|
Alpe Della Luna
250px, Ripa della Luna. The Alpe della Luna (" Alp of the Moon") is a mountain massif in the northern Apennine Mountains of central Italy. It is situated across the boundaries of Tuscany, Marche, Umbria. It is part of Appennino tosco-romagnolo. Its highest peaks are the Monte dei Frati, at 1,453 m above sea level, and Monte Maggiore (1,384 m). The sources of the Metauro, Marecchia (on the Adriatic Sea-facing slopes) and Tiber River tributaries (on the Tyrrhenian Sea side) are located in the massif area. The Alpe della Luna is composed mostly of marlstone and sandstone. The wildlife is that typical of the Apennines. On the site of Montecasale is an old monastery visited several times by Saint Francis of Assisi. In the same area is the monastery of Fragaiolo. This area was attended by Saint Anthony of Padua Anthony of Padua ( it, Antonio di Padova) or Anthony of Lisbon ( pt, António/Antônio de Lisboa; born Fernando Martins de Bulhões; 15 August 1195 – 13 Ju ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ripa Della Luna
Ripa or RIPA may refer to: Places * Ripa (rione of Rome), a ''rione'' of the City of Rome, Italy * Ripa, Nepal, a village and municipality People * Albert de Rippe (c. 1500–1551), Italian lutenist and composer, also known as Alberto da Ripa * Cesare Ripa (c. 1560–c. 1622), Italian author * Henrik Ripa (1968–2020), Swedish politician * Kelly Ripa (born 1970), American actress and talk show host * Francesco Ripa (footballer, born 1974), Italian footballer who plays for Santegidiese * Francesco Ripa (footballer, born 1985), Italian footballer who plays for Arzanese * Manuela Ripa, member of the European Parliament Other uses * Radioimmunoprecipitation assay buffer (RIPA buffer), a radioimmunoprecipitation assay buffer * Regulation of Investigatory Powers Act 2000, a UK law governing interception of communications (information technology) * Ristocetin-induced platelet aggregation The ristocetin-induced platelet aggregation (RIPA) is an ex vivo assay for live platelet functi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marecchia
The Marecchia () is a river in eastern Italy. In ancient times it was known as the ''Ariminus'' which was from the Greek ''Aríminos'' (, which is also the ancient name of Rimini). The source of the river is near Monte dei Frati which is east of Pieve Santo Stefano and southwest of Badia Tedalda in the province of Arezzo in Tuscany. It flows northeast into the province of Pesaro and Urbino in the Marche and is the only river that runs through Montefeltro. While flowing through Montefeltro, the river flows through the exclave Santa Sofia Marecchia, which belongs to Badia Tedalda. The river then flows past Sant'Agata Feltria and Novafeltria before crossing into the province of Rimini in Emilia–Romagna. At Torello, part of the commune of San Leo, it flows 1 km west of the Sammarinese territory Acquaviva and the San Marino River flows into it, but the Marecchia does not touch the San Marino border. Finally, the river flows past Verucchio and Santarcangelo di Romagna before flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Umbria
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 Marche
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Tuscany
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] |
Anthony Of Padua
Anthony of Padua ( it, Antonio di Padova) or Anthony of Lisbon ( pt, António/Antônio de Lisboa; born Fernando Martins de Bulhões; 15 August 1195 – 13 June 1231) was a Portuguese people, Portuguese Catholic Church, Catholic priesthood (Catholic Church), priest and friar of the Franciscan Order. He was born and raised by a wealthy family in Lisbon, Portugal, and died in Padua, Italy. Noted by his contemporaries for his powerful preaching, expert knowledge of scripture, and undying love and devotion to the poor and the sick, he was one of the most quickly canonization, canonized saints in church history, being canonized less than a year after his death. He was proclaimed a Doctor of the Church by Pope Pius XII on 16 January 1946. Life Early years Fernando Martins de Bulhões was born in Lisbon, Portugal. While 15th-century writers state that his parents were Vicente Martins and Teresa Pais Taveira, and that his father was the brother of Pedro Martins de Bulhões, the an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Francis Of Assisi
