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 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, 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 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 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 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.

Definition

Land 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 is called the shoreline.

Etymology

The word ''land'' is derived from Old English, from the Proto-Germanic word , "untilled land", and then the Proto-Indo-European , 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 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 , is also present in many country and location names, such as Pakistan, Afghanistan, and others throughout Central Asia. The suffix is also used more generally, as in Persian () "place of sand, desert", () "place of flowers, garden", () "graveyard, cemetery", and '' Hindustân'' () "land of the Indo people".

Physical science

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 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.

Formation

The earliest material found in the Solar System is dated to (billion years ago); therefore, Earth itself must have been formed by accretion around this time. The formation and evolution of 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 the nebular hypothesis, planetesimals begin to form as particulate matter accumulates by cohesive clumping and then by gravity. The primordial Earth's assembly took 10–. By , 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 , 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 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 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 (million years ago), one of the earliest known supercontinents, Rodinia, began to break apart. The continents later recombined to form Pannotia, 600–, then finally Pangaea, which also broke apart .

Landmasses

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: Africa-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

Terrain refers to an area of land and its features. Terrain affects travel, mapmaking, ecosystems, and surface water flow and distribution. Over 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 the low point of at the Dead Sea, to a maximum altitude of at the top of Mount Everest. The mean height of land above sea level is about , 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 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 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" 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

Geomorphology refers to the study of the natural processes that shape land's surface, creating landforms. Erosion and tectonics, volcanic eruptions, flooding, weathering, glaciation, 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 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 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 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 developed his idea throughout the 20th century into the now widely accepted theory of plate tectonics.

Several key characteristics define the 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 the world's volcanos, and over 70% of Earth's seismological activity, comprises plate boundaries surrounding the Pacific Ocean.

Climate

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 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 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 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.

Features

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.

Coasts and islands

The shoreline 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 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 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 .

According to a United Nations atlas, 44% of all people live within of the sea. Because of their importance in society and high concentration of population, 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, 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 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 the ocean surface and leaves a ring of reefs around it.

Mountains and plateaus

Mountains are features that usually rise at least 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 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 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 the widest, and mesas are a general-sized plateau with horizontal bedrock strata.

Plains and valleys

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 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.

Caves and craters

Any natural void in the ground which can be entered by a human can be considered 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.

Layers

The pedosphere 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 the land.

Land cover

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 of cropland, and of pastureland.

Land cover change detection using remote sensing and geospatial data provides baseline information for assessing 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

Soil is a mixture of organic matter, minerals, gases, liquids, and organisms that together support life. Soil consists of 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, 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 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.{{cite journal , last1=Davidson , first1=Eric A. , last2=Janssens , first2=Ivan A. , year=2006 , title=Temperature sensitivity of soil carbon decomposition and feedbacks to climate change , url=https://www.nature.com/articles/nature04514.pdf , url-status=live , journal=Nature , volume=440 , issue=9 March 2006 , pages=165‒73 , bibcode=2006Natur.440..165D , doi=10.1038/nature04514 , pmid=16525463 , archive-url=https://web.archive.org/web/20220706182824/https://www.nature.com/articles/nature04514.pdf , archive-date=July 6, 2022 , access-date=April 3, 2022 , doi-access=free , s2cid=4404915 As 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

{{Main, Continental crust, Continental shelf
{{See also, Abundance of elements in Earth's crust

Continental crust is the layer of igneous, sedimentary, and metamorphic rocks that forms 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 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.{{Cite book , last1=Rudnick , first1=Roberta L. , url=https://www.sciencedirect.com/referencework/9780080983004/treatise-on-geochemistry , title=Treatise on Geochemistry , last2=Gao , first2=S. , publisher=Elsevier , year=2014 , isbn=978-0-08-098300-4 , editor1-last=Holland , editor1-first=Heinrich D. , editor1-link=Heinrich Holland , edition=2nd , volume=4: The Crust , pages=1–51 , chapter=Composition of the Continental Crust , author1-link=Roberta Rudnick , access-date=September 3, 2022 , editor2-last=Turekian , editor2-first=Karl K. , editor2-link=Karl Turekian , chapter-url=https://www.sciencedirect.com/science/article/pii/B9780080959757003016 , archive-url=https://web.archive.org/web/20220903010959/https://www.sciencedirect.com/referencework/9780080983004/treatise-on-geochemistry , archive-date=September 3, 2022 , url-status=live The continental crust consists of lower density material such as the igneous rocks granite and andesite. Less common is basalt, a denser volcanic rock that is the primary constituent of the ocean floors.{{cite web , author=Staff , title=Layers of the Earth , url=http://volcano.oregonstate.edu/vwdocs/vwlessons/plate_tectonics/part1.html , url-status=dead , archive-url=https://web.archive.org/web/20130211014443/http://volcano.oregonstate.edu/vwdocs/vwlessons/plate_tectonics/part1.html , archive-date=February 11, 2013 , access-date=March 11, 2007 , work=Volcano World , publisher=Oregon State University 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.{{cite web , last1=Jessey , first1=David , title=Weathering and Sedimentary Rocks , url=http://geology.csupomona.edu/drjessey/class/Gsc101/Weathering.html , url-status=dead , archive-url=https://web.archive.org/web/20070703170212/http://geology.csupomona.edu/drjessey/class/Gsc101/Weathering.html , archive-date=July 3, 2007 , access-date=March 20, 2007 , website=California State Polytechnic University, Pomona

