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We consider TWO types of migrants: temporary migrants, who tend to make short TRIPS and then return to the area of ORIGIN, and PERMANENT migrants, who tend to move over longer distances with no intention to return.

Topography concerns with the SHAPE and character of the Earth's SURFACE, and maps were among the first artifacts to record these observationsExplanation:In modern mapping, a topographic map or topographic sheet is a type of map characterized by large-scale detail and quantitative representation of relief FEATURES, usually using contour lines (connecting POINTS of equal elevation), but HISTORICALLY using a variety of methods.

tion:Economic Factors Most of the studies INDICATE that migration is primarily motivated by economic factors. In developing countries, low AGRICULTURAL income, agricultural unemployment and UNDEREMPLOYMENT are considered BASIC factors pushing the migrants towards developed area with greater JOB opportunities.

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UTTERPRADESHExplanation:

The economic activity INVOLVING felling, hauling, logging of timber is KNOWN as lumbering. It is well developed in the coniferous forest belt of the cool temperate lands, because:  (ii) The land and rivers freeze which MAKES transportation of the logs easy. (III) The SPECIES of trees are few and the area is accessible.

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The Himalayas are a MOUNTAIN range in South ASIA, the highest in the world. The west end is in Pakistan. They run through Jammu and Kashmir, into the Republic of INDIA's Himachal Pradesh andUttaranchal states, Nepal, and the Kingdoms of Sikkim, and Bhutan. They end in the south of CHINA's Tibetan Autonomous Region........

Libya is a country that suffers from water scarcity. The situation has become more problematic due to continued population growth, low RAINFALL and higher water demand for agriculture and INDUSTRIAL use. ... Despite these efforts, the problem of water DEFICITS continues, due to EVER INCREASING water demands.

In geography, a plain is a flat, sweeping landmass that generally does not change much in ELEVATION. Plains OCCUR as lowlands along VALLEYS or on the doorsteps of MOUNTAINS, as coastal plains, and as plateaus or uplands. ... In a few instances, deserts and rainforests can also be plains.plz mark brainliest

Ocean islands are volcanic in nature.Explanation:The Pacific Ocean was originated by the Panthalassic Ocean by rifting APART of Rodinia.The islands are produced in the Pacific Ocean due to linear chains of volcanic islands.These islands rested above the plates .The oceanic PLATE of Pacific Ocean is CLOSE to the magmatic chamber of the earth.These islands are formed by :-mantle plumespropagating FRACTURE originuplifted coralline reefsfragments of crustsubducted PARTS of adjoining lithospheric platessubduction along convergent plate margin.

Hey!mplementation and associated organizational and social change that coexist in information SYSTEMS in developing countries (ISDC) research, namely as a process of technology and knowledge TRANSFER and adaptation to LOCAL social CONDITIONS; as a process of socially embedded action.hope it will be HELPFUL ✌️

The region which RECEIVE more than 200 CM of RAIN is Western COSTAL plains because it lies on windward side of Western ghats.Hope it helps you....

a, there is 14,500 NAVIGABLE land.Explanation:Inland waterway is a NETWORK of canals,rivers,etc. which can be used for transportation INSTEAD of roads and railways.In India,there is APPROXIMATELY 14,500km of navigable land.During the early times,Ganga was a BUSY network .But,in recent times its utility fell because of introduction of roadways and railwaysThe government has now revived the Ganga as the National Waterway 1(NW1).NW1 will ferry the cargo from eastern seaport Haldia to Varanasi,1620km  inland.

tion:The composition of Atmosphere is said to be a mixture of different gases. It envelops around the Earth. 99% of total mas of atmosphere is confined to highest of 32 KM from the Earth’s SURFACE.Atmosphere is consists of various gases, water vapour and dust particles.The presence of oxygen becomes negligible at the height of 120 km from the surface of earth with regards to the composition of atmosphere.Carbon dioxide and water vapour occur only upto 90 km.Carbon dioxide is meteorically very important as it is transparent to incoming solar radiation but opaque to outgoing terrestrial radiation. It is also responsible for greenhouse effect.Ozone GAS: 10-50 km above earth surface and acts as filter, absorbing ultraviolet rays from the sun. Ozone prevents the rays from reaching the surface of earth.Water vapour is variable gas, decreases with altitude.It also decreases from equator towards the poles.Acts like blanket allowing the earth to neither to become too cold nor too hot. Also contributes to the stability and instability in the air.Dust particles: are in higher concentration in subtropical and temperate regions due to dry WINDS in comparison to equatorial and polar regions.Dust particles act as a hygroscopic nuclei over which water vapour of atmosphere condenses to PRODUCE clouds.The composition of atmosphere varies with local environmental factors also.

