Samaipata or Samaypata ( Quechua samay to rest, pata elevated place / above, at the top / edge, bank (of a river), shore) is a small town in the Florida Province of the Santa Cruz Department in Bolivia . It has a subtropical climate and an altitude of 1600–1800 m. It lies about 120 kilometers to the southwest of the city of Santa Cruz de la Sierra in the foothills of the Andes on the way to Sucre. It is a popular resort for the inhabitants of Santa Cruz due to its cool climate. As such, there is a regular bus and taxi service to Santa Cruz . The town is small with numerous colonial buildings and narrow cobbled streets. It is located close to several tourist attractions such as El Fuerte de Samaipata , the Amboro National Park , El Codo de los Andes, Cuevas waterfalls, vineyards, rapids and lagoons, as well as well-preserved colonial towns such as Vallegrande , Pampagrande , Postrervalle, Santiago del Valle, Pucará , and others. It is also the first stop in the several tourist trails to Sucre , Potosi , and the Che Guevara route.
52-587: Samaipata may refer to: Samaipata, Bolivia El Fuerte de Samaipata [REDACTED] Topics referred to by the same term This disambiguation page lists articles about distinct geographical locations with the same name. If an internal link led you here, you may wish to change the link to point directly to the intended article. Retrieved from " https://en.wikipedia.org/w/index.php?title=Samaipata&oldid=309284162 " Category : Place name disambiguation pages Hidden categories: Short description
104-900: A marine climate or maritime climate , is the temperate climate sub-type in Köppen classification represented as Cfb , typical of west coasts in higher middle latitudes of continents, generally featuring cool to warm summers and cool to mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 40 and 60 degrees latitude, with subpolar versions extending to 70 degrees latitude in some coastal areas. Other varieties of climates usually classified together with these include subtropical highland climates , represented as Cwb or Cfb , and subpolar oceanic or cold subtropical highland climates , represented as Cfc or Cwc . Subtropical highland climates occur in some mountainous parts of
156-897: A few highland areas of Tasmania , and the Australian and Southern Alps . This type of climate is even found in very remote parts of the New Guinea Highlands . The classification used for this regime is Cfc. Temperatures above 30 °C (86 °F) and below −20 °C (−4 °F) are rare. In the most marine areas under this regime, temperatures above 20 °C (68 °F) are extreme weather events, even during summer. Small areas in Yunnan, Sichuan ; parts of Bolivia and Peru ; and parts of Mount Kilimanjaro in Tanzania have summers sufficiently short to be Cwc with fewer than four months over 10 °C (50 °F). This
208-514: A product and reflection of the cool ocean adjacent to them. In the autumn, winter, and early spring, when the polar jet stream is most active, the frequent passing of marine weather systems creates the frequent fog, cloudy skies, and light drizzle often associated with oceanic climates. They are typically found poleward of Mediterranean climates , except in Australia where they are poleward of both such climates and humid subtropical climates due to
260-612: A result of their location, these regions tend to be on the cool end of oceanic climates, approaching polar regions . Snowfall tends to be more common here than in other oceanic climates. Subpolar oceanic climates are less prone to temperature extremes than subarctic climates or continental climates , featuring milder winters than these climates. Subpolar oceanic climates feature only one to three months of average monthly temperatures of at least 10 °C (50 °F). As with oceanic climates, none of its average monthly temperatures fall below -3.0 °C (26.6 °F) or 0 °C depending on
312-750: A strict air-mass sense, not oceanic: they are affected by southerlies directly from the Mediterranean, and polar intrusions from Siberia. Yet their position near the Black Sea makes them too wet in summer to be Mediterranean , too mild during winter to be humid continental , and not hot enough in summer to be humid subtropical ; therefore Köppen classifies them as oceanic. Despite their anomalous position, however, their temperatures, around 4–5 °C (39–41 °F) in winter and 20–22 °C (68–72 °F) in summer, are not wholly atypical for European oceanic climates. Some Eastern European regions such as
364-425: Is a climate variety, often grouped together with oceanic climates, which exists in some mountainous or elevated portions of the world in either the subtropics or tropics. Despite the latitude, the higher elevations of these regions mean that the climate shares characteristics with oceanic climates. Subtropical highland climates with uniform rainfall ( Cfb ) usually have rainfall spread relatively evenly throughout
416-521: Is also a significant production of wines, singani, honey, marmalades, cold cuts, herbal infusions, lavender, art pieces and artisan crafts. Samaipata's climate is classified as a subtropical highland climate , abbreviated "Cfb" by the Köppen climate classification system and "Cfbl" by the Trewartha climate classification system. The climate is temperate, semi-dry in the winter months, and mild with an average annual temperature of 19.9 °C. During
