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86-414: Terrestrial refers to things related to land or the planet Earth , as opposed to extraterrestrial. Terrestrial may also refer to: Land Land , also known as dry land , ground , or earth , is the solid terrestrial surface of Earth not submerged by the ocean or another body of water . It makes up 29.2% of Earth's surface and includes all continents and islands . Earth's land surface

172-465: A cave . They have been important to humans as a place of shelter since the dawn of humanity. Craters are depressions in the ground, but unlike caves, they do not provide shelter or extend underground . There are many kinds of craters, such as impact craters , volcanic calderas , and isostatic depressions . Karst processes can create both solution caves , the most frequent cave type, and craters, as seen in karst sinkholes . The pedosphere

258-434: A habitat refers to the environment where a given species or population of organisms lives. Biomes may span more than one continent, and contain a variety of ecosystems and habitats. Land plants evolved from green algae , and are called embryophytes . They include trees , shrubs , ferns , grass , moss , and flowers . Most plants are vascular plants , meaning that their tissues distribute water and minerals throughout

344-623: A coastline may be impacted by the tides , caused by changes in gravitational forces on larger bodies of water. Coasts are important zones in natural ecosystems, often home to a wide range of biodiversity . On land, they harbour important ecosystems such as freshwater or estuarine wetlands , which are important for bird populations and other terrestrial animals. In wave-protected areas they harbor saltmarshes , mangroves or seagrasses , all of which can provide nursery habitat for finfish, shellfish , and other aquatic species. Rocky shores are usually found along exposed coasts and provide habitat for

430-588: A habitat for soil organisms , a recycling system for nutrients and organic wastes , a regulator of water quality , a modifier of atmospheric composition , and a medium for plant growth , making it a critically important provider of ecosystem services . Since soil has a tremendous range of available niches and habitats , it contains a prominent part of the Earth's genetic diversity . A gram of soil can contain billions of organisms, belonging to thousands of species, mostly microbial and largely still unexplored. Soil

516-455: A large area, it can influence climate and weather patterns. The terrain of a region largely determines its suitability for human settlement: flatter alluvial plains tend to have better farming soils than steeper, rockier uplands. Elevation is defined as the vertical distance between an object and sea level, while altitude is defined as the vertical distance from an object to Earth's surface. The elevation of Earth's land surface varies from

602-491: A large elevation difference between the highest and lowest points would be deemed "high relief". Most land has relatively low relief. The change in elevation between two points of the terrain is called a slope or gradient. A topographic map is a form of terrain cartography which depicts terrain in terms of its elevation, slope, and the orientation of its landforms. It has prominent contour lines , which connect points of similar elevation, while perpendicular slope lines point in

688-526: A long time to cause noticeable changes in the landscape—for example, the Grand Canyon was created over the past 70 million years by the Colorado River , which scientists estimate continues to erode the canyon at a rate of 0.3 meters (1 foot) every 200 years. However, humans have caused erosion to be 10–40 times faster than normal, causing half the topsoil of the surface of Earth's land to be lost within

774-518: A role in the regional and global climate. Densely populated cities are warmer and create urban heat islands that have effects on the precipitation, cloud cover , and temperature of the region. A landform is a natural or manmade land feature. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography . Landforms include hills , mountains , canyons , and valleys , as well as shoreline features such as bays , capes , and peninsulas . The shoreline

860-421: A set of practices called sustainable land management . A biome is an area "characterized by its vegetation, soil, climate, and wildlife ." There are five major types of biomes on land: grasslands, forests, deserts, tundras, and freshwater. Other types of biomes include shrublands, wetlands, and polar ice caps . An ecosystem refers to the interaction between organisms within a particular environment, and

946-746: A solid phase of minerals and organic matter (the soil matrix), as well as a porous phase that holds gases (the soil atmosphere) and water (the soil solution). Accordingly, soil is a three- state system of solids, liquids, and gases. Soil is a product of several factors: the influence of climate , relief (elevation, orientation, and slope of terrain), organisms, and the soil's parent materials (original minerals) interacting over time. It continually undergoes development by way of numerous physical, chemical and biological processes, which include weathering and erosion . Given its complexity and strong internal connectedness , soil ecologists regard soil as an ecosystem . Soil acts as an engineering medium,

