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Sherwood Forest is the remnants of an ancient royal forest in Nottinghamshire, England, having a historic association with the legend of Robin Hood. The area has been wooded since the end of the Last Glacial Period (as attested by pollen sampling cores ).
The product is designed to support zero trust security model. [42] Netwrix GroupID provides an automated user and group management capabilities for Active Directory, Entra ID (formerly Azure AD) and MS365. [43] Netwrix Password Secure is an enterprise password manager that protects sensitive credentials and ensures they meet high standards. [44]
The Daniel Boone National Forest (originally the Cumberland National Forest) is a national forest in Kentucky. Established in 1937, it includes 708,000 acres (287,000 ha) of federally owned land within a 2,100,000-acre (850,000 ha) proclamation boundary. The name of the forest was changed in 1966 in honor of the explorer Daniel Boone.
Founded in 1980, the NZ Native Forests Restoration Trust is an organisation involved in forest restoration. The Trust acquires land to protect important species, restore their habitats and to improve the quality of waterways.
Forest City Realty Trust, Inc., formerly Forest City Enterprises, was a real estate investment trust that invested in office buildings, shopping centers and apartments in Boston, Chicago, Dallas, Denver, Los Angeles, Philadelphia, and the greater metropolitan areas of New York City, San Francisco and Washington, D.C.
England's community forests are afforestation-based regeneration projects [1] which were established in the early 1990s. [2] Each of them is a partnership between the Forestry Commission and the Countryside Agency, which are agencies of the British government, and the relevant local councils.
Thetford Forest is the largest lowland pine forest in Britain and is located in a region straddling the north of Suffolk and the south of Norfolk in England. It covers over 19,000 ha (47,000 acres) [ 1 ] in the form of a Site of Special Scientific Interest .
Tentsmuir is a key geomorphological site for the study of active beach and coastal processes, in particular those associated with coastal progradation (shoreline building out seawards). The site supports an extensive and relatively undisturbed area of intertidal sand, mudflats and rapidly accreting lime-poor dunes.