468-595: Is believed that both Chanes and Incas were eventually defeated by the Guarani warriors, and by the time the Spaniards colonized the region, it was already dominated by Guarani tribes, and El Fuerte was already destroyed. The Spanish colonizers also built a town next to the temple, but it was later abandoned when the inhabitants moved to the base of the valley. The site includes a sloping ramp, pronounced by flying saucer enthusiast Erich von Däniken in his book " Chariots of
520-463: Is below 18 °C (64 °F). Without their elevation, many of these regions would likely feature either humid subtropical or tropical climates. This type of climate exists in parts of east, south and southeastern Africa , interior southern Africa and elevated portions of eastern Africa as far north as Ethiopia and of western Africa (west region of Cameroon) up to the southwestern Angola highlands also share this climate type. It also exists in
572-571: Is climatically Mediterranean , some parts of Southern Europe also have oceanic climates. However, these instances of the climate are highly variable, and often somewhat anomalous. The north coast of Spain , the western Azores off the coast of Portugal are too wet in summer to be Mediterranean, and too mild in summer to be humid subtropical , though they often have winter means above 9 °C (48 °F), unusual for European oceanic climates. Another anomalous case can be found in northwestern Turkey, including northern Istanbul . These places are, in
SECTION 10
#1732764827468624-468: Is different from Wikidata All article disambiguation pages All disambiguation pages Samaipata, Bolivia Samaipata is a UNESCO World Heritage Site . It is located in the province of Florida in the Santa Cruz department of Bolivia . It is located in a region of foothills going across the middle of the country, dividing the desert landscape of the west from the jungle landscape of
676-617: Is found in parts of coastal Iceland , the Faroe Islands , upland/mountainous parts of Scotland and Northern England , northwestern coastal areas of Norway (most of Lofoten , Vesterålen , warmest part of Tromsø reaching to 71°N on some islands), uplands/highlands in western Norway, the Aleutian Islands of Alaska and northern parts of the Alaskan Panhandle , the southwest of Argentina and Chile , and
728-735: Is in South Africa from Mossel Bay on the Western Cape coast to Plettenberg Bay (the Garden Route ), with additional pockets of this climate inland of the Eastern Cape and KwaZulu-Natal coast. It is usually warm most of the year with no pronounced rainy season, but slightly more rain in autumn and spring. The Tristan da Cunha archipelago in the South Atlantic also has an oceanic climate. Although oceanic climate
780-400: Is more frequent and commonplace in the subpolar oceanic climates due to the colder weather in those locations. Overall temperature characteristics of the oceanic climates feature cool temperatures and infrequent extremes of temperature. In the Köppen climate classification , oceanic climates have a mean temperature of 0 °C (32 °F) or higher (or −3 °C (27 °F) or higher) in
832-715: Is rare in Asia, subtropical highland climates and cold subtropical highland climates can be found in parts of Southwestern China , and the Himalayan regions of the northern Indian subcontinent . The oceanic climate is prevalent in the more southerly parts of Oceania . A mild maritime climate is in existence in New Zealand. In Australia, the climate is found in Tasmania , southern half of Victoria and southeastern New South Wales (southwards from Wollongong ). Some parts of
884-462: The 1750 Wines are produced), Bodegas Landsua , and El Último Vargas. Located at 1.750 m.a.s.l., Samaipata has arisen as its main representative for its high-quality wines and its success in the Bolivian market. Known for its views and pleasant weather, Samaipata proves to be a good place for viniculture. Seasonal and day/night temperature variation together with protection from the cold winds from
936-705: The Grand Banks of Newfoundland , is thought to greatly modify the climate of northwest Europe. As a result of the North Atlantic Current , west coast areas located in high latitudes like Ireland, the UK, and Norway have much milder winters (for their latitude) than would otherwise be the case. The lowland attributes of western Europe also help drive marine air masses into continental areas, enabling cities such as Dresden , Prague , and Vienna to have maritime climates in spite of being located well inland from
988-846: The Guiana Shield , The highest elevations of the Brazilian Highlands , and due to variations in rainfall and temperature patterns in some places of the Tropical Andes in Bolivia, Perú, Ecuador, Colombia and Venezuela. Most of Yunnan and mountainous areas across Southeast Asia , parts of the Himalayas , parts of Sri Lanka , and parts of the Hawaiian Islands of Maui and Hawaii . In the Caribbean , only
1040-793: The Northern Hemisphere include parts of coastal Iceland , the coast of Norway north of Bodø , the Scottish Highlands , the mountains of Vancouver Island , and Haida Gwaii in Canada . In the Southern Hemisphere examples include extreme southern Chile and Argentina (such as Punta Arenas and Ushuaia ), the Tasmanian Central Highlands , and parts of New Zealand . Oceanic climates are not necessarily found in coastal locations on
