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Yardangs

ON THE SURFACE

Martian Fleets

(By Paul De Schutter)

НА ПОВЕРХНОСТИ
Марсианские Флоты
(Paul De Schutter)
http://ougseurope.org/rockon/surface/yardangs.asp
Atlas of the World's Deserts

Now that all our eyes are trained on Mars for the arrival of Beagle II as well as the NASA and Japanese missions, it seems appropriate to discuss a landform which can be found not only on Earth, but occurs extensively on Mars as well.

Since the disappearance of liquid water and volcanic activity at least 2 Ga ago, aeolian erosion is now the dominant mechanism of geomorphic change on Mars. One prominent landform which results from this aeolian acivity are yardangs.

Теперь, когда все наши глаза обучаются на Марсе для прибытия Гончей II так же как НАСА и японских миссий, кажется уместным обсудить очертания суши, которые могут быть найдены не только на Земле, но и происходят экстенсивно на Марсе также.

Начиная с исчезновения жидкой водной и вулканической деятельности по крайней мере 2 Ga назад, эолийская эрозия - теперь доминирующий механизм изменения geomorphic на Марсе. Видные очертания суши, которые следуют из этого эолийского acivity, являются ярданги.

Layered Yardangs
Слоистый ярданг в кратере Генри на Марсе. Layered Yardangs in Henry Crater on Mars. A Mars Global Surveyor image which shows yardangs in layered sedimentary rock on the northwestern floor of Henry Crater, an impact basin located at 11.7°N, 336.4°W. The image covers an area 2.3 km wide. (MGS MOC Release No. MOC2-389, 12 June 2003) Image credit: NASA/JPL/Malin Space Science Systems.

Yardangs are streamlined hills or ridges carved from any consolidated or semiconsolidated material – or, occasionally, bedrock – by wind erosion (aided by airborne dust and sand grains) and deflation (the removal of particles by wind). 
Ярданги - упрощенные холмы или горные хребты, вырезанные из любого объединенного, или полуобъединенного материала – или, иногда, основа – эрозией ветра (помогший бортовой пылью и зернами песка) и дефляция (удаление частиц ветром).

Yardangs range in size from a few centimetres to several kilometres long, and can be up to 30 metres high. Viewed from above, their shape resembles inverted boat hulls. They are highest and broadest at the end which faces the direction of the incoming wind, and become lower and narrower toward the lee end.

Abrasion is the pimary process which carves the windward side of a yardang, while deflation shapes the leeward side. Along the base of the flank of the yardang, especially the larger ones, a wind-scoured trough may occur, which indicates the densest part of the airborne sediment load.

The formation of yardangs usually begins with the downcutting of low areas, producing a series of parallel ridges which are gradually further eroded into separate hills. These hills are then shaped into the typical aerodynamic shape of a yardang, while the troughs separating the yardangs usually have a U-shaped cross section.

Thus most yardangs occur in fields — often called fleets, because of their resemblance to inverted ship hulls —, although occasionally they may be found in isolation. Within any one yardang fleet, the individual sizes tend to be fairly consistent.

The development of yardangs requires strong, persistent, almost unidirectional winds with an airborne sediment load of dust and sand grains. Wind speeds are highest along the flanks and top of the yardang where its cross-section is largest, while the flow towards the lee end tends to become turbulent.

Most yardang fields are found in arid, relatively sand-poor areas. On Earth, large yardangs occur in the arid regions of the Ica Valley of Peru, the Lut desert in Iran, southwestern Egypt and the Taklimakan Desert of northwest China. They have been observed in evaporites, siltstone, sandstone, shale, limestone and very occasionally even in crystalline rocks such as schist and gneiss. Yardangs may also be formed from the cemented core of a large dune which becomes exposed as the dune migrates.

Although the name yardang certainly conjures up images of visitors from a distant planet in a Star Wars movie, it is actually derived from the Turkish ‘yar’, meaning ‘steep bank’ and the Turkish-Mongol ‘yardang’ which means ‘dividing’.

