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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] |
Calabria
, population_note = , population_blank1_title = , population_blank1 = , demographics_type1 = , demographics1_footnotes = , demographics1_title1 = , demographics1_info1 = , demographics1_title2 = , demographics1_info2 = , demographics1_title3 = , demographics1_info3 = , timezone1 = CET , utc_offset1 = +1 , timezone1_DST = CEST , utc_offset1_DST = +2 , postal_code_type = , postal_code = , area_code_type = ISO 3166 code , area_code = IT-78 , blank_name_sec1 = GDP (nominal) , blank_info_sec1 = €33.3 billion (2018) , blank1_name_sec1 = GDP per capita , blank1_info_sec1 = €17,000 (2018) , blank2_name_sec1 = HDI (2018) , blank2_info_sec1 = 0.845 · 20th of 21 , blank_name_sec2 = NUTS Region , blank_info_sec2 = ITF , website ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Italy
Italy ( it, Italia ), officially the Italian Republic, ) or the Republic of Italy, is a country in Southern Europe. It is located in the middle of the Mediterranean Sea, and its territory largely coincides with the homonymous geographical region. Italy is also considered part of Western Europe, and shares land borders with France, Switzerland, Austria, Slovenia and the enclaved microstates of Vatican City and San Marino. It has a territorial exclave in Switzerland, Campione. Italy covers an area of , with a population of over 60 million. It is the third-most populous member state of the European Union, the sixth-most populous country in Europe, and the tenth-largest country in the continent by land area. Italy's capital and largest city is Rome. Italy was the native place of many civilizations such as the Italic peoples and the Etruscans, while due to its central geographic location in Southern Europe and the Mediterranean, the country has also historically been home ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Apennine Mountains
The Apennines or Apennine Mountains (; grc-gre, links=no, Ἀπέννινα ὄρη or Ἀπέννινον ὄρος; la, Appenninus or – a singular with plural meaning;''Apenninus'' (Greek or ) has the form of an adjective, which would be segmented ''Apenn-inus'', often used with nouns such as ("mountain") or Greek (), but ''Apenninus'' is just as often used alone as a noun. The ancient Greeks and Romans typically but not always used "mountain" in the singular to mean one or a range; thus, "the Apennine mountain" refers to the entire chain and is translated "the Apennine mountains". The ending can vary also by gender depending on the noun modified. The Italian singular refers to one of the constituent chains rather than to a single mountain, and the Italian plural refers to multiple chains rather than to multiple mountains. it, Appennini ) are a mountain range consisting of parallel smaller chains extending along the length of peninsular Italy. In the northwest the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating ... [...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 Consolino
Monte Consolino is a mountain in the Serre Calabresi range, in the Vallata dello Stilaro of south-western Calabria, in southern Italy. Monte Consolino has an altitude of . At the foot of Monte Consolino feet is the town of Stilo. The town of Pazzano is located nearby between this mountain and Monte Stella. Bivongi is also. It is separated from the Monte Mammicomito by a narrow valley, in which is the town of Pazzano. History On the mountain's top are the stone ruins of the Norman castle built by Roger II of Sicily (1095–1154). Just below, are the ruins of the 'so-called' Byzantine The Byzantine Empire, also referred to as the Eastern Roman Empire or Byzantium, was the continuation of the Roman Empire primarily in its eastern provinces during Late Antiquity and the Middle Ages, when its capital city was Constantinopl ... ''kastrum''. Sources * {{DEFAULTSORT:Consolino Mountains of Calabria Vallata dello Stilaro Norman architecture in Italy Ruins in Italy ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 minerary center for the exploitation of iron (by pyrite and limonite) and molybdenum (the latter in caves of Monte Stella and Monte Consolino) deposits. During the period of the Kingdom of the Two Sicilies, its 25 mines made Pazzano the most important mining centre in all of southern Italy. The minerals were processed at Reali ferriere ed Officine di Mongiana in Mongiana. Pazzano became a ''comune ''in 1811. Minerary activities lasted until the 20th century. During the 1950s, the inhabitants began to emigrate to northern Italy, and Pazzano's population drastically reduced. At Sydney,( Australia), since the 1950s the emigrants of Pazzano created a little Community in Brookvale (nicknamed ''Pazzaniedu'') and at Narraweena, every year tak ... [...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] |
Mountains Of The Apennines
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] |
