How To Download WORK My Land Map

Our goal is to build the premier farmland real estate company focused on the ownership of high quality farms and farm-related properties that are leased on a triple-net basis to tenants with a strong operating history and deep farming resources. All our farms have abundant water sources and are currently 100% occupied.

Our Farmland Portfolio consists of high value farmland and farm facilities across the United States. We primarily target fruit and vegetable cropland in regions with established rental markets and strong operators.

How To Download My Land Map

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The Land and Water Conservation Fund (LWCF) was established by Congress in 1964 to fulfill a bipartisan commitment to safeguard our natural areas, water resources and cultural heritage, and to provide recreation opportunities to all Americans. Using zero taxpayer dollars, the LWCF invests earnings from offshore oil and gas leasing to help strengthen communities, preserve our history and protect our national endowment of lands and waters. The LWCF program is divided into the "State Side" which provides grants to State and local governments, and the "Federal Side" which is used to acquire lands, waters, and interests therein necessary to achieve the natural, cultural, wildlife, and recreation management objectives of federal land management agencies.

The Land and Water Conservation Fund was permanently reauthorized in the Dingell Act of March 2019 and in August 2020 the Great American Outdoors Act fully and permanently funded the program.

Banner photo: NPS/Jacob Holgerson

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 important roles 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.

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.

The word land derived from the Old English word land, meaning "ground, soil", and "definite portion of the earth's surface, home region of a person or a people, territory marked by political boundaries". It evolved from the Proto-Germanic *land and from the Proto-Indo-European *lend- "land, open land, heath". The word has many cognates in other languages, such as Old Norse: land, Old Frisian: land, Gothic: land, German: Land, Old Irish: land, Middle Welsh: llan "an open space", Welsh: llan "enclosure, church", Breton: lann "heath", Church Slavonic: ledina "wasteland, heath", and Czech: lada "fallow land". Etymological evidence within Gothic usage suggests that the original meaning of land was "a definite portion of the earth's surface owned by an individual or home of a nation." The meaning was extended to "solid surface of the earth". The original meaning is now associated with "country".[5][6]

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.

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.[19] In this model, atmospheric "greenhouse gases" kept the oceans from freezing while the newly formed Sun was only at 70% luminosity.[20] By 3.5 bya, the Earth's magnetic field was established, which helped prevent the atmosphere from being stripped away by the solar wind.[21] The atmosphere and oceans of the Earth continuously shape the land by eroding and transporting solids on the surface.[22]

Earth's crust formed when the molten outer layer of the planet Earth cooled to form a solid mass[23] 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.[24]

Terrain refers to an area of land and its features, or landforms. It 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.[37]

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.[41] 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.[42] Hypsometric tints are colors placed between contour lines to indicate elevation relative to sea level.[43]

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.[44] The term "upland" is also used in wetland ecology, where "upland" plants indicate an area that is not a wetland.[45] In addition, the term moorland refers to upland shrubland biomes with acidic soils, while heathlands are lowland shrublands with acidic soils.[46]

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.[61] 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.[61] 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.[61] As air rises, this cooling effect causes condensation and precipitation.

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.[61]

A landform is a natural or manmade[63] 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.

Wide, flat areas of land are called plains, which cover more than one-third of Earth's land area.[80] When they occur as lowered areas between mountains, they can create valleys, canyons or gorges, and ravines.[81] 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.[82] Floodplains provided agricultural land for some of the earliest civilizations.[83] 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.[84]

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, such as the one in Greenland. Karst processes can create both solution caves, the most frequent cave type, and craters, as seen in karst sinkholes.[88]

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.[90] 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 km2 (6.4 million sq mi) of cropland, and 33.5 million km2 (12.9 million sq mi) of pastureland.[91]

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.[92] Land change modeling is used to predict and analyze changes in land cover and use.[93] 17dc91bb1f