Erosion, whether it is by water, wind or tillage, involves three DISTINCT actions – soil detachment, movement and DEPOSITION. Topsoil, which is high in organic matter, fertility and soil life, is relocated ELSEWHERE "on-site" where it builds up over time or is carried "off-site" where it fills in drainage channels.

te responsibility (CR)is concerned with the substainabiliity of an organisation over along term. Corporate responsibility seeks to add VALUE to an organisation's activities by ENSURING they have a positive IMPACT on society ,the ENVIRONMENT and the economy..........if it become helpful to you so mark as brainliest...................

The land absorbs much of the sun's energy as well. However, WATER heats up much more slowly than land and so the air above the land will be warmer compared to the air over the ocean. ... The SEA breeze strength will vary DEPENDING on the temperature difference between the land and the ocean. At night, the roles REVERSE.

अलंकार अलंकृति ; अलंकार : अलम् अर्थात् भूषण। जो भूषित करे वह अलंकार है। अलंकार, कविता-कामिनी के सौन्दर्य को बढ़ाने वाले तत्व होते हैं। जिस प्रकार आभूषण से नारी का लावण्य बढ़ जाता है, उसी प्रकार अलंकार से कविता की शोभा बढ़ जाती है(शब्द तथा अर्थ की जिस विशेषता से काव्य का श्रृंगार होता है उसे ही अलंकार कहते हैं) । कहा गया है - 'अलंकरोति इति अलंकारः' (जो अलंकृत करता है, वही अलंकार है।) भारतीय साहित्य में अनुप्रास, उपमा, रूपक, अनन्वय, यमक, श्लेष, उत्प्रेक्षा, संदेह, अतिशयोक्ति, वक्रोक्ति आदि प्रमुख अलंकार हैं। इसके अलावा अन्य अलंकार भी हैं।इस कारण व्युत्पत्ति से उपमा आदि अलंकार कहलाते हैं। उपमा आदि के लिए अलंकार शब्द का संकुचित अर्थ में प्रयोग किया गया है। व्यापक रूप में सौंदर्य मात्र को अलंकार कहते हैं और उसी से काव्य ग्रहण किया जाता है। (काव्यं ग्राह्ममलंकारात्। सौंदर्यमलंकार: - वामन)। चारुत्व को भी अलंकार कहते हैं। (टीका, व्यक्तिविवेक)। भामह के विचार से वक्रार्थविजा एक शब्दोक्ति अथवा शब्दार्थवैचित्र्य का नाम अलंकार है। (वक्राभिधेतशब्दोक्तिरिष्टा वाचामलं-कृति:।) रुद्रट अभिधानप्रकारविशेष को ही अलंकार कहते हैं। (अभिधानप्रकाशविशेषा एव चालंकारा:)। दंडी के लिए अलंकार काव्य के शोभाकर धर्म हैं (काव्यशोभाकरान् धर्मान् अलंकारान् प्रचक्षते)। सौंदर्य, चारुत्व, काव्यशोभाकर धर्म इन तीन रूपों में अलंकार शब्द का प्रयोग व्यापक अर्थ में हुआ है और शेष में शब्द तथा अर्थ के अनुप्रासोपमादि अलंकारों के संकुचित अर्थ में। एक में अलंकार काव्य के प्राणभूत तत्व के रूप में ग्रहीत हैं और दूसरे में सुसज्जितकर्ता के रूप में।विभावना अलंकार:- ज़हाँ कारण के बिना या कारण के विपरीत कार्य की उत्पति का वर्णन किया जाऐ, वहाँ विभावना अलंकार होता है।उदः- बिन पद चलै, सुने बिन काना,कर बिन करम करै विधि नाना ।