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1032-455: A steady growth to the present-day forms or, more likely, a rapid growth early in Earth history followed by a long-term steady continental area. Continents are formed by plate tectonics , a process ultimately driven by the continuous loss of heat from the Earth's interior. On time scales lasting hundreds of millions of years, the supercontinents have formed and broken apart three times. Roughly 750  mya (million years ago), one of

1118-412: A valuable by-product. The sources of atmospheric water vapor are the bodies of water (oceans, seas, lakes, rivers, swamps), and vegetation on the planetary surface , which humidify the troposphere through the processes of evaporation and transpiration respectively, and which influences the occurrence of weather phenomena; the greatest proportion of water vapor is in the atmosphere nearest the surface of

1204-433: A wide range of sessile animals (e.g. mussels , starfish , barnacles ) and various kinds of seaweeds . Along tropical coasts with clear, nutrient-poor water, coral reefs can often be found between depths of 1–50 meters (3.3–164.0 feet). According to a United Nations atlas, 44% of all people live within 150 km (93 mi) of the sea. Because of their importance in society and high concentration of population,

1290-474: A year is equal to the energy radiated (lost) into outer space. The Earth's energy balance does not equally apply to each latitude because of the varying strength of the sunlight that strikes each of the three atmospheric cells, consequent to the inclination of the axis of planet Earth within its orbit of the Sun. The resultant atmospheric circulation transports warm tropical air to the geographic poles and cold polar air to

1376-442: Is a major component of the Earth's ecosystem. The world's ecosystems are impacted in far-reaching ways by the processes carried out in the soil, with effects ranging from ozone depletion and global warming to rainforest destruction and water pollution . With respect to Earth's carbon cycle , soil acts as an important carbon reservoir , and it is potentially one of the most reactive to human disturbance and climate change. As

1462-470: Is a reasonably sharp contrast between the more felsic upper continental crust and the lower continental crust, which is more mafic in character. The composition of land is not uniform across the Earth, varying between locations and between strata within the same location. The most prominent components of upper continental crust include silicon dioxide , aluminium oxide , and magnesium . The continental crust consists of lower density material such as

1548-599: Is almost entirely covered by regolith , a layer of rock , soil , and minerals that forms the outer part of the crust . Land plays an important role in Earth's climate system , being involved in the carbon cycle , nitrogen cycle , and water cycle . One-third of land is covered in trees, another third is used for agriculture , and one-tenth is covered in permanent snow and glaciers . The remainder consists of desert , savannah , and prairie . Land terrain varies greatly, consisting of mountains, deserts, plains, plateaus, glaciers, and other landforms . In physical geology,

1634-442: Is also used in wetland ecology, where "upland" plants indicate an area that is not a wetland. In addition, the term moorland refers to upland shrubland biomes with acidic soils, while heathlands are lowland shrublands with acidic soils. Geomorphology refers to the study of the natural processes that shape land's surface, creating landforms. Erosion and tectonics , volcanic eruptions , flooding , weathering , glaciation ,

1720-520: Is also used more generally, as in Persian rigestân ( ریگستان ) "place of sand, desert", golestân ( گلستان ) "place of flowers, garden", gurestân ( گورستان ) "graveyard, cemetery", and Hindustân ( هندوستان ) "land of the Indo people". The study of land and its history in general is called geography . Mineralogy is the study of minerals, and petrology is the study of rocks. Soil science

1806-488: Is an island , and a chain of islands is an archipelago . The smaller the island, the larger the percentage of its land area will be adjacent to the water, and subsequently will be coast or beach. Islands can be formed by a variety of processes. The Hawaiian islands , for example, even though they are not near a plate boundary, formed from isolated volcanic activity . Atolls are ring-shaped islands made of coral , created when subsidence causes an island to sink beneath

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1892-628: Is called the shoreline . The word land is derived from Old English , from the Proto-Germanic word * landą , "untilled land", and then the Proto-Indo-European * lendʰ- , especially in northern regions that were home to languages like Proto-Celtic and Proto-Slavic . Examples include Old Irish land , "land, plot, church building" and Old Irish ithlann , "threshing floor", and Old East Slavic ljadina "wasteland, weeds". A country or nation may be referred to as

