Introduction to Deserts

In this brief introduction we will discuss thethe Sierra Vicuna Mackenna. There are more than 20
geographical location of deserts, some of their maincactus species in the area, mainly of the genus
physical features, flora and fauna, effect on climateCopiapoa The Guanaco is the main mammal found
and human use.in the park. Other mammals include Culpeo Fox, Chilla
Main locations and types of DesertsFox and European Hare. The shoreline area is home
A desert is a landscape or region that receives anto marine mammals, such as the Marine Otter and
extremely low amount of precipitation, less thanthe South American Sea Lion. Among the birds are
enough to support growth of plants. Deserts arethe Humboldt Penguin and Peruvian Pelican. Also
defined as areas with an average annual precipitationreptile species of the genera Tropidurus and
of less than 250 millimetres (10 in) per year or asCallopistes inhabit the park.
areas where more water is lost byHuman Uses
evapotranspiration than falls as precipitation. DesertsMineral resources
are part of a wide classification of regions that, on anDeserts may contain great amount of mineral
average annual basis, have a moisture deficit (i.e. theyresources over their entire surface. This occurrence in
can potentially lose more than is received). Desertsminerals also determines the color. For example, the
are located where vegetation cover is sparse tored color of many sand deserts is a result of the
almost nonexistent and make up about one thirdoccurrence of laterite. .Some mineral deposits too
(33%) of the Earth's land surface. This briefare formed, improved, or preserved by geologic
introduction shall concentrate on hot deserts. Hotprocesses that occur in arid lands as a consequence
deserts usually have a large diurnal and seasonalof climate. Ground water leaches ore minerals and
temperature range, with high daytime temperatures,redeposits them in zones near the water table. This
and low nighttime temperatures (due to extremelyleaching process concentrates these minerals as ore
low humidity). In hot deserts the temperature in thethat can be mined. Evaporation in arid lands enriches
daytime can reach 45 °C/113 °F or higher in themineral accumulation in their lakes. Lake beds known
summer, and dip to 0 °C/32 °F or lower in theas playas may be sources of mineral deposits
winter. Dry desert air is incapable of blockingformed by evaporation. Water evaporating in closed
sunlight during the day or trapping heat during thebasins precipitates minerals such as gypsum, salts
night.(including sodium nitrate and sodium chloride), and
Thus, during daylight most of the sun's heat reachesborates.
the ground, and as soon as the sun sets the desertThe minerals formed in these evaporite deposits
cools quickly by radiating its heat into space. Urbandepend on the composition and temperature of the
areas in deserts lack large (more than 14 °C/25saline waters at the time of deposition. Significant
°F) daily temperature variations, partially due to theevaporite resources occur in the Great Basin
urban heat island effect. Many deserts are formedDesert of the United States, mineral deposits made
by rain shadows; mountains blocking the path offamous by the "20-mule teams" that once hauled
precipitation to the desert (on the lee side of theborax-laden wagons from Death Valley to the
mountain). Deserts are often composed of sand andrailroad. Boron, from borax and borate evaporites, is
rocky surfaces. Sand dunes called ergs and stonyan essential ingredient in the manufacture of glass,
surfaces called hamada. Exposures of rocky terrainenamel, agricultural chemicals, water softeners, and
are typical, and reflect minimal soil development andpharmaceuticals. Borates are mined from evaporite
sparseness of vegetation. The soil is rocky becausedeposits at Searles Lake, California, and other desert
of low chemical weathering. The largest hot desert islocations. The total value of chemicals that have been
the Sahara in northern Africa, covering 9 millionproduced from Searles Lake substantially exceeds
square kilometres and 12 countries. Other large hotUS$ 1 billion The Atacama Desert of Chile is unique
deserts include the Arabian Desert, Kalahari Desert,among the deserts of the world in its great
Great Victoria Desert, Great Basin Desert and theabundance of saline minerals. Sodium nitrate has been
Syrian Desert. Deserts are also classified by theirmined for explosives and fertilizer in the Atacama
geographical location and dominant weather patternsince the middle of the 19th century. Nearly 3 million
as trade wind, mid-latitude, rain shadow, coastal,metric tons were mined during World War 1. See our
monsoon, or polar deserts. Former desert areasgroup Chile Mining and Power on and our other mining
presently in non-arid environments are paleodesertsarticles on Articles Base.
e.g Nebraska Sand Hills. Montane deserts are aridValuable minerals located in arid lands include
places with a very high altitude; the most prominentcopper in the United States, Chile, Peru, and Iran,
example is found north of the Himalaya especially iniron and lead zinc ore in Australia; and gold, silver and
Ladakh region of Jammu and Kashmir, in parts of theuranium deposits in Australia and the United States.
