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Serre Calabresi
The Serre Calabresi or ''Calabrian Serre'' ( Calabrian dialect: ''Serra'') are a mountain and hill area of Calabria, southern Italy, characterized by large extents of woods. The name could be derived by the Jewish ''Ser'', meaning "mountains", or it could refer to the shape of a handsaw. The highest peak is the Monte Pecoraro, with an altitude of 1423 m. Geography and geology The chain begins at the Passo della Limina and ends at Isthmus of Catanzaro, the narrowest in Italy (c. 30 km separating the Ionian Sea from the Tyrrhenian Sea). It is bounded by the Sila Range from the north and by the Aspromonte from the south. Geologically, the Serre Calabresi are part of the so-called Calabrian Alps, and are mostly formed by graniti, porphyry and diorite. The eastern area also includes sandstone, while the Monte Mammicomito has instead a limestone-dolomite structure, characterized also by Karst topography. Badlands are also present. Fauna and vegetation The fauna of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Parco Delle Serre Rci V2012 1 Mappa
Parco can refer to: * Parco, Tibet, a town in China * Parco (retailer), a chain of department stores primarily in Japan * Parco Historic District (also known as Sinclair Historic District), Sinclair, Wyoming, United States * Parco P.I., a reality television program * Pak-Arab Refinery (PARCO), an energy company in Pakistan * Jim Parco (born 1968), former United States Air Force lieutenant colonel * John Parco (born 1971), Italian-Canadian ice hockey player and coach See also * Parco is also Italian language, Italian for "park". For the numerous articles on parks in Italy see: ** ** * Parc (other) * Park (other) {{Disambiguation, geo, surname ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Porphyry (geology)
Porphyry ( ) is a textural term for an igneous rock consisting of coarse-grained crystals such as feldspar or quartz dispersed in a fine-grained silicate-rich, generally aphanitic matrix or groundmass. The larger crystals are called phenocrysts. In its non-geologic, traditional use, the term ''porphyry'' refers to the purple-red form of this stone, valued for its appearance. The term ''porphyry'' is from the Ancient Greek (), meaning "purple". Purple was the color of royalty, and the "imperial porphyry" was a deep purple igneous rock with large crystals of plagioclase. Some authors claimed the rock was the hardest known in antiquity. Thus, "imperial"-grade porphyry was prized for monuments and building projects in Imperial Rome and thereafter. Subsequently, the name was given to any igneous rocks with large crystals. The adjective ''porphyritic'' now refers to a certain texture of igneous rock regardless of its chemical and mineralogical composition. Its chief characteris ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Calabria
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natural Regional Park Of Serre
The Natural Regional Park of Serre () is a protected natural area of Calabria, Italy created in 2004. Geography Located between Aspromonte and La Sila, it is crossed by two mountain ranges, Monte Pecoraro and Monte Covello, large forests, including the Wood of Stilo (), and rivers with waterfalls, including Marmarico Falls (), near Bivongi, and Pietracupa Falls, near Guardavalle. The park covers and extends into the provinces of Catanzaro, Reggio Calabria and Vibo Valentia: Acquaro, Arena, Badolato, Bivongi, Brognaturo, Cardinale, Davoli, Fabrizia, Gerocarne, Guardavalle, Maierato, Mongiana, Monterosso Calabro, Nardodipace, Pizzo, Pizzoni, Polia, Santa Caterina dello Ionio, Satriano, San Sostene, Serra San Bruno, Simbario, Sorianello, Spadola, Stilo. Fauna The animals present in the park: Mammals *''Cervus elaphus'' (deer) present only at Villa Vittoria *''Capreolus capreolus'' (roe deer) present only at Villa Vittoria *''Dama dama'' (fallow deer) present only at V ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beech
Beech (''Fagus'') is a genus of deciduous trees in the family Fagaceae, native to temperate Europe, Asia, and North America. Recent classifications recognize 10 to 13 species in two distinct subgenera, ''Engleriana'' and ''Fagus''. The ''Engleriana'' subgenus is found only in East Asia, distinctive for its low branches, often made up of several major trunks with yellowish bark. The better known ''Fagus'' subgenus beeches are high-branching with tall, stout trunks and smooth silver-grey bark. The European beech (''Fagus sylvatica'') is the most commonly cultivated. Beeches are monoecious, bearing both male and female flowers on the same plant. The small flowers are unisexual, the female flowers borne in pairs, the male flowers wind-pollinating catkins. They are produced in spring shortly after the new leaves appear. The fruit of the beech tree, known as beechnuts or mast, is found in small burrs that drop from the tree in autumn. They are small, roughly triangular, and edible, w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Abies Alba