1978-418: Is often defined as the solid, dry surface of Earth. The word land may also collectively refer the collective natural resources of Earth, including its land cover , rivers , shallow lakes , its biosphere , the lowest layer of the atmosphere ( troposphere ), groundwater reserves, and the physical results of human activity on land, such as architecture and agriculture. The boundary between land and sea

2064-459: Is pushed upwards, or subductional events, where Earth's crust is pushed into the mantle, causing the crust to melt, rise due to its low density, and solidify into hardened rock, thickening the crust. A plateau , also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side, creating steep cliffs or escarpments . Both volcanic activity such as

2150-768: Is the heat capacity ratio ( γ ≈ {\displaystyle \gamma \approx \,} 7 ⁄ 5 ) for air. The combination of the equation for the air pressure yields the dry adiabatic lapse rate : d T d z = − m g R γ − 1 γ = − 9.8 ∘ C / k m {\displaystyle {\frac {\,dT\,}{dz}}=-{\frac {\;mg\;}{R}}{\frac {\;\gamma \,-\,1\;}{\gamma }}=-9.8^{\circ }\mathrm {C/km} } . The environmental lapse rate ( d T / d z {\displaystyle dT/dz} ), at which temperature decreases with altitude, usually

2236-464: Is the atmospheric boundary layer between the troposphere and the stratosphere , and is located by measuring the changes in temperature relative to increased altitude in the troposphere and in the stratosphere. In the troposphere, the temperature of the air decreases at high altitude, however, in the stratosphere the air temperature initially is constant, and then increases with altitude. The increase of air temperature at stratospheric altitudes results from

2322-448: Is the interface between the land and the ocean . It migrates each day as tides rise and fall, and moves over long periods of time as sea levels change. The shore extends from the low tide line to the highest elevation that can be reached by storm waves, and the coast stretches out inland until the point where ocean-related features are no longer found. When land is in contact with bodies of water, it can be eroded. The weathering of

2408-479: Is the numeric difference between the temperature of the planetary surface and the temperature of the tropopause divided by the altitude. Functionally, the ELR equation assumes that the planetary atmosphere is static, that there is no mixing of the layers of air, either by vertical atmospheric convection or winds that could create turbulence. The difference in temperature derives from the planetary surface absorbing most of

2494-399: Is the outermost layer of Earth's continental surface and is composed of soil and subject to soil formation processes . Below it, the lithosphere encompasses both Earth's crust and the uppermost layer of the mantle . The lithosphere rests, or "floats", on top of the mantle below it via isostasy . Above the solid ground, the troposphere and humans' use of land can be considered layers of

2580-461: Is the study of soils, encompassing the sub-disciplines of pedology , which focuses on soil formation, and edaphology , which focuses on the relationship between soil and life. The earliest material found in the Solar System is dated to 4.5672 ± 0.0006  bya (billion years ago); therefore, the Earth itself must have been formed by accretion around this time. The formation and evolution of

2666-465: Is thicker than oceanic crust , and it is far more varied in terms of composition. About 31% of this continental crust is submerged in shallow water, forming continental shelves. Land provides many ecosystem services , such as mitigating climate change, regulating water supply through drainage basins and river systems, and supporting food production. Land resources are finite, which has led to regulations intended to safeguard these ecosystem services, and

Terrestrial - Misplaced Pages Continue

2752-406: Is unequal to the adiabatic lapse rate ( d S / d z ≠ 0 {\displaystyle dS/dz\neq 0} ). If the upper air is warmer than predicted by the adiabatic lapse rate ( d S / d z > 0 {\displaystyle dS/dz>0} ), then a rising and expanding parcel of air will arrive at the new altitude at a lower temperature than

2838-685: The Earth's magnetic field was established, which helped prevent the atmosphere from being stripped away by the solar wind . The atmosphere and oceans of the Earth continuously shape the land by eroding and transporting solids on the surface. Earth's crust formed when the molten outer layer of the planet Earth cooled to form a solid mass as the accumulated water vapour began to act in the atmosphere. Once land became capable of supporting life, biodiversity evolved over hundreds of millions of years, expanding continually except when punctuated by mass extinctions. The two models that explain land mass propose either