The four requirements of PRODUCTION of goods and services are LAND, labor, physical capital and HUMAN capital. Land is the physical place where all the ECONOMIC activity takes place. Land plays an important part in production because land itself and the resources on it are usually limitedExplanation:mark brainlistfollow me if U liked answer.

ntry has various tourist destinations at SWAT, Malam Jabba, Behrain, Kalam, Shangla, Balakot, Kaghan, Naran, Ayoubia, MURREE, Chitral, Gilgit BALTISTAN, HUNZA, and Neelam valleys, other mountainous ranges, and historical and archaeological sites. please mark as BRAINLIEST.....hope it helped

as OCCUPIED more LAND than BRAZIL.

An ephemeral RIVER is a river that only FLOWS when there is rain or snow has MELTED. The REST of the year there is just a dry river bed with no waterExplanation:

Soil Type: SandySandy soil has the largest particles AMONG the different soil types. It’s dry and gritty to the touch, and because the particles have huge spaces between them, it can’t hold on to water.Water drains rapidly, straight through to places where the roots, particularly those of seedlings, cannot reach. Plants don’t have a chance of using the nutrients in sandy soil more efficiently as they’re SWIFTLY carried away by the runoff.The upside to sandy soil is that it’s light to work with and warms much more quickly in the spring.Testing what type of soil you’re working with involves moistening the soil and rolling it into a ball to check the predominating soil particle. When you roll the slightly wet sandy soil in your palms, no ball should be formed and it crumbles through your fingers easily.2. Soil Type: SiltySilty soil has much smaller particles than sandy soil so it’s smooth to the touch. When moistened, it’s soapy slick. When you roll it between your fingers, dirt is left on your skin.Silty soil retains water longer, but it can’t hold on to as much nutrients as you’d want it to though it’s fairly fertile. Due to its moisture-retentive quality, silty soil is cold and drains poorly.Silty soil can also easily compact, so avoid trampling on it when working your garden. It can become poorly aerated, too.3. Soil Type: ClayClay soil has the smallest particles among the three so it has good water storage qualities. It’s sticky to the touch when wet, but smooth when dry.Due to the tiny size of its particles and its tendency to settle together, little air passes through its spaces. Because it’s also slower to drain, it has a tighter hold on plant nutrients. CLAY soil is thus rich in plant food for better growth.Clay soil is cold and in the spring, takes time to warm since the water within also has to warm up. The downside is that clay soil could be very heavy to work with when it gets dry. Especially during the summer months, it could turn hard and compact, making it difficult to turn. (When clay soil is worked while it’s too wet though, it’s prone to damage).If moistened soil feels sticky, rolls up easily, and forms into a ball or sausage-like shape, then you’ve got yourself clay.4. Soil Type: PeatyPeaty soil is dark brown or black in color, soft, easily compressed due to its high water content, and rich in organic matter. Peat soil started forming over 9,000 years ago, with the rapid melting of glaciers. This rapid melt drowned plants quickly and died in the process. Their decay was so slow underwater that it led to the accumulation of organic area in a concentrated spot.Although peat soil tends to be heavily saturated with water, once drained, it turns into a good growing medium. In the summer though, peat could be very dry and become a fire hazard. (I kid you not—peat is the precursor of coal.) The most desirable quality of peat soil, however, is in its ability to hold water in during the dry months and its capacity to protect the roots from damage during very wet months.Peat contains acidic water, but growers use it to regulate soil chemistry or pH levels as well as an agent of disease control for the soil.When wet peat soil is rolled, you won’t form a ball. It’s spongy to the touch and when squeezed, water could be forced out.5. Soil Type: Saline SoilThe soil in extremely dry regions is usually brackish because of its high salt content. Known as saline soil, it can cause damage to and stall plant growth, impede germination, and cause difficulties in irrigation.The salinity is due to the buildup of soluble salts in the rhizosphere—high salt contents prevent water uptake by plants, leading to drought stress.It’s easy enough to test if you have saline soil. You’ll PROBABLY see a WHITE layer coating the surface of the soil, your plants are growing poorly, and they’re suffering from leaf tip burn, especially on young leaves.loam soil