Atlas of Pidgin and Creole Language Structures Online

Nicaraguan Creole English (or Miskito Coast Creole English) is spoken as a first language by several groups of people: ethnic Creoles, the Rama, Nicaraguan Garifuna, and some Miskitos, and as a second language by other Miskitos and some Mestizos. It is mainly spoken (nowadays as a minority language) in the two Nicaraguan Autonomous Regions of the Atlantic Coast but also elsewhere in Nicaragua, the United States, and other small diaspora communities. Estimates of speaker numbers vary between 35,000 and 50,000.

Nicaraguan Creole English can be considered one of the oldest English-based varieties in the Americas. Belizean Creole constitutes a direct off-shoot of Nicaraguan Creole English which, on the other hand, has undergone influence from several other Western Caribbean Creoles, obscuring the genetic relationships of the creoles of the region in question.

Speakers themselves identify at least the variants of Bluefields, the Corn Islands, Pearl Lagoon, Rama Cay, Orinoco, and Bilwi. It is commonly felt that the urban variety of Bluefields should constitute the basis for standardization. On the other hand, Spanish is much more present in Bluefields than in rural communities. Over recent years, there have been signs that the Spanish–Creole English diglossia has started to leak. Nevertheless, it has been postulated that there continue to exist separate Anglo, "costeño" (coastal) and Black identities within the Creole population and those most closely identifying with the Anglo identity are unlikely to be in favor of bilingual Creole-Spanish programs any more than they were in the 1980s. Indeed, Standard English is valued not only as an international language but also as the foundation of that particular facet of Creole identity as a cross of a class and an ethnic position.

The default lect in APiCS is constituted by data gathered in Bluefields and surrounding locations in 2006-2007. It appears quite clear that Nicaraguan Creole English constitutes a genuine instance of decreolization when compared to materials collected in the early 1970s.

Unless otherwise specified, all examples in APiCS were recorded in Nicaragua in 2006-2007 (see Nicaragua project recordings CD).