2924-523: The biosphere . Human manipulation of the land, including agriculture and architecture , can also be considered part of land. Land is formed from the continental crust , the layer of rock on which soil . groundwater , and human and animal activity sits. Though modern terrestrial plants and animals evolved from aquatic creatures, Earth's first cellular life likely originated on land. Survival on land relies on fresh water from rivers, streams, lakes, and glaciers, which constitute only three percent of

3010-507: The motherland , fatherland , or homeland of its people. Many countries and other places have names incorporating the suffix -land (e.g. England , Greenland , and New Zealand ). The equivalent suffix -stan from Indo-Iranian , ultimately derived from the Proto-Indo-Iranian * sthāna- , is also present in many country and location names, such as Pakistan , Afghanistan , and others throughout Central Asia . The suffix

3096-409: The ozone layer 's absorption and retention of the ultraviolet (UV) radiation that Earth receives from the Sun. The coldest layer of the atmosphere, where the temperature lapse rate changes from a positive rate (in the troposphere) to a negative rate (in the stratosphere) locates and identifies the tropopause as an inversion layer in which limited mixing of air layers occurs between the troposphere and

3182-434: The upwelling of magma and extrusion of lava, or erosion of mountains caused from water, glaciers, or aeolian processes, can create plateaus. Plateaus are classified according to their surrounding environment as intermontane , piedmont , or continental . A few plateaus may have a small flat top while others are wider. Buttes are smaller, with less extrusive and more intrusive igneous rock, while plateaus or highlands are

3268-648: The whale , that evolved from terrestrial mammals back to an aquatic lifestyle. Many megafauna of the past, such as non-avian dinosaurs , have become extinct due to extinction events, e.g. the Quaternary extinction event . Land is "deeply intertwined with human development." It is a crucial resource for human survival, humans depend on land for subsistence, and can develop strong symbolic attachments to it. Access to land can determine "survival and wealth," particularly in developing countries, giving rise to complex power relationships in production and consumption. Most of

3354-441: The Earth heats the troposphere by means of latent heat , thermal radiation , and sensible heat . The gas layers of the troposphere are less dense at the geographic poles and denser at the equator, where the average height of the tropical troposphere is 13 km, approximately 7.0 km greater than the 6.0 km average height of the polar troposphere at the geographic poles; therefore, surplus heating and vertical expansion of

3440-432: The Earth's crust. About 30 percent of land has a dry climate, due to losing more water through evaporation than it gains from precipitation . Since warm air rises, this generates winds, though Earth's rotation and uneven sun distribution also play a part. Land is commonly defined as the solid, dry surface of Earth. It can also refer to the collective natural resources that the land holds, including rivers , lakes , and

3526-433: The Earth. The temperature of the troposphere decreases at high altitude by way of the inversion layers that occur in the tropopause , which is the atmospheric boundary that demarcates the troposphere from the stratosphere . At higher altitudes, the low air-temperature consequently decreases the saturation vapor pressure , the amount of atmospheric water vapor in the upper troposphere. The maximum air pressure (weight of

Terrestrial - Misplaced Pages Continue

3612-579: The Solar System bodies occurred in tandem with the Sun. In theory, a solar nebula partitions a volume out of a molecular cloud by gravitational collapse, which begins to spin and flatten into a circumstellar disc , out of which the planets then grow (in tandem with the star). A nebula contains gas, ice grains and dust (including primordial nuclides ). In nebular theory , planetesimals begin to form as particulate matter accumulates by cohesive clumping and then by gravity. The primordial Earth's assembly took 10– 20  myr . By 4.54 ± 0.04 bya ,

3698-414: The air contains water vapor , then cooling of the air can cause the water to condense, and the air no longer functions as an ideal gas. If the air is at the saturation vapor pressure , then the rate at which temperature decreases with altitude is called the saturated adiabatic lapse rate . The actual rate at which the temperature decreases with altitude is the environmental lapse rate . In the troposphere,