By Paul De Schutter 


http://www.aapg.org/explorer/2001/06jun/el_baz.cfm

Sahara May Have Sparked Creations

Geology Inspires Desert Wonders?

 

Farouk El-Baz served as lead scientist for remote sensing in 1975 for the NASA-Soyuz mission, a joint effort between the United States and the Soviet Union.

Can he recall his emotion upon seeing those first images of his native Egypt from space?

"Yes. Disgust! Because I didn't understand them," he said.

El-Baz, an AAPG member who received the Michel T. Halbouty Award in 1996 for "outstanding application of geology to the benefit of human needs," is director of Boston University's Center for Remote Sensing. He holds degrees from Ain Shams University in Egypt, the Missouri School of Mines and Metallurgy and the University of Missouri. He has conducted research at the Massachusetts Institute of Technology and has taught at the University of Heidelberg.

"I thought I'd rubbed shoulders with the best geologists in the world, and was lucky to do so," he said. "Then I looked at the ground in my own country and I didn't understand it."

He's not bragging when he mentions his global activities. El-Baz' wide-ranging and far-flung experience includes studies of the four corners of the Earth, and beyond.

From 1967-72, he took part in NASA's Apollo program, serving as chairman of the Astronaut Training Group and secretary of the Landing Site Selection Committee for the Apollo missions to the moon.

He then joined the Smithsonian Institution in Washington, D.C., where he established the National Air and Space Museum's Center for Earth and Planetary Studies.

In 1979, El-Baz coordinated the first official visit by American scientists to deserts in northwestern China. As science advisor to the president of Egypt, he helped identify desert tracks for development in support of the country's growing population -- without damage to the environment.

The past 25 years have given El-Baz time to develop numerous theories about Egypt's mostly desert-covered expanse.

He outlined the most recent, and one of the most intriguing, in a recent issue of Archaeology magazine.

In his article "Pyramids and Sphinx: Gifts of the Desert," El-Baz identified the most likely models for those enduring monuments created by the ancient Egyptians:

Natural geologic forms found in the desert itself.

Weathering Heights

His theory begins with an understanding of the climate cycles alternating in Egypt since at least 500,000 years ago.

"It was really the alternation of wet and dry climates that shaped the features on the surface of the land," El-Baz said. "The last episode was very wet and ended 5,000 years ago."

More than shaping geology, the end of the favorable wet period shaped the course of Egyptian civilization, El-Baz believes. Desert nomads wandered east in search of water and swelled the population along the Nile River.

"The social organization, division of labor and increased land productivity to feed the whole lot would have resulted in a fertile ground for the development of a complex society," he wrote.

Earlier, rulers of individual towns began to extend their kingdoms, El-Baz said, and one king eventually united Upper and Lower Egypt around 3100 BC.

He said the development and accomplishments of the Egyptian Early Dynastic Period during the following 500 years has "no parallel in history."

Egypt's first pyramidal structure at Sakkara was built by Imhotep, architect of King Djoser, around 2780 BC, El-Baz noted. The famous Pyramids of Giza were completed just 125 years later.

An entry in El-Baz's own notebooks from 1978 led him to develop a theory about the pyramids' origins. In a brief note, he wondered if the early Egyptians had been inspired by the natural conical shapes of the desert.

Years of geological field trips to Egypt's Western Desert convinced him that was exactly the case.

El-Baz described this desert region as windblown terrain, 40 percent sand with fragments and pebbles on the surface.

Mostly crescent-shaped sand dunes dominate the landscape.

Of more interest to the petroleum industry, there are hints of sedimentary basins from 1.5-4 kilometers deep, as well as "a great deal of structural deformation, domes, arches, many faults," he said.

"In this whole western desert, the features are only sandstones and limestones," he said. "Once in a while you find a pile of shales, soft shale that has been shaped by the wind and survives."