The most abundant silicate minerals on Earth's surface include quartz, feldspars, amphibole, mica, pyroxene and olivine.{{cite book , last1=de Pater , first1=Imke , title=Planetary Sciences , last2=Lissauer , first2=Jack J. , date=2010 , publisher=Cambridge University Press , isbn=978-0-521-85371-2 , edition=2nd , page=154 , author1-link=Imke de Pater , author2-link=Jack J. Lissauer Common carbonate minerals include calcite (found in limestone) and dolomite.{{cite book , last1=Wenk , first1=Hans-Rudolf , title=Minerals: their constitution and origin , last2=Bulakh , first2=Andreĭ Glebovich , date=2004 , publisher=Cambridge University Press , isbn=978-0-521-52958-7 , page=359 , author1-link=Hans-Rudolf Wenk , author2-link=:ru:Булах, Андрей Глебович The rock that makes up land 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.

Life science

{{Main, Terrestrial ecosystem, Landscape ecology
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 a set of practices called sustainable land management.

Land biomes

{{Main, Biome

A biome is an area "characterized by its vegetation, soil, climate, and wildlife."{{Cite web , date=May 20, 2022 , title=The Five Major Types of Biomes {{! National Geographic Society , url=https://education.nationalgeographic.org/resource/five-major-types-biomes/ , access-date=October 4, 2022 , website= National Geographic , archive-date=October 8, 2022 , archive-url=https://web.archive.org/web/20221008074316/https://education.nationalgeographic.org/resource/five-major-types-biomes/ , url-status=live There are five major types of biomes on land: grasslands, forests, deserts, tundras, and freshwater. Other types of biomes include shrublands,{{efn, World Wildlife Fund's definition of 14 biomes includes Temperate grasslands, savannas and shrublands, Mediterranean forests, woodlands, and scrub, and Deserts and xeric shrublands.{{cite web , url=https://www.arcgis.com/apps/View/index.html?appid=d60ec415febb4874ac5e0960a6a2e448 , title=WWF Terrestrial Ecoregions Of The World (Biomes) , publisher= World Wildlife Fund , access-date=October 11, 2022 , archive-date=July 13, 2022 , archive-url=https://web.archive.org/web/20220713001111/https://www.arcgis.com/apps/View/index.html?appid=d60ec415febb4874ac5e0960a6a2e448 , url-status=live wetlands,{{efn, World Wildlife Fund's definition of 14 biomes includes Flooded grasslands and savannas, and Mangroves, which are both wetlands. and polar ice caps. An ecosystem refers to the interaction between organisms within a particular environment, and 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.