3784-521: The air parcel; atmospheric compression and expansion are measured as an isentropic process ( d S = 0 {\displaystyle dS=0} ) wherein there occurs no change in entropy as the air parcel rises or falls within the atmosphere. Because the heat exchanged ( d Q = 0 {\displaystyle dQ=0} ) is related to the change in entropy ( d S {\displaystyle dS} by d Q = T d S {\displaystyle dQ=TdS} )

3870-413: The atmosphere) is at sea level and decreases at high altitude because the atmosphere is in hydrostatic equilibrium , wherein the air pressure is equal to the weight of the air above a given point on the planetary surface. The relation between decreased air pressure and high altitude can be equated to the density of a fluid, by way of the following hydrostatic equation: where: The planetary surface of

3956-431: The atmospheric pH by negligible amounts. Respiration from animals releases out of equilibrium carbonic acid and low levels of other ions. Combustion of hydrocarbons which is not a chemical reaction releases to atmosphere carbonic acid water as; saturates, condensates, vapour or gas (invisible steam). Combustion can releases particulates (carbon/soot and ash) as well as molecules forming nitrites and sulphites which will reduce

4042-410: The atmospheric pH of the water slightly or harmfully in highly industrialised areas where this is classed as air pollution and can create the phenomena of acid rain, a pH lower than the natural pH5.56. The negative effects of the by-products of combustion released into the atmospheric vapour can be removed by the use of scrubber towers and other physical means, the captured pollutants can be processed into

4128-552: The average environmental lapse rate is a decrease of about 6.5 °C for every 1.0 km (1,000m) of increased altitude. For dry air, an approximately ideal gas , the adiabatic equation is: p ( z ) [ T ( z ) ] − γ γ − 1 = constant {\displaystyle p(z){\Bigl [}T(z){\Bigr ]}^{-{\frac {\gamma }{\,\gamma \,-\,1\,}}}={\text{constant}}} wherein γ {\displaystyle \gamma }

4214-506: The climate change impacts on habitats and biodiversity, as well as natural resources, in the target areas. Land cover change detection and mapping is a key component of interdisciplinary land change science , which uses it to determine the consequences of land change on climate. Land change modeling is used to predict and analyze changes in land cover and use. Soil is a mixture of organic matter , minerals , gases , liquids , and organisms that together support life . Soil consists of

4300-636: The coast is important for major parts of the global food and economic system, and they provide many ecosystem services to humankind. For example, important human activities happen in port cities . Coastal fisheries for commercial, recreational, and subsistence purposes, and aquaculture are major economic activities and provide jobs, livelihoods, and protein for the majority of coastal human populations. Other coastal spaces like beaches and seaside resorts generate economic activity through tourism . Marine coastal ecosystems can also provide protection against sea level rise and tsunamis . In many countries,

4386-419: The coastal mangrove is the primary source of wood for fuel (e.g. charcoal) and building materials. Coastal ecosystems have a much higher capacity for carbon sequestration than many terrestrial ecosystems , and as such can play a critical role in the near future to help mitigate climate change effects by uptake of atmospheric anthropogenic carbon dioxide . A subcontinental area of land surrounded by water

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4472-580: The direction of the steepest slope. Hypsometric tints are colors placed between contour lines to indicate elevation relative to sea level . A difference between uplands, or highlands , and lowlands is drawn in several earth science fields. In river ecology, " upland " rivers are fast-moving and colder than "lowland" rivers, encouraging different species of fish and other aquatic wildlife to live in these habitats. For example, nutrients are more present in slow-moving lowland rivers, encouraging different species of macrophytes to grow there. The term "upland"

4558-981: The earliest known supercontinents, Rodinia , began to break apart. The continents later recombined to form Pannotia , 600– 540 mya , then finally Pangaea , which also broke apart 180 mya . A continuous area of land surrounded by an ocean is called a landmass. Although it is most often written as one word to distinguish it from the usage "land mass"—the measure of land area—it may also be written as two words. There are four major continuous landmasses on Earth: Afro-Eurasia , America (landmass) , Antarctica , and Australia (landmass) , which are subdivided into continents. Up to seven geographical regions are commonly regarded as continents. Ordered from greatest to least land area, these continents are Asia , Africa , North America , South America , Antarctica , Europe , and Australia . Terrain refers to an area of land and its features. Terrain affects travel, mapmaking, ecosystems, and surface water flow and distribution. Over

