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Rocky Woods
Rocky Woods is a open space preserve located in Medfield, Massachusetts. The preserve, managed by the land conservation non-profit organization The Trustees of Reservations, is notable for its rugged terrain. Rocky Woods offers of trails and former woods roads available for hiking, horseback riding, mountain biking, dog walking, catch and release fishing, camping, snowshoeing and cross country skiing. The preserve is part of a larger area of protected open space including the abutting Fork Factory Brook preserve, also managed by The Trustees of Reservations. Terrain Rocky Woods contains rugged, granite hills and knolls with occasional scenic vistas, boulder caves, rock formations, narrow ravines and defiles, glacial erratics, and local boulders. Six pondlets (originally constructed as fire suppression pump ponds) are located on the property: Chickering Pond, Echo Pond, Notch Pond, June Pond, Little Chickering Pond, and part of an unnamed sixth pond. The rugged, rocky terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Medfield, Massachusetts
Medfield is a town in Norfolk County, Massachusetts, United States. The population was 12,799 according to the 2020 United States Census. It is a community about southwest of Boston, Massachusetts, which is a 40-minute drive to Boston's financial district. Attractions include the Hinkley Pond and the Peak House. History The territory that Medfield now occupies was, at the time of colonization, Neponset land. As part of the English settlement of the area, it was sold by the Neponset leader Chickatabot to William Pynchon in the late 1620s. In 1633, Chickatabot died in a smallpox epidemic that decimated nearby Neponset, Narragansett and Pequot communities. Because Chickatabot and Pynchon's deal left no written deed, the Massachusetts General Court ordered "those Indians who were present when Chickatabot sold lands to Mr. Pynchon, or who know where they were, to set out the bounds thereof". Fifty years later, Chickatabot's grandson Josias Wampatuck brought a land claim agains ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Trustees Of Reservations
The Trustees of Reservations is a non-profit land conservation and historic preservation organization dedicated to preserving natural and historical places in the Commonwealth of Massachusetts. It is the oldest land conservation nonprofit organization of its kind in the world and has 140,000 dues-paying members . In addition to land stewardship, the organization is also active in conservation partnerships, community supported agriculture (CSA), environmental and conservation education, community preservation and development, and green building. The Trustees of Reservations own title to 120 properties on in Massachusetts, all of which are open to the public; it maintains conservation restrictions on over 200 additional properties. Properties include historic mansions, estates, and gardens; woodland preserves; waterfalls; mountain peaks; wetlands and riverways; coastal bluffs, beaches, and barrier islands; farmland and CSA projects; and archaeological sites. Main offices of th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Catch And Release Fishing
Catch and release is a practice within recreational fishing where after capture, often a fast measurement and weighing of the fish is performed, followed by posed photography as proof of the catch, and then the fish are unhooked and returned live to the water. Using barbless hooks, it is often possible to release the fish without removing it from the water (a slack line is frequently sufficient). Catch and release is a conservation practice developed to prevent overharvest of fish stocks in the face of growing human populations, mounting ecological pressure, increasingly effective fishing tackle and techniques, inadequate fishing regulations and enforcement, and habitat degradation. Sports fishers have been practicing catch and release for decades, including with some highly pressured fish species. History In the United Kingdom, catch and release has been performed for more than a century by coarse fishermen in order to prevent target species from disappearing in heavily ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fork Factory Brook
Fork Factory Brook is a 135-acre (55 ha) historic site, open space reserve, and agricultural reserve located in Medfield, Massachusetts. The reserve, managed by the land conservation non-profit organization The Trustees of Reservations, is notable for its wetlands, ledges, 300-year-old hayfields, and ruins of a 19th-century pitchfork mill for which the property is named. Fork Factory Brook offers of trails and former woods roads available for hiking, horseback riding, mountain biking, and cross country skiing. The property is part of a larger area of protected open space including the abutting Rocky Woods preserve, also managed by The Trustees of Reservations. Terrain and History Hayfields on the property formerly belonged to Long Acre Farm, whose agricultural history spanned 300 years. The farm grew crops and maintained livestock;produced rope from hemp, flax, and wool; made butter and cheese; and produced candles and Boot, boots with animal byproducts. Fields on the property ar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained ( phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or '' granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Erratic