Conical hills, many of them faceted, dot the deep desert.

"These appear to have developed from flat-topped or mesa-like elevations, which had separated from large escarpments that bounded the many depressions," El-Baz explained.

Over time, water erosion began to reduce the hills into pyramidal shapes. A conical or pyramidal form evades wind-erosion destruction by leading the wind upslope to dissipate at its apex, he said.

The desert people who emigrated to the settlements along the Nile took their memory of the shape and durability of those natural pyramids, according to El-Baz.

He compared Egypt's great pyramids to a public works initiative under the U.S. Work Projects Administration in the 1930s. "I think this was a kind of WPA project to unite the people of the north and south (Nile area)," he said.

Some movies may depict the workers who built the pyramids as slaves, whipped to exhaustion by cruel overlords, but El-Baz said they were more likely proud craftsmen carving out a stable life.

"Everybody who worked on the pyramid had a measure of beer and bread every day," he noted. "We know that because of messages they left behind: 'Not a day without beer and bread.'"

Secret of the Sphinx

The Great Sphinx might also reflect a natural form from the desert, El-Baz theorized.

Exploring the Taklimakan Desert in northwest China in the 1890s, Swedish explorer Sven Hedin encountered a strange landform of parallel ridges separated by gullies. His guides called the ridges yardang, from the Turkish word for "steep bank."

Numerous yardang exist in the Western Desert of Egypt, carved and shaped by the ever-blowing wind, El-Baz said. He described them as resembling inverted boat hulls with prows pointing into the wind.

The Sphinx-shapers may have started with a limestone yardang near the edge of the Giza plateau, El-Baz suggested.

They sculpted its upward protrusion into an image of their king, in a royal headcloth, and gave it a lion-like body conforming to the shape of the rock.

To complete the form, the ancient engineers had to dig a moat around the sculpture, El-Baz said. They then completed the lion with its characteristic, elongated legs.

To support his theory, El-Baz provided a photograph of a yardang with a protruding mass -- looking amazingly like a sphinx.

Ancient Egyptians had a deep understanding and knowledge of desert geology, as evidenced by their mines, quarries and excavations, he said. The oldest known map in the world is that of a gold mine between the Nile and the Red Sea, according to El-Baz.

To further understanding of desert geology, the Geological Society of America in 1999 created the Farouk El-Baz Desert Research Award.

Desert covers two-thirds of Egypt's 387,000 square miles, and he considers this an ideal area for study.

"It is a geological paradise because there is no vegetation," he said. "The features and the faults and the joints are clearly visible on the surface."

But the desert is not much studied, El-Baz observed, and he gave three possible reasons for that lack of interest:

  • Classical geology developed in Europe, where there are no deserts.
  • Deserts present a hostile environment.
    "Grad students like to study in cool areas," El Baz said, "in places where they can go out at night and have a glass of beer."
  • Geologists typically study rocks in situ.

"In the desert there are no rocks in situ. It's a mixture of fragments, rocks and sand," El-Baz said. "So in the desert, there's nothing for the classical geologist to do."

His own experience has convinced him that the desert rewards careful study. It also happens to be a wonderful area for remote sensing, with few clouds and no ground disturbance, he noted.

Even the great monuments of Egypt attest to what can be learned from an observation of desert geology, El-Baz said.

As for his theory published in Archaeology, it took more than 20 years from that fist note in his notebook until his thoughts about the pyramid builders finally sank in.

"No one had a theory about why this civilization developed when it did," he said. "When it sank in, I thought I'd tell it to the archaeologists."

 

http://www.scribd.com/doc/6528928/Atlas-of-the-Worlds-Deserts
http://www2.tu-berlin.de/~kehl/project/lv-twk/106-desert_types_wadis.htm
http://www2.tu-berlin.de/~kehl/project/lv-twk/10-Landscapes_A_SFB69-Kehl-Darius.htm

 

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