4644-420: The effect of the expansion of dry air as it rises in the atmosphere, and the wet adiabatic lapse rate (WALR) includes the effect of the condensation-rate of water vapor upon the environmental lapse rate. A parcel of air rises and expands because of the lower atmospheric pressure at high altitudes. The expansion of the air parcel pushes outwards against the surrounding air, and transfers energy (as work ) from

4730-404: The energy from the sun, which then radiates outwards and heats the troposphere (the first layer of the atmosphere of Earth) while the radiation of surface heat to the upper atmosphere results in the cooling of that layer of the atmosphere. The ELR equation also assumes that the atmosphere is static, but heated air becomes buoyant, expands, and rises. The dry adiabatic lapse rate (DALR) accounts for

4816-436: The equation governing the air temperature as a function of altitude for a mixed atmosphere is: d S d z = 0 {\displaystyle {\frac {\,dS\,}{dz}}=0} where S is the entropy. The isentropic equation states that atmospheric entropy does not change with altitude; the adiabatic lapse rate measures the rate at which temperature decreases with altitude under such conditions. If

4902-486: The geological continents and the areas of shallow seabed close to their shores, known as continental shelves . This layer is sometimes called sial because its bulk composition is richer in aluminium silicate and has a lower density compared to the oceanic crust , called sima which is richer in magnesium silicate . Changes in seismic wave velocities have shown that at a certain depth (the Conrad discontinuity ), there

4988-409: The growth of coral reefs , and meteorite impacts are among the processes that constantly reshape Earth's surface over geological time . Erosion transports one part of land to another via natural processes, such as wind , water, ice , and gravity . In contrast, weathering wears away rock and other solid land without transporting the land somewhere else. Natural erosional processes usually take

5074-402: The harvest of crops. Floodplains provided agricultural land for some of the earliest civilizations . Erosion is often a main driver for the creation of plains and valleys, with rift valleys being a noticeable exception. Fjords are glacial valleys that can be thousands of meters deep, opening out to the sea. Any natural void in the ground which can be entered by a human can be considered

5160-410: The heat loss. The parcel of air loses energy as it reaches greater altitude, which is manifested as a decrease in the temperature of the air mass. Analogously, the reverse process occurs within a cold parcel of air that is being compressed and is sinking to the planetary surface. The compression and the expansion of an air parcel are reversible phenomena in which energy is not transferred into or out of

5246-623: The igneous rocks granite and andesite . Less common is basalt , a denser volcanic rock that is the primary constituent of the ocean floors . Sedimentary rock is formed from the accumulation of sediment that becomes buried and compacted together . Nearly 75% of the continental surfaces are covered by sedimentary rocks, although they form about 5% of the crust. The most abundant silicate minerals on Earth's surface include quartz , feldspars , amphibole , mica , pyroxene and olivine . Common carbonate minerals include calcite (found in limestone ) and dolomite . The rock that makes up land

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5332-476: The land is divided into two major categories: Mountain ranges and relatively flat interiors called cratons . Both form over millions of years through plate tectonics . Streams – a major part of Earth's water cycle – shape the landscape , carve rocks, transport sediments, and replenish groundwater. At high elevations or latitudes , snow is compacted and recrystallized over hundreds or thousands of years to form glaciers, which can be so heavy that they warp

5418-489: The land will influence how much solar radiation reaches its surface. High latitudes receive less solar radiation than low latitudes. The land's topography is important in creating and transforming airflow and precipitation . Large landforms, such as mountain ranges, can divert wind energy and make air parcels less dense and therefore able to hold less heat. As air rises, this cooling effect causes condensation and precipitation. Different types of land cover will influence

5504-425: The land's albedo , a measure of the solar radiation that is reflected, rather than absorbed and transferred to Earth. Vegetation has a relatively low albedo, meaning that vegetated surfaces are good absorbers of the sun's energy. Forests have an albedo of 10–15 percent while grasslands have an albedo of 15–20 percent. In comparison, sandy deserts have an albedo of 25–40 percent. Land use by humans also plays