Kunlun Mountains and the Tibetan Plateau.Nonmetalic mineral resources and rocks such
Many locations within this category have elevationsas beryllium, mica, lithium, clays, pumice,
exceeding 3,000 meters (10,000 ft) and the thermaland scoria also occur in arid regions. Sodium
regime can be hemiboreal. These places owe theircarbonate, sulfate, borate,nitrate,
profound aridity (the average annual precipitation islithium, bromine, iodine, calcium,
often less than 40 mm or 1.5 in) to being very farand strontium compounds come from sediments
from the nearest available sources of moisture.and near-surface brines formed by evaporation of
Montane deserts are normally cold. Rain shadowinland bodies of water, often during geologically
deserts form when tall mountain ranges block cloudsrecent times. The Green River
from reaching areas in the direction the wind is going.Formation of Colorado, Wyoming,
As the air moves over the mountains, it cools andand Utah contains alluvial fan deposits and playa
moisture condenses, causing precipitation on theevaporites created in a huge lake whose level
windward side. When that air reaches the leewardfluctuated for millions of years. Economically significant
side, it is dry because it has lost the majority of itsdeposits of trona, a major source
moisture, resulting in a desert. The air then warms,of sodium compounds, and thick layers of oil
expands, and blows across the desert. The warm,shale were created in the arid environment.
desiccated air takes with it any remaining moisture inSome of the more productive petroleum areas on
the desert. An example of a rain shadow desert isEarth are found in arid and semiarid regions of Africa
Death Valley which lies in the rain shadow of theand the Mideast, although the oil fields were
Pacific Coast Ranges of California and the Sierraoriginally formed in shallow marine environments.
Nevada Mountains.Recent climate change has placed these reservoirs in
Main Physical Featuresan arid environment. It's noteworthy that Ghawar,
Sand covers only about 20 percent of Earth'sthe world's largest and most productive oilfield is
deserts. Most of the sand is in sand sheets and sandmostly under theEmpty
seas—vast regions of undulating dunes. In general,Quarter and Al-Dahnadeserts. For more oil
there are six forms of deserts: 1) Mountain and basininformation please check out Other oil reservoirs,
deserts 2) Hamada deserts, which consist of plateauhowever, are presumed to be eolian in origin and
landforms 3) Regs, which consist of rock pavementsare presently found in humid environments.
4) Ergs, which are formed by sand seas 5)The Rotliegendes, a hydrocarbon reservoir in
Intermontane Basins and 6) Badlands, which arethe North Sea, is associated with extensive
located at the margins of arid lands comprisingevaporite deposits. Many of the major U.S.
clay-rich soil Nearly all desert surfaces are plainshydrocarbon resources may come from eolian sands.
where eolian deflation—removal of fine-grainedAncient alluvial fan sequences may also be
material by the wind—has exposed loose gravelshydrocarbon reservoirs.
consisting predominantly of pebbles but withSolar energy resources
occasional cobbles. The remaining surfaces of aridDeserts are increasingly seen as sources for solar
lands are composed of exposed bedrock outcrops,energy. The Negev Desert and the surrounding
desert soils, and fluvial deposits including alluvial fans,area, including the Arava Valley, are the sunniest
playas, desert lakes, and oases. Bedrock outcropsparts of Israel and little of this land is arable, which is
occur as small mountains surrounded by extensivewhy it has become the center of the Israeli solar
erosional plains. Several different types of dunesindustry. David Faiman, a world expert on solar
exist. Barchan dunes are produced by strong windsenergy, feels the energy needs of a country
blowing across a level surface and arelike Israel could be met by building solar energy
crescent-shaped. Longitudinal or seif dunes are dunesplants in the Negev. Faiman also feels the technology
that are parallel to a strong wind that blows in onenow exists to supply all of the world's electricity
general direction. Transverse dunes run at a rightneeds with 10 per cent of the Sahara. Solel has nine
angle to the constant wind direction. Star dunes arefields of solar collectors in the Mojave Desert of
star-shaped and have several ridges that spread outCalifornia  It recently signed a contract to build
around a point. Oases are vegetated areasthe Mojave Solar Park, which will be the world's
moistened by springs, wells or by irrigation. Many arelargest solar generating plant.
