Uniendo la Costa Atlantica-Uniendo Nicaragua

Somos Miskitos, Sumus, Ramas, Criollos, Mestizos, y Garifonas

Pagina Principal de SCA

Estatutos

Nuestra Vision

Sobre Nosotros

Membresia

Palo de Mayo

Libro de Huepedes

Programas SCA

Galleria de Fotos

Carrera de Canoas

Noticias

Eventos SCA

Donaciones

Voluntarios

English

Bluefields Medical Center

Community Clinics

Community Role Models

About us

Volunteer Center

Mosquitia History

Our Vision

SCA Programs

SCA Events

membership

Mosquitia News

Autonomy Laws

hurricane relief

Guest Book

sca donation

Photo Gallery

Miskito Dictionary

Memories Page

business portal

Community Links

Pagina De Memorias

Otras Paginas

Our History

In 1502 Cristopher Columbus was the first European known to have reached what is now Nicaragua as he sailed south along the Central America East Coast. On his fourth voyage Columbus sailed alongside and explored the Mosquito Coast on the east of Nicaragua. However, it was not until 1524, that Conquistador Francisco Hernández de Córdoba founded the first Spanish permanent settlements, including two of Nicaragua's principal towns: Granada on Lake Nicaragua, León east of Lake Managua and also Nueva Segovia in Nicaragua's north. Settled as a colony of Spain within the kingdom of Guatemala in the 1520s, Nicaragua became a part of the Mexican Empire and then gained its independence as a part of the United Provinces of Central America in 1821 and as an independent republic in its own right in 1838. The Mosquito Coast based on Bluefields on the Atlantic was claimed by the United Kingdom and its predecessors as a protectorate from 1655 to 1850; this was delegated to Honduras in 1859 and transferred to Nicaragua in 1860 through a treaty known as Clayton/Bulwar Treaty, though it remained autonomous until 1894. Through a treaty known as Chamorro/Bryan, Jose Santos Zelaya managed to negotiate with the Queen of England for the annexation of this region to the rest of Nicaragua. In his honour the entire region was named Zelaya, though this was later changed under the Sandinista government and it was divided into two autonomous regions. Nicaragua was considered by the Spanish Kingdom as a very important colony, considering it had a natural route in which it would permit transportation of good from the Atlantic Ocean to the Pacific Ocean. However, at the time it was not considered of much value for the mining of minerals. Although there were high concentrations of gold, they were smaller compared to the amounts in the other Spanish colonies. During the early years of the colony Nicaragua produced many goods which gave it some prosperity, and there was an ever increasing desire to build a canal along the San Juan River, through Lake Nicaragua and across the isthmus of Rivas. In the 1800s Nicaragua experienced a wave of immigration, primarily from Europe. In particular, families from Germany, Italy, Spain, France and Belgium generally moved to Nicaragua to set up businesses with money they brought from Europe. They established many agricultural businesses such as coffee and sugar cane plantations, and also newspapers, hotels and banks. In the late 1800s, the United States government negotiated with President Jose Santos Zelaya to lease the land so they could build a canal through Nicaragua. However, Zelaya opposed the United States controlling Nicaraguan sovereign land and sought assistance from Japan and Germany to build the canal. It was determined to be too costly. Furthermore, opponents of the canal suggested Momotombo posed a threat of volcanic activity, as depicted on a Nicaraguan stamp, though it was far away from the site.

The eastern Caribbean lowlands of Nicaragua form the extensive (occupying more than 50 percent of national territory) and still sparsely settled lowland area known as the Costa de Mosquitos (Miskito Coast). The Caribbean lowlands are sometimes considered synonymous with the former department of Zelaya, which is now divided into the North Atlantic Autonomous Region (Región Autonomista Atlántico Norte, RAAN) and the South Atlantic Autonomous Region (Región Autonomista Atlántico Sur, RAAS) and constitutes about 45 percent of Nicaragua's territory. These lowlands are a hot, humid area that includes coastal plains, the eastern spurs of the central highlands, and the lower portion of the Río San Juan basin. The soil is generally leached and infertile. Pine and palm savannas predominate as far south as the Laguna de Perlas. Tropical rain forests are characteristic from the Laguna de Perlas to the Río San Juan, in the interior west of the savannas, and along rivers through the savannas. Fertile soils are found only along the natural levees and narrow floodplains of the numerous rivers, including the Escondido, the Río Grande de Matagalpa, the Prinzapolka, and the Coco, and along the many lesser streams that rise in the central highlands and cross the region en route to the complex of shallow bays, lagoons, and salt marshes of the Caribbean coast.