* Deserts have an arid climate, generally defined to mean that they receive less than {{convert, 25, cm, in of precipitation per year. They make up around one fifth of the Earth's land area, are found on every continent, and can be very hot or very cold (see polar desert). They are home to animals and plants which evolved to be tolerant of droughts. In deserts, most erosion is caused by running water, usually during violent thunderstorms, which cause flash floods. Deserts are expanding due to desertification, which is caused by excessive deforestation and overgrazing.{{Rp, pages=598–621
* Tundra is a biome where tree growth is hindered by frigid temperatures and short growing seasons. There are types of tundra associated with different regions: Arctic tundra, alpine tundra, and Antarctic tundra.{{cite web , title=The Tundra Biome , url=http://www.ucmp.berkeley.edu/glossary/gloss5/biome/tundra.html , url-status=live , archive-url=https://web.archive.org/web/20160121074551/http://www.ucmp.berkeley.edu/glossary/gloss5/biome/tundra.html , archive-date=January 21, 2016 , access-date=March 5, 2006 , work=The World's Biomes , publisher=University of California, Berkeley{{cite web , title=Terrestrial Ecoregions: Antarctica , url=http://www.nationalgeographic.com/wildworld/profiles/terrestrial_an.html , url-status=dead , archive-url=https://web.archive.org/web/20110805095438/http://www.nationalgeographic.com/wildworld/profiles/terrestrial_an.html , archive-date=August 5, 2011 , access-date=November 2, 2009 , work=Wild World , publisher=National Geographic Society
* A forest is an area of land dominated by trees. Many definitions of "forest" are used throughout the world, incorporating factors such as tree density, tree height, land use, legal standing, and ecological function. The United Nations' Food and Agriculture Organization (FAO) defines a forest as: "land spanning more than 0.5 hectares with trees higher than 5 meters and a canopy cover of more than 10 per cent, or trees able to reach these thresholds ''in situ''. It does not include land that is predominantly under agricultural or urban use."{{Cite book , url=http://www.fao.org/3/I8661EN/i8661en.pdf , title=Global Forest Resources Assessment 2020 – Terms and definitions , publisher=FAO , year=2018 , location=Rome , access-date=October 11, 2022 , archive-date=December 8, 2021 , archive-url=https://web.archive.org/web/20211208192636/https://www.fao.org/3/i8661en/i8661en.pdf , url-status=live Types of forests include rainforests, deciduous forests, and boreal forests.
* Grasslands are areas where the vegetation is dominated by grasses (Poaceae). However, sedge (Cyperaceae) and rush ( Juncaceae) can also be found, along with variable proportions of legumes like clover and other herbs. Grasslands occur naturally on all continents except Antarctica and are found in most ecoregions of the Earth. Furthermore, grasslands are one of the largest biomes on earth and dominate the landscape worldwide. Types include natural, semi-natural, and agricultural grasslands. Savannas are grasslands with occasional, scattered trees.

Fauna and flora

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 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 the whale, that evolved from terrestrial mammals back to an aquatic lifestyle.{{cite journal , last1=Garwood , first1=Russell J. , last2=Edgecombe , first2=Gregory D. , date=September 2011 , title=Early Terrestrial Animals, Evolution, and Uncertainty , journal=Evolution: Education and Outreach , location=New York , publisher=Springer Science+Business Media , volume=4 , issue=3 , pages=489–501 , doi=10.1007/s12052-011-0357-y , doi-access=free Many megafauna of the past, such as non-avian dinosaurs, have become extinct due to extinction events, e.g. the Quaternary extinction event.

Humans and land

Land is "deeply intertwined with human development."{{Rp, page=21 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 the world's philosophies and religions recognize a human duty of stewardship towards land and nature.

Culture

{{Main, Earth in culture

Many humans see land as a source of "spirituality, inspiration, and beauty." Many also derive a sense of belonging from land, especially if it also belonged to their ancestors. Various religions teach about a connection between humans and the land (such as veneration of Bhumi, a personification of the Earth in Hinduism, and the obligation to protect land as hima in Islam), and in almost every Indigenous group there are etiological stories about the land they live on. For Indigenous peoples, connection to the land is an important part of their identity and culture,{{cite web , url=http://www.un.org/development/desa/indigenouspeoples/wp-content/uploads/sites/19/2021/03/State-of-Worlds-Indigenous-Peoples-Vol-V-Final.pdf , title=State of the World's Indigenous Peoples, Volume V, Rights to Lands, Territories and Resources , author=United Nations Department of Economic and Social Affairs , access-date=October 20, 2022 and some religious groups consider a particular area of land to be sacred, such as the Holy Land in the Abrahamic religions.

Creation myths in many religions involve stories of the creation of the world by a supernatural deity or deities, including accounts wherein the land is separated from the oceans and the air. The Earth itself has often been personified as a deity, in particular a goddess. In many cultures, the mother goddess is also portrayed as a fertility deity. To the Aztecs, Earth was called '' Tonantzin''—"our mother"; to the Incas, Earth was called '' Pachamama''—"mother earth". In Norse mythology, the Earth giantess Jörð was the mother of Thor and the daughter of Annar. Ancient Egyptian mythology is different from that of other cultures because Earth ( Geb) is male and the sky ( Nut) is female.

Ancient Near Eastern cultures conceived of the world as a flat disk of land surrounded by ocean. The Pyramid Texts and Coffin Texts reveal that the ancient Egyptians believed Nun (the ocean) was a circular body surrounding ''nbwt'' (a term meaning "dry lands" or "islands"). The Hebrew Bible

HOME


Content is Copyleft
Website design, code, and AI is Copyrighted (c) 2014-2017 by Stephen Payne


Consider donating to Wikimedia



As an Amazon Associate I earn from qualifying purchases