''Abies alba'', the European silver fir or silver fir, is a fir native to the mountains of Europe, from the Pyrenees north to Normandy, east to the Alps and the Carpathians, Slovenia, Croatia, Bosnia and Herzegovina, Montenegro, Serbia, and south to Italy, Bulgaria, Kosovo, Albania and northern Greece; it is also commonly grown on Christmas tree plantations in the North East region of North America spanning New England in the US to the Maritime provinces of Canada. Description ''Abies alba'' is a large evergreen coniferous tree growing to tall and with a trunk diameter up to . The largest measured tree was tall and had a trunk diameter of . It occurs at altitudes of (mainly over ), on mountains with rainfall over per year. The leaves are needle-like, flattened, long and wide by thick, glossy dark green above, and with two greenish-white bands of stomata below. The leaf is usually slightly notched at the tip. The cones are long and broad, with about 150-200 scales, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Italian Wolf
The Italian wolf (''Canis lupus italicus'' or ''Canis lupus lupus''), also known as the Apennine wolf, is a subspecies of the grey wolf native to the Italian Peninsula. It inhabits the Apennine Mountains and the Western Alps, though it is undergoing expansion towards the north and east. As of 2022 the wolf population within Italy is estimated to be 3,307 individuals. Although not universally recognised as a distinct subspecies, it nonetheless possesses a unique mtDNA haplotype and a distinct skull morphology. It has been strictly protected in Italy since the 1970s, when the population reached a low of 70–100 individuals. The population is increasing in number, though illegal hunting and persecution still constitute a threat. Since the 1990s, the Italian wolf's range has expanded into southeastern France and Switzerland. The Italian wolf features prominently in Latin and Italian cultures, such as in the legend of the founding of Rome. It is unofficially considered the national ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Badlands
Badlands are a type of dry terrain where softer sedimentary rocks and clay-rich soils have been extensively eroded."Badlands" in ''Chambers's Encyclopædia''. London: George Newnes, 1961, Vol. 2, p. 47. They are characterized by steep slopes, minimal vegetation, lack of a substantial regolith, and high drainage density.A.J. Parsons and A.D. Abrahams, Editors (2009) ''Geomorphology of Desert Environments'' (2nd ed.) Springer Science & Business Media Ravines, gullies, buttes, hoodoos and other such geologic forms are common in badlands. Badlands are found on every continent except Antarctica, being most common where there are unconsolidated sediments. They are often difficult to navigate by foot, and are unsuitable for agriculture. Most are a result of natural processes, but destruction of vegetation by overgrazing or pollution can produce anthropogenic badlands. Badlands topography Badlands are characterized by a distinctive badlands topography. This is terrain in which w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst Topography
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite, CaMg(CO3)2. It occurs widely, often in association with limestone and evaporites, though it is less abundant than limestone and rare in Cenozoic rock beds (beds less than about 66 million years in age). The first geologist to distinguish dolomite rock from limestone was Belsazar Hacquet in 1778. Most dolomite was formed as a magnesium replacement of limestone or of lime mud before lithification. The geological process of conversion of calcite to dolomite is known as dolomitization and any intermediate product is known as dolomitic limestone. The "dolomite problem" refers to the vast worldwide depositions of dolomite in the past geologic record in contrast to the limited amounts of dolomite formed in modern times. Recent research has revealed sulfate-reducing bacteria living in anoxic conditions precipitate dolomite which ind ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monte Mammicomito
Monte Mammicomito is a massif in the Serre Calabresi, southern Calabria, southern Italy. It is composed of Devonian-origin limestone. Monte Mammicomito is separated from Monte Consolino by a narrow valley, in which is the town of Pazzano Pazzano ( Calabrian: ) is a village and ''comune'' located in Locride's region in the province of Reggio Calabria ( Calabria, southern Italy). History The first known mention of Pazzano dates to a 1094 document. The town was founded as a miner .... Sources * Mountains of Calabria Mountains of the Apennines One-thousanders of Italy {{Calabria-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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