as a member of the 1952 Swiss expedition. The Chinese mountaineering team of Wang Fuzhou, Gonpo, and Qu Yinhua made the first reported ascent of the peak from the north ridge on 25 May 1960.

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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.

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