artificial. Oases are often the only places in desertsHuman life in deserts
that support crops and permanent habitation.A desert is a hostile, potentially deadly environment
Flora and Faunafor unprepared humans. In hot deserts, high
Deserts have a reputation for supporting very littletemperatures cause rapid loss of water due to
life, but in reality deserts often have high biodiversity,sweating, and the absence of water sources with
including animals that remain hidden during daylightwhich to replenish it can result in dehydration and
hours to control body temperature or to limitdeath within a few days. In addition, unprotected
moisture needs. Some fauna for example in thehumans are also at risk from heatstroke. Humans
Mojave desert includes the brush mouse, cactusmay also have to adapt to sandstorms in some
mouse, gray fox, porcupine, kangaroo rat, coyote,deserts, not just in their adverse effects
jack rabbit and many kinds of lizards. In the Australianon respiratory systems and eyes, but also in their
deserts we have the Bilby, Perentie, Thorny Devil,potentially harmful effects on equipment such
Bearded Dragon, Red Kangaroo and Dingo asas filters, vehicles and communication equipment.
examples. These animals adapted to live in desertsSandstorms can last for hours, sometimes even days.
are called xerocoles. Many desert animals (and plants)This makes surviving in the desert quite difficult for
show especially clear evolutionary adaptations forhumans. Despite this, some cultures have made hot
water conservation or heat tolerance, and so aredeserts their home for thousands of years, including
often studied in comparative physiology,the Bedouin, Tuareg and Pueblo people.
ecophysiology and evolutionary physiology.Modern technology, including
One well-studied example is the specializations ofadvanced irrigation systems, desalinization and air
mammalian kidneys shown by desert-inhabitingconditioning have made deserts much more
species. Many examples of convergenthospitable. In the United States and Israel for
evolution have been identified in desert organisms,example, desert farming has found extensive use
including between cacti and Euphorbia, kangaroo ratsand locations such as Las Vegas owe much to air
and jerboas, Phrynosoma and Moloch lizards. Someconditioning. In cold
flora includes shrubs, Prickly Pears, Desert Holly, anddeserts, hypothermia and frostbite are the chief
the Brittlebush. Most desert plants are drought- orhazards, as well as dehydration in the absence of a
salt-tolerant, such as xerophytes. Some store watersource of heat to melt ice for drinking. Falling through
in their leaves, roots, and stems. Other desert plantspack-ice or surface ice layers into freezing water is a
have long taproots that penetrate to the waterparticular danger requiring emergency action to
table if present, or have adapted to the weather byprevent rapid hypothermia. Starvation is also a
having wide-spreading roots to absorb water from ahazard; in low temperatures the body requires much
greater area of the ground. Another adaptation ismore food energy to maintain body heat and to
the development of small, spiny leaves which shedmove. As with hot deserts, some people such as
less moisture than deciduous leaves with greaterthe Inuit have adapted to the harsh conditions of
surface areas.cold deserts. Most traditional human life in deserts
The stems and leaves of some plants lower theis nomadic. It depends in hot deserts on finding
surface velocity of sand-carrying winds and protectwater, and on following infrequent rains to obtain
the ground from erosion. Even small fungi andgrazing for livestock. In cold deserts, it depends on
microscopic plant organisms found on the soil surfacefinding good hunting and fishing grounds, on sheltering
(so-called cryptobiotic soil) can be a vital link infrom blizzards and winter extremes, and on storing
preventing erosion and providing support for otherenough food for winter. Permanent settlement in
living organisms. Deserts typically have a plant coverboth kinds of deserts requires permanent water and
that is sparse but enormously diverse. The giantfood sources and adequate shelter, or the
saguaro cacti of the Sonoran Desert provide neststechnology and energy sources to provide it. Many
for desert birds and serve as "trees" of the desert.deserts are flat and featureless, lacking landmarks, or
Saguaro grow slowly but may live up to 200 years.composed of repeating landforms such as sand
When 9 years old, they are about 15 centimeters (6dunes or the jumbled ice-fields of glaciers. Advanced
in) high. After about 75 years, the cacti develop theirskills or devices are required to navigate through such
first branches. When fully grown, saguaro cacti are 15landscapes and inexperienced travellers may perish
meters tall and weigh as much as 10 tons. They dotwhen supplies run out after becoming lost. In addition
the Sonoran and reinforce the general impression ofsandstorms or blizzards may cause disorientation in
deserts as cactus-rich land. Although cacti are oftenseverely reduced visibility.