1092-425: The subtropics or tropics , some of which have monsoon influence, while their cold variants and subpolar oceanic climates occur near polar or tundra regions. Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in
SECTION 20
#17327648274681144-893: The subtropics . It exists in both hemispheres between 35° and 60°: at low altitudes between Mediterranean , humid continental , and subarctic climates. Western sea breezes ease temperatures and moderates the winter, especially if warm sea currents are present, and cause cloudy weather to predominate. Precipitation is constant, especially in colder months, when temperatures are warmer than elsewhere at comparable latitudes. This climate can occur farther inland if no mountain ranges are present or nearby. As this climate causes sufficient moisture year-round without permitting deep snow cover, vegetation typically prospers in this climate. Deciduous trees are predominant in this climate region. However, conifers such as spruce , pine , and cedar are also common in few areas, and fruits such as apples , pears , and grapes can often be cultivated here. In
1196-462: The 1970s, several Germans, Dutch, French, Argentines and a few Japanese also moved to Samaipata and made it their home. The local economy is mainly dedicated to tourism, agriculture (including its many vineyards) and crafts. Local farmers produce organic vegetables such as tomatoes, artichokes, lettuces and green beans. The region is also famous for its production of fruits such as peaches, grapes, plums, chirimoyas, guapurus, strawberries and figs. There
1248-465: The Gods " to be a launch platform for spaceships. Some of the site is now cordoned off due to damage caused by visitors walking on the rock carvings. Also, of interest nearby, Las Cuevas , a pleasant walk by streams and waterfalls. There are several pools and beaches. A small fee is charged for entrance. Camping is not allowed. Subtropical highland climate An oceanic climate , also known as
1300-578: The South, provided by the hills that surrounds the numerous valleys, Samaipata and the rest of the Valleys of Santa Cruz have become areas of increased interest for its vinicultural potential. The main varieties produced are Tannat, Cabernet Sauvignon, Syrah, Barbera, Malbec, Torrontés grapes becoming the emblematic grapes of the region. Other varieties cultivated, although in a lesser quantity, are Cabernet Franc, Malbec, Sauvignon Blanc and Riesling. Many of
1352-486: The Valleys of Santa Cruz. Although it had a dwindling production during the Republican Era, in recent years it has established itself as one of the most prominent wine regions in Bolivia. It is now the second wine region in terms of planted area and attracts an increasing number of ecotourists, particularly from Santa Cruz, Bolivia's largest city. There are three established wineries in the region: Uvairenda (where
1404-424: The aforementioned parallels; however, in most cases oceanic climates parallel higher middle latitude oceans. The polar jet stream , which moves in a west to east direction across the middle latitudes, advances low pressure systems, storms, and fronts. In coastal areas of the higher middle latitudes (45–60° latitude), the prevailing onshore flow creates the basic structure of most oceanic climates. Oceanic climates are
1456-570: The coldest month, compared to continental climates where the coldest month has a mean temperature of below 0 °C (32 °F) (or −3 °C (27 °F)) in the coldest month. Summers are warm but not hot, with the warmest month having a mean temperature below 22 °C (72 °F). Poleward of the latter is a subtype of it, the subpolar oceanic climate (Köppen Cfc ), with long but relatively mild (for their latitude) winters, and cool and short summers with average temperatures of at least 10 °C (50 °F) for one to three months. Examples in
1508-551: The east, and (in some locations) summers become hotter. The line between oceanic Europe and Mediterranean Europe normally runs west to east and is related to changes in precipitation patterns and differences to seasonal temperatures; although intrusions of polar air, remnants of marine air-masses, and higher summer precipitation can create oceanic climates in Eastern Europe and transcontinental regions as far south as 40°N. The oceanic climate exists in an arc spreading across
1560-551: The east. The nearest city is Santa Cruz de La Sierra , the largest city in Bolivia. The valley was originally populated by people of the Chane culture dedicated to agriculture, hunting and gathering. The Chanes are famous for their densely populated villages, their ceramics and graphic designs, and most importantly the construction of the temple at El Fuerte de Samaipata . They cultivated mainly corn and peanuts and were rather peaceful. There are several Chane burial sites all through
1612-635: The exposed areas of the High Atlas , some mountainous areas across southern Europe , mountainous sections of North America , including parts of the southern Appalachians and the Central America Volcanic Arc . In South America , it can be found mainly in temperate mountainous areas in the Tropical Andes , Venezuelan Coastal Range , the highest elevations of Serra do Mar in Southeastern Brazil , and tepuis of