Climate

Temperature varies little with the seasons in Nicaragua and is largely a function of elevation. The tierra caliente, or the "hot land," is characteristic of the foothills and lowlands from sea level to about 750 meters of elevation. Here, daytime temperatures average 30° C to 33° C, and night temperatures drop to 21° C to 24° C most of the year. The tierra templada, or the "temperate land," is characteristic of most of the central highlands, where elevations range between 750 and 1,600 meters. Here, daytime temperatures are mild (24° C to 27° C), and nights are cool (15° C to 21° C). Tierra fría, the "cold land," at elevations above 1,600 meters, is found only on and near the highest peaks of the central highlands. Daytime averages in this region are 22° C to 24° C, with nighttime lows below 15° C.

Rainfall varies greatly in Nicaragua. The Caribbean lowlands are the wettest section of Central America, receiving between 2,500 and 6,500 millimeters of rain annually. The western slopes of the central highlands and the Pacific lowlands receive considerably less annual rainfall, being protected from moistureladen Caribbean trade winds by the peaks of the central highlands. Mean annual precipitation for the rift valley and western slopes of the highlands ranges from 1,000 to 1,500 millimeters. Rainfall is seasonal--May through October is the rainy season, and December through April is the driest period.

During the rainy season, Eastern Nicaragua is subject to heavy flooding along the upper and middle reaches of all major rivers. Near the coast, where river courses widen and river banks and natural levees are low, floodwaters spill over onto the floodplains until large sections of the lowlands become continuous sheets of water. River bank agricultural plots are often heavily damaged, and considerable numbers of savanna animals die during these floods. The coast is also subject to destructive tropical storms and hurricanes, particularly from July through October. The high winds and floods accompanying these storms often cause considerable destruction of property. In addition, heavy rains (called papagayo storms) accompanying the passage of a cold front or a low-pressure area may sweep from the north through both eastern and western Nicaragua (particularly the rift valley) from November through March. Hurricanes or heavy rains in the central highlands, where agriculture has destroyed much of the natural vegetation, also cause considerable crop damage and soil erosion. In 1988 Hurricane Joan forced hundreds of thousands of Nicaraguans to flee their homes and caused more than US$1 billion in damage, most of it along the Caribbean coast.

Other facts

Area:
total: 129,494 km²
land: 120,254 km²
water: 9,240 km²

Area - comparative: slightly smaller than the state of New York

Climate: tropical in lowlands, cooler in highlands

Terrain: extensive Atlantic coastal plains rising to central interior mountains; narrow Pacific coastal plain interrupted by volcanoes; Lake Nicaragua (or Lake Cocibolca) is the second largest lake in Latin America after Lake Titicaca. (unless Lake Maracaibo is considered a lake and not a bay).

Elevation extremes:
lowest point: Pacific Ocean 0 m
highest point:
Mogoton 2,438 m

Natural resources: gold, silver, copper, tungsten, lead, zinc, timber, fish

Land use:
arable land: 9%
permanent crops: 1%
permanent pastures: 46%
forests and woodland: 27%
other: 17% (1993 est.)

Irrigated land: 880 km² (1993 est.)

Natural hazards: destructive earthquakes, volcanoes, landslides, and occasionally severe hurricanes

Environment - current issues: deforestation; soil erosion; water pollution; Hurricane Mitch damage

Environment - international agreements:
party to:
Biodiversity, Climate Change, Climate Change-Kyoto Protocol, Desertification, Endangered Species, Hazardous Wastes, Nuclear Test Ban, Ozone Layer Protection, Wetlands
signed, but not ratified: Environmental Modification, Law of the Sea


All information on this site is the exclusive property of SOMOS COSTA ATLANTICA.  The copying, reproduction, or sales in part or its entirety, without the expressed consent of this organization is prohibited.  All rights reserved. Copywrite 2007.

Please call or write us at:
(650) 273-3778 or (954) 237-5629

 
admin@somoscostaatlantica.org

You can deposit your contribution to Bank of America, account #0437766302.  You can also mail your contribution 49 Lausanne Ave, Daly City CA 94014

Website powered by Network Solutions®