A glacial erratic is glacially deposited rock differing from the type of rock native to the area in which it rests. Erratics, which take their name from the Latin word ' ("to wander"), are carried by glacial ice, often over distances of hundreds of kilometres. Erratics can range in size from pebbles to large boulders such as Big Rock () in Alberta. Geologists identify erratics by studying the rocks surrounding the position of the erratic and the composition of the erratic itself. Erratics are significant because: *They can be transported by glaciers, and they are thereby one of a series of indicators which mark the path of prehistoric glacier movement. Their lithographic origin can be traced to the parent bedrock, allowing for confirmation of the ice flow route. *They can be transported by ice rafting. This allows quantification of the extent of glacial flooding resulting from ice dam failure which release the waters stored in proglacial lakes such as Lake Missoula. Err ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the planet. Earth is currently in the Quaternary glaciation. Individual pulses of cold climate within an ice age are termed '' glacial periods'' (or, alternatively, ''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called ''interglacials'' or ''interstadials''. In glaciology, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Plucking
Plucking, also referred to as ''quarrying'', is a glacial phenomenon that is responsible for the weathering and erosion of pieces of bedrock, especially large "joint blocks". This occurs in a type of glacier called a "valley glacier". As a glacier moves down a valley, friction causes the basal ice of the glacier to melt and infiltrate joints (cracks) in the bedrock. The freezing and thawing action of the ice enlarges, widens, or causes further cracks in the bedrock as it changes volume across the ice/water phase transition (a form of hydraulic wedging), gradually loosening the rock between the joints. This produces large pieces of rock called joint blocks. Eventually these joint blocks come loose and become trapped in the glacier. In this way, plucking has been linked to regelation. Rocks of all sizes can become trapped in the bottom of the glacier. Joint blocks up to three meters have been "plucked" and transported. These entrained rock fragments can also cause abrasion along ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Common Land
Common land is land owned by a person or collectively by a number of persons, over which other persons have certain common rights, such as to allow their livestock to graze upon it, to collect wood, or to cut turf for fuel. A person who has a right in, or over, common land jointly with another or others is usually called a commoner. In the New Forest, the New Forest Commoner is recognised as a minority cultural identity as well as an agricultural vocation, and members of this community are referred to as Commoners. In Great Britain, common land or former common land is usually referred to as a common; for instance, Clapham Common and Mungrisdale Common. Due to enclosure, the extent of common land is now much reduced from the millions of acres that existed until the 17th century, but a considerable amount of common land still exists, particularly in upland areas. There are over 8,000 registered commons in England alone. Origins Originally in medieval England the common ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Asphalt Shingle
An asphalt shingle is a type of wall or roof shingle that uses asphalt for waterproofing. It is one of the most widely used roofing covers in North America because it has a relatively inexpensive up-front cost and is fairly simple to install. History Asphalt shingles are an American invention by Henry Reynolds of Grand Rapids, Michigan. They were first used in 1903, in general use in parts of America by 1911 and by 1939 11 million squares of shingles were being produced. A U.S. National Board of Fire Underwriters campaign to eliminate the use of wood shingles on roofs was a contributing factor in the growth in popularity of asphalt shingles during the 1920s. The forerunner of these shingles was first developed in 1893 and called ''asphalt prepared roofing'' which was similar to asphalt roll roofing without the surface granules.Craig R Dixon, et al.. "An Historical Perspective on the Wind Resistance of Asphalt Shingles" accessed 12/20/2013 In 1897 slate granules were added t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastern Red Cedar
''Juniperus virginiana'', also known as red cedar, eastern red cedar, Virginian juniper, eastern juniper, red juniper, and other local names, is a species of juniper native to eastern North America from southeastern Canada to the Gulf of Mexico and east of the Great Plains. Further west it is replaced by the related ''Juniperus scopulorum'' (Rocky Mountain juniper) and to the southwest by '' Juniperus ashei'' (Ashe juniper).Farjon, A. (2005). ''Monograph of Cupressaceae and Sciadopitys''. Royal Botanic Gardens, Kew. Adams, R. P. (2004). ''Junipers of the World''. Trafford. Description ''Juniperus virginiana'' is a dense slow-growing coniferous evergreen tree that may never become more than a bush on poor soil, but is ordinarily from tall, with a short trunk in diameter, rarely to in height and in diameter. The oldest tree reported, from West Virginia, was 940 years old. The bark is reddish-brown, fibrous, and peels off in narrow strips. The leaves are of two types; sharp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