5590-705: The land. Land cover refers to the material physically present on the land surface, for example, woody crops, herbaceous crops, barren land, and shrub-covered areas. Artificial surfaces (including cities) account for about a third of a percent of all land. Land use refers to human allocation of land for various purposes, including farming, ranching, and recreation (e.g. national parks); worldwide, there are an estimated 16.7 million km (6.4 million sq mi) of cropland, and 33.5 million km (12.9 million sq mi) of pastureland. Land cover change detection using remote sensing and geospatial data provides baseline information for assessing

5676-460: The low point of −418 m (−1,371 ft) at the Dead Sea , to a maximum altitude of 8,848 m (29,029 ft) at the top of Mount Everest. The mean height of land above sea level is about 797 m (2,615 ft), with 98.9% of dry land situated above sea level. Relief refers to the difference in elevation within a landscape; for example, flat terrain would have "low relief", while terrain with

5762-441: The ocean surface and leaves a ring of reefs around it. Mountains are features that usually rise at least 300 metres (980 ft) higher than the surrounding terrain. The formation of mountain belts is called orogenesis, and results from plate tectonics . For example, where a plate at a convergent plate boundary pushes one plate above the other, mountains could be formed by either collisional events, such that Earth's crust

5848-402: The parcel of air to the atmosphere. Transferring energy to a parcel of air by way of heat is a slow and inefficient exchange of energy with the environment, which is an adiabatic process (no energy transfer by way of heat). As the rising parcel of air loses energy while it acts upon the surrounding atmosphere, no heat energy is transferred from the atmosphere to the air parcel to compensate for

5934-405: The past 150 years. Plate tectonics refers to the theory that Earth's lithosphere is divided into "tectonic plates" that move over the mantle. This results in continental drift , with continents moving relative to each other. The scientist Alfred Wegener first hypothesized the theory of continental drift in 1912. More researchers gradually developed his idea throughout the 20th century into

6020-426: The physical environment and may not be in this pH range.) Atmospheric water vapour holds suspended gasses in it (not by mass),78.08% nitrogen as N 2 , 20.95% oxygen as O 2 , 0.93% argon , trace gases, and variable amounts of condensing water (from saturated water vapor ). Any carbon dioxide released into the atmosphere from a pressurised source combines with the carbonic acid water vapour and momentarily reduces

6106-408: The planet warms, it has been predicted that soils will add carbon dioxide to the atmosphere due to increased biological activity at higher temperatures, a positive feedback (amplification). This prediction has, however, been questioned on consideration of more recent knowledge on soil carbon turnover. Continental crust is the layer of igneous , sedimentary , and metamorphic rocks that forms

6192-410: The planetary atmosphere of the Earth. The three-cell model of the atmosphere of the Earth describes the actual flow of the atmosphere with the tropical-latitude Hadley cell , the mid-latitude Ferrel cell , and the polar cell to describe the flow of energy and the circulation of the planetary atmosphere. Balance is the fundamental principle of the model — that the solar energy absorbed by the Earth in

6278-480: The planetary surface affects the flow of the air, and so forms the planetary boundary layer (PBL) that varies in height from hundreds of meters up to 2 km (1.2 mi; 6,600 ft). The measures of the PBL vary according to the latitude, the landform , and the time of day when the meteorological measurement is realized. Atop the troposphere is the tropopause , which is the functional atmospheric border that demarcates

6364-433: The plant. Through photosynthesis , most plants nourish themselves from sunlight and water, breathing in carbon dioxide and breathing out oxygen. Between 20 and 50% of oxygen is produced by land vegetation. Unlike plants, terrestrial animals are not a monophyletic group —that is, a group including all terrestrial animals does not encompass all lineages from a common ancestor . This is because there are organisms, such as

6450-441: The primordial Earth had formed. Earth's atmosphere and oceans were formed by volcanic activity and outgassing that included water vapour . The origin of the world's oceans was condensation augmented by water and ice delivered by asteroids , protoplanets , and comets . In this model , atmospheric " greenhouse gases " kept the oceans from freezing while the newly formed Sun was only at 70% luminosity . By 3.5 bya ,