Samaipata - Misplaced Pages Continue
1664-817: The hottest month, the average temperature is below 22 °C (72 °F), and at least four months feature average temperatures higher than 10 °C (50 °F). The average temperature of the coldest month must not be colder than −3–0 °C (27–32 °F), or the climate will be classified as continental. The average temperature variations in the year are between 10–15 °C (50–59 °F), with average annual temperatures between 6–13 °C (43–55 °F). Rain values can vary from 50–500 cm (20–197 in), depending on whether mountains cause orographic precipitation . Frontal cyclones can be common in marine west coast regions, with some areas experiencing more than 150 rainy days annually, but strong storms are rare. Cfb climates are predominant in most of Europe except
1716-765: The immediate west and northwest in transition for humid continental , the remainder of Cape Cod ) and northeastern Georgia both in the eastern United States . It is also found in the highest portions of the Brazilian state of Bahia and Roraima (in transition or strongly influenced for Cwb ), Brønnøy Municipality in Nordland at 65.28 °N ( Norway north-central coast), the provinces of Sabah (northeastern Malaysia ), and Baluchistan , Pakistan . Although there are more or less rare places associated with relatively isolated mountainous regions (e.g., North Oceania islands and China ). The subtropical highland climate
1768-561: The isotherm used. Typically, these areas in the warmest month experience daytime maximum temperatures below 17 °C (63 °F), while the coldest month features highs slightly above freezing and lows near or just below freezing while keeping the average warm enough. It typically carries a Cfc designation, though very small areas in Argentina and Chile have summers sufficiently short to be Cwc with fewer than four months over 10 °C (50 °F). This variant of an oceanic climate
1820-534: The local Guarani natives that had invaded the valley prior to the arrival of the Spaniards. Beginning in the 1880s, some Arab families settled in Samaipata, they were followed by a few Croatians and Italians, all of which mixed and assimilated into the local population. After the road that passes by the town was paved in the 1960s, many migrants from all over Bolivia (mainly from nearby Santa Cruz , but also Cochabamba and Sucre) settled in this little town. Since
1872-542: The north of Croatia and Serbia and some parts of the Czech Republic , also have oceanic climates; these are generally near the boundary for being humid continental . The line between oceanic and continental climates in Europe runs in a generally north to south direction. For example, western Germany is more impacted by milder Atlantic air masses than eastern Germany. Thus, winters across Europe become colder to
1924-818: The northeast, as global temperatures became warmer towards late 20th and early 21st century. They are the main climate type in New Zealand and the Australian states of Tasmania , Victoria , and southeastern New South Wales (starting from the Illawarra region). In North America, they are found mainly in Vancouver Island and neighbouring parts of British Columbia , as well as many coastal areas of southeast Alaska . There are pockets of this iteration of Cfb climates in South American countries, mostly in regions of southern Chile and Argentina, parts of
1976-655: The northeastern coast of Honshu , such as Mutsu, Aomori in Japan, feature this climate, which is rare in Asia due to the lack of a west coast in the middle latitudes. Île Amsterdam and Île Saint-Paul , both part of the French Southern and Antarctic Lands , are located in the subtropics and have an oceanic climate (akin to Tristan da Cunha; see above). Temperate oceanic climates, also known as "marine mild winter" climates or simply oceanic climates, are found either at middle latitudes . They are often found on or near
2028-620: The northwestern coast of North America from the Alaskan panhandle to northern Washington . In addition, some east coast areas such as Block Island , Cape Cod , Martha's Vineyard , and Nantucket have a similar climate. And in the highlands of Central and South America with the variant Cfb. An extensive area of oceanic climates distinguishes the coastal regions of southern Chile and extends into bordering Argentina . The only noteworthy area of maritime climate at or near sea-level within Africa
2080-763: The ocean. Oceanic climates in Europe occupy a large stretch of land, from Norway 's Atlantic coast, Ireland and the United Kingdom and southeast to some parts of Turkey . Western Europe is almost exclusively oceanic between 45°N to 54.913°N; including most of France (away from the Mediterranean), nearly all of Belgium , the Netherlands , Austria , most of Luxembourg , most of Denmark , western Germany , northwestern Switzerland , south coast and western areas of Norway north to Skrova and extreme southern Sweden . While most of Southern Europe