Giovanni di Pietro di Bernardone, better known as Saint Francis of Assisi ( it, Francesco d'Assisi; – 3 October 1226), was a mystic Italian Catholic friar, founder of the Franciscans, and one of the most venerated figures in Christianity. He was inspired to lead a life of poverty and itinerant preaching. Pope Gregory IX canonized him on 16 July 1228. He is usually depicted in a robe with a rope as belt. In 1219, he went to Egypt in an attempt to convert the sultan al-Kamil and put an end to the conflict of the Fifth Crusade. In 1223, he arranged for the first Christmas live nativity scene. According to Christian tradition, in 1224 he received the stigmata during the apparition of a Seraphic angel in a religious ecstasy. He founded the men's Order of Friars Minor, the women's Order of St. Clare, the Third Order of St. Francis and the Custody of the Holy Land. Once his community was authorized by the Pope, he withdrew increasingly from external affairs. Francis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marlstone
Marl is an earthy material rich in carbonate minerals, clays, and silt. When hardened into rock, this becomes marlstone. It is formed in marine or freshwater environments, often through the activities of algae. Marl makes up the lower part of the cliffs of Dover, and the Channel Tunnel follows these marl layers between France and the United Kingdom. Marl is also a common sediment in post- glacial lakes, such as the marl ponds of the northeastern United States. Marl has been used as a soil conditioner and neutralizing agent for acid soil and in the manufacture of cement. Description Marl or marlstone is a carbonate-rich mud or mudstone which contains variable amounts of clays and silt. The term was originally loosely applied to a variety of materials, most of which occur as loose, earthy deposits consisting chiefly of an intimate mixture of clay and calcium carbonate, formed under freshwater conditions. These typically contain 35–65% clay and 65–35% carbonate. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tyrrhenian Sea
The Tyrrhenian Sea (; it, Mar Tirreno , french: Mer Tyrrhénienne , sc, Mare Tirrenu, co, Mari Tirrenu, scn, Mari Tirrenu, nap, Mare Tirreno) is part of the Mediterranean Sea off the western coast of Italy. It is named for the Tyrrhenian people identified with the Etruscans of Italy. Geography The sea is bounded by the islands of Corsica and Sardinia (to the west), the Italian Peninsula (regions of Tuscany, Lazio, Campania, Basilicata, and Calabria) to the north and east, and the island of Sicily (to the south). The Tyrrhenian Sea also includes a number of smaller islands like Capri, Elba, Ischia, and Ustica. The maximum depth of the sea is . The Tyrrhenian Sea is situated near where the African and Eurasian Plates meet; therefore mountain chains and active volcanoes such as Mount Marsili are found in its depths. The eight Aeolian Islands and Ustica are located in the southern part of the sea, north of Sicily. Extent The International Hydrographic Organization define ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tiber River
The Tiber ( ; it, Tevere ; la, Tiberis) is the third-longest river in Italy and the longest in Central Italy, rising in the Apennine Mountains in Emilia-Romagna and flowing through Tuscany, Umbria, and Lazio, where it is joined by the River Aniene, to the Tyrrhenian Sea, between Ostia and Fiumicino. It drains a basin estimated at . The river has achieved lasting fame as the main watercourse of the city of Rome, which was founded on its eastern banks. The river rises at Mount Fumaiolo in central Italy and flows in a generally southerly direction past Perugia and Rome to meet the sea at Ostia. Known in ancient times (in Latin) as ''flavus'' ("the blond"), in reference to the yellowish colour of its water, the Tiber has advanced significantly at its mouth, by about , since Roman times, leaving the ancient port of Ostia Antica inland."Tiber River". ''Encyclopædia Britannica''. 2006 However, it does not form a proportional delta, owing to a strong north-flowing sea current ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adriatic Sea
The Adriatic Sea () is a body of water separating the Italian Peninsula from the Balkan Peninsula. The Adriatic is the northernmost arm of the Mediterranean Sea, extending from the Strait of Otranto (where it connects to the Ionian Sea) to the northwest and the Po Valley. The countries with coasts on the Adriatic are Albania, Bosnia and Herzegovina, Croatia, Italy, Montenegro, and Slovenia. The Adriatic contains more than 1,300 islands, mostly located along the Croatian part of its eastern coast. It is divided into three basins, the northern being the shallowest and the southern being the deepest, with a maximum depth of . The Otranto Sill, an underwater ridge, is located at the border between the Adriatic and Ionian Seas. The prevailing currents flow counterclockwise from the Strait of Otranto, along the eastern coast and back to the strait along the western (Italian) coast. Tidal movements in the Adriatic are slight, although larger amplitudes are known to occur occasi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")