6536-416: The stratosphere. The general flow of the atmosphere is from west to east, which, however, can be interrupted by polar flows, either north-to-south flow or a south-to-north flow, which meteorology describes as a zonal flow and as a meridional flow. The terms are used to describe localized areas of the atmosphere at a synoptic scale ; the three-cell model more fully explains the zonal and meridional flows of

6622-453: The surrounding air. In which case, the air parcel is denser than the surrounding air, and so falls back to its original altitude as an air mass that is stable against being lifted. If the upper air is cooler than predicted by the adiabatic lapse rate, then, when the air parcel rises to a new altitude, the air mass will have a higher temperature and a lower density than the surrounding air and will continue to accelerate and rise. The tropopause

6708-453: The tropics. The effect of the three cells is the tendency to the equilibrium of heat and moisture in the planetary atmosphere of Earth. A zonal flow regime is the meteorological term meaning that the general flow pattern is west to east along the Earth's latitude lines, with weak shortwaves embedded in the flow. The use of the word "zone" refers to the flow being along the Earth's latitudinal "zones". This pattern can buckle and thus become

6794-679: The tropopause. At the geographical poles , the Arctic and the Antarctic regions, the tropospheric temperature decreases from an average temperature of 0 °C (32 °F) at sea level to approximately −45 °C (−49 °F) at the tropopause. The temperature of the troposphere decreases with increased altitude, and the rate of decrease in air temperature is measured with the Environmental Lapse Rate ( − d T / d z {\displaystyle -dT/dz} ) which

6880-611: The troposphere from the stratosphere . As such, because the tropopause is an inversion layer in which air-temperature increases with altitude, the temperature of the tropopause remains constant. The layer has the largest concentration of nitrogen. The Earth's planetary atmosphere contains, besides other gases, water vapour and carbon dioxide, which produce carbonic acid in rain water , which therefore has an approximate natural pH of 5.0 to 5.5 (slightly acidic). (Water other than atmospheric water vapour fallen as fresh rain, such as fresh/sweet/potable/river water, will usually be affected by

6966-426: The troposphere occur in the tropical latitudes. At the middle latitudes, tropospheric temperatures decrease from an average temperature of 15 °C (59 °F) at sea level to approximately −55 °C (−67 °F) at the tropopause . At the equator , the tropospheric temperatures decrease from an average temperature of 20 °C (68 °F) at sea level to approximately −70 to −75 °C (−94 to −103 °F) at

7052-446: The water on Earth. The vast majority of human activity throughout history has occurred in habitable land areas supporting agriculture and various natural resources . In recent decades, scientists and policymakers have emphasized the need to manage land and its biosphere more sustainably, through measures such as restoring degraded soil , preserving biodiversity , protecting endangered species , and addressing climate change . Land

7138-701: The widely accepted theory of plate tectonics of today. Several key characteristics define modern understanding of plate tectonics. The place where two tectonic plates meet is called a plate boundary , with different geological phenomena occurring across different kinds of boundaries. For example, at divergent plate boundaries , seafloor spreading is usually seen, in contrast with the subduction zones of convergent or transform plate boundaries . Earthquakes and volcanic activity are common in all types of boundaries. Volcanic activity refers to any rupture in Earth's surface where magma escapes, therefore becoming lava . The Ring of Fire , containing two-thirds of

7224-512: The widest, and mesas are a general-sized plateau with horizontal bedrock strata . Wide, flat areas of land are called plains , which cover more than one-third of Earth's land area. When they occur as lowered areas between mountains, they can create valleys , canyons or gorges, and ravines . A plateau can be thought of as an elevated plain. Plains are known to have fertile soils and be important for agriculture due to their flatness supporting grasses suitable for livestock and facilitating

7310-462: The world's philosophies and religions recognize a human duty of stewardship towards land and nature. Troposphere The term troposphere derives from the Greek words tropos (rotating) and sphaira (sphere) indicating that rotational turbulence mixes the layers of air and so determines the structure and the phenomena of the troposphere. The rotational friction of the troposphere against

7396-459: The world's volcanos, and over 70% of Earth's seismological activity , comprises plate boundaries surrounding the Pacific Ocean . Earth's land interacts with and influences its climate heavily, since the land's surface heats up and cools down faster than air or water. Latitude , elevation , topography , reflectivity , and land use all have varying effects on climate. The latitude of

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