There are 16 high school codes in Honduras today, according to the ACT. The full list is shown below by city, with name of each high school and the city where the school is located (based on the ACT official site). You can search a school code by pressing “Ctrl” + “F” and then type school name or 6-digit school code.
Map of Honduras
High School Codes by City
- High School Code
- 862040
- High School Code
- 862145
- High School Code
- 862020
- High School Code
- 862199
- High School Code
- 862150
- High School Code
- 862309
- High School Code
- 862201
- High School Code
- 862295
- High School Code
- 862300
- High School Code
- 862240
- High School Code
- 862298
- High School Code
- 862299
- High School Code
- 862340
- High School Code
- 862104
- High School Code
- 862220
- High School Code
- 862021
The above lists CEEB codes (College Entrance Examination Board) for all accredited Honduras high schools. Please be informed that the list of high school codes in Honduras may change throughout the year. If you can’t find codes for the high schools of your interest, please write to us or come back at a later time. We will update our database soon after a new high school code is added to the country of Honduras.
Country Abbreviations
HND is the three-letter country code of Honduras, and HN is the two-letter country code of Honduras. The two-letter suffix is used in top-level domains on the Internet as .hn.
Morphology
In its general features the territory of Honduras corresponds to a vast plateau, extending from one bank of the Isthmus to the other and crossed by mountain ranges with a prevalent WE trend. Geologically, the country rests on a base of crystalline rocks, which crops out widely in the northern section. Bent in the Paleozoic era and subsequently leveled by slow erosion, this hoof was violently affected by the orogenetic movements of the Cenozoic, typical of the entire isthmic area, which caused numerous fractures with consequent release of magma; lava expansions and volcanic systems are present in the southern part of the country, connecting to that alignment of volcanoes that runs throughout Central America. Above the base there are Mesozoic and Cenozoic sedimentary layers, the latter particularly extensive in the western section of the plateau; a quaternary coveragefinally it characterizes the Mosquitia and the north-eastern coastal plain. The orography is complex, especially in the central and more compact area of the plateau, dominated by short chains (Montañas de Comayagua, Cordillera de Montecillos, Sierra Opalaca, Montaña La Sierra etc.) in several points above 2000 m and culminating in 2849 m of Cerro Las Minas, in the Sierra de Celaque; from this nucleus of other lands, a series of mountain ridges branches off towards the N, with a more clearly defined SW-NE course, such as the Cerros de Cangreja (2435 m), the Montaña La Esperanza, the Sierra de Agalta (2590 m) and the Montañas de Colón, which sometimes reach the Caribbean coast, resulting in a coast in some parts high and rocky: such it is, p. eg, the one faced by the Islas de la Bahía archipelago. The Atlantic coastal front extends for 500 km, from the Golfo de Honduras to Cabo Gracias in Dios, and is bordered by lagoons (Los Micos, Guaimoreto, Ibans Ébano, Brus, Caratasca etc.); here the major Honduran plains extend, which however occupy only a limited portion of the total territory. Among the main ones are the plain of Sula, extending to the mouth of the Aguán river, and above all the Mosquitia, largely marshy; another large flat area faces SW on the Gulf of Fonseca, where the Choluteca river flows.
Hydrography
The hydrographic network of Honduras is on the whole rather irregular. The sward shift of the watershed causes the major rivers to flow into the Sea of the Antilles; they descend through valleys that are often tortuous, but which still represent very useful means of access within the country: the Ulúa, the most important Honduran river, which cuts through the rich plain of Sula, the aforementioned Aguán and the Patuca; the latter is the longest watercourse in the country (excluding the Río Coco which marks a large part of the border with Nicaragua), of which it crosses the entire south-eastern section, but of little importance as a communication route as it largely corresponds to the semi-desert Mosquitia. Finally, there are two main rivers on the Pacific side: the Goascorán, which marks the border with El Salvador for a good stretch, and the Choluteca, which springs from the mountains near Tegucigalpa.