2132-842: The peaks in the highest mountain ranges have this climate (including the Blue Mountains in Jamaica and Cerro Maravilla in Puerto Rico ), with only Hispaniola 's Cordillera Central and Chaîne de la Selle having significant urban settlements under this climate zone, such as cities like Kenscoff in Haiti and Constanza in the Dominican Republic . Areas with subpolar oceanic climates feature an oceanic climate but are usually located closer to polar regions, with long but relatively mild winters and short, cool summers. As
Samaipata - Misplaced Pages Continue
2184-650: The provinces of Chubut , Santa Cruz , and southeast Buenos Aires province in Argentina. In Western Asia , the climate can be found on the Black Sea coast of northern Turkey and Georgia , often transitional to humid subtropical . While Cfb zones are rare in Africa, one dominates the coastline of the Eastern Cape in South Africa . The climate subtype can also be found in Nantucket , Massachusetts (in
2236-419: The regions, but are more common in subtropical highland climates where these air masses meet more frequently due to the influence of hotter weather in the subtropics or tropics, especially in monsoon-influenced climates. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. Most oceanic climate zones, however, experience at least one snowfall per year. Snowfall
2288-615: The shape of the continent. Only in Europe do they penetrate far inland, where they eventually transition into warm-summer humid continental climates ; in other continents, they are blocked by a large mountain range or limited by nearby oceans. The North Atlantic Gulf Stream , a tropical oceanic current that passes north of the Caribbean and up the East Coast of the United States to North Carolina , then heads east-northeast to
2340-621: The south and defeated both the Incas and Chanes. The Guaranis continued raiding the valley and the region until the 19th century. In 1618, Pedro de Escalante y Mendoza founded Samaipata, as a point of contact between Santa Cruz and Vallegrande . The town moved from its original location in a place known as Castilla to its current location a few kilometers west. Samaipata is quite cosmopolitan and diverse. Samaipateños from old families are descendants of Spanish colonists from Vallegrande and Santa Cruz (many of whom were of Sephardic origin) and
2392-448: The tropics, a subtropical highland climate typically features mild weather year-round. Temperatures there remain relatively constant throughout the year and snowfall is seldom seen due to warmer winters than most oceanic climates. Areas with this climate feature monthly averages below 22 °C (72 °F) but above either 0 °C (32 °F) or −3 °C (27 °F) depending on isotherm used. At least one month's average temperature
2444-627: The valleys and pampas of Santa Cruz between the Siberia mountain ridge and the Guapay River. The region was later conquered by the Incas as they expanded to the southeast from their native Peru. The Incas reached a pact with the Chanes and built a city at El Fuerte de Samaipata . In the 16th century, Guarani warrior tribes, called Chiriguanos by the Incas and Spanish, invaded the valley from
2496-461: The vineyards of Samaipata are within walking distance from the town center. Most vineyards provide guided tours which include a wine tasting at the end of the tour. Nearby is the pre- Inca ruin of El Fuerte de Samaipata . It is not actually a fort, but a temple. This is Bolivia's largest pre-Inca site. Declared a world heritage site by UNESCO in 1998, this archaeological complex presents pre-Inca (Chane), Inca, and colonial Spanish ruins. The temple
2548-414: The west coast of continents; hence another name for Cfb, "marine west coast climates". In addition to moderate temperatures year-round, one of the characteristics is the absence of a dry season. Except for Europe , this type of climate is confined to narrow bands of territory, largely in mid or high latitudes, although it can appear in elevated areas of continental terrain in low latitudes, e.g. plateaus in
2600-488: The winter months cold fronts called Surazos come from the Argentine Pampas and enter the plains and valleys of Santa Cruz , these cold winds combined with the altitude can reach temperatures below freezing. In the summer, the days are warm and the nights cool. Frost occurs on nine days in an average year, mostly in the winter months. Samaipata has a wine culture dating back to the first Spanish settlements in
2652-571: The year, similar to other oceanic climates, but unlike these climates, they have a high diurnal temperature variation and low humidity, owing to their inland location and relatively high elevation. Subtropical highland climates with monsoon influence ( Cwb ) have distinctive wet summers and dry winters . In locations outside the tropics, other than the drying trend in the winter, subtropical highland climates tend to be essentially identical to an oceanic climate, with mild summers and noticeably cooler winters, plus, in some instances, some snowfall. In
SECTION 50
#17327648274682704-583: Was originally built by the Arawak people most likely belonging to the Chane culture that inhabited the surrounding valleys and the pampas to the East. The temple was carved on an enormous rock. The Incas also built a city adjacent to the temple and established trade and alliances with the Chanes to protect the territories from the constant invasions of warrior Guarani tribes that raided the region from time to time. It
#467532