thought of as characteristic desert plants, otherThe danger represented by wild animals in deserts
types of plants have adapted well to the aridhas been featured in explorers' accounts but does
environment. They include the pea andnot cause higher rates of death than in other
sunflower families. Cold deserts have grasses andenvironments such as rain forests or savanna
shrubs as dominant vegetation.woodland, and generally does not by itself affect
Biodiversity Case Study - The Atacamahuman distribution. Defence against polar bears may
Atacama is the driest place on Earth and is virtuallybe advisable in some areas of the Arctic, as may
sterile because it is blocked from moisture on bothprecautions against venomous
sides by the Andes mountains and by the Chileansnakes and scorpions in choosing sites at which
Coastal Range. The cold Humboldt Current and theto camp in some hot deserts. However, it is hard to
anticyclone of the Pacific are essential to keep theoverestimate the importance of deserts in our
dry climate of the Atacama. The average rainfall incultural and historical background. Three of the
the Chilean region of Antofagasta is just 1 mm perWorld's largest religions Christianity, Islam and Judaism
year. Some weather stations in the Atacama havebegan and are set against a desert backdrop. All
never received rain. Evidence suggests that thethree religions are monotheistic, and today have
Atacama may not have had any significant rainfallenormous geopolitical influence extending far beyond
from 1570 to 1971. It is so arid that mountains thattheir area of origin -see articles on Christianity here
reach as high as 6,885 meters (22,590 feet) areon Articles Base and Biblon Deserts are also now a
completely free of glaciers and, in the southern partmajor source of tourism and travel interest e.g.
from 25°S to 27°S, may have been glacier-freeJoshua Tree, Death Valley National Parks as well as
throughout the Quaternary, thoughvital to the movie industry.
permafrost extends down to an altitude of 4,400Deserts are also vital areas for scientific interest. -
meters and is continuous above 5,600 meters.specific examples include Deep Canyon on the
Some locations in the Atacama do receive a marinewestern edge of the Colorado Desert is associated
fog known locally as the Camanchaca, providingwith the University of California, Riverside located in
sufficient moisture for hypolithic algae, lichens andthe P.L. Boyd Deep Canyon Desert Research Center.
even some cacti. But in the region that is in the "fogIt receives a variety of visiting scientists and
shadow" of the high coastal crest-line, whichstudents and, in addition to research, addresses
averages 3,000 metres (10,000 ft) m height forconservation issues of the surrounding environment
about 100 kilometres (60 mi) south of Antofagasta,such as the fate of the fringe-toed lizard. Another
the soil has been compared to that of Mars. Due todesert centre established by one visionary biologist,
its otherworldly appearance, the Atacama has beenthe Gobabeb Training and Research Centre, is located
used as a location for filming Mars scenes. The desertin Namibia within the driest part of the coastal Namib
was also primarily featured in the 2008 James BondDesert in the Namib-Naukluft Park. As the United
film Quantum of Solace. In 2003, a team ofNations Environment Program concludes "People have
researchers published a report in Sciencelived in deserts for millennia, as hunter-gatherers,
Magazine titled "Mars-like Soils in the Atacamaagriculturalists and pastoralists, and some people
Desert, Chile, and the Dry Limit of Microbial Life" incontinue to do so today. But other people now live in
which they duplicated the tests used by the Viking 1urban developments situated in deserts, or enjoy
and Viking 2 Mars landers to detect life, and weredeserts temporarily for tourism or recreation. Yet
unable to detect any signs in Atacama Desert soil.others are extracting profits from mining or other
The region may be unique on Earth in this regard andnon-renewable resources. Deserts are a large and
is being used by NASA to test instruments forprobably growing environment globally and their
future Mars missions. Let us take a closer look atfuture will be best supported if it is based on a
some of the biology of a particular region of thethorough understanding of their structure and
Atacama - the nearby Pan de Azucar National Park.function, and the influence of people's activities in the
Pan de Azúcar NP is divided into two ecosystems:past, present and future.
the coastal desert of Taltal and the steppe desert of