Whereas our immediate concerns must be with management, protection, and the development of economically and ecologically viable activities, the ultimate success of environmental projects globally will only be obtained by winning long-term commitment to non-destructive human-nature interaction. To ensure realization of this vision, Programme for Belize expends much energy and resources, directly and indirectly on community and education outreach in the villages surrounding the RBCMA and throughout the country.

Although there are no human settlements currently located on the lands comprising the RBCMA, Programme for Belize makes a particular effort to involve other Belizeans in our economic projects wherever possible. We concentrate on the villages surrounding the RBCMA. So far, PFB has assisted in the establishment of several cultural groups. Handicrafts made by these groups are sold to visitors of the RBCMA. PFB also extends assistance to these groups in honing their craftsmanship as well as their business skills by coordinating with other organizations or groups in the country for training. As tourism, horticulture, and forestry develop, job opportunities for each of these activities will simultaneously arise, providing much needed employment to the area.

The commitment of future generations to environmental ethics can best be secured through directed environmental education programs which teach our children to respect their human and natural environments. To this end, PfB has implemented various educational initiatives. We have worked with the Government of Belize in the past facilitating the incorporation of environmental science into the curricula for elementary schools and visiting schools to conduct ecology-related educational lectures. We continue to deliver these lectures today to various elementary schools in the greater RBCMA region and other presentations on environmental topics to secondary and tertiary level students from all areas of Belize. We also continue to host on site a number of local, secondary and tertiary level student classes throughout the year in furthering and expanding an appreciation of the sciences and ecology at the field level. There are more than 1,000 students visiting the RBCMA annually. PfB reaches international students by hosting ‘Save the Rainforest’ courses which include one week of terrestrial ecology and one week of marine ecology.

The merit of these efforts has encouraged us to expand our outreach programs to benefit more Belizeans economically and to touch the hearts and minds of more students nationally and internationally. Outreach remains a priority component of all our activities.

The topography of the area is characterized by flat rolling hills and a moderate strip of land with steeper slopes between 15 and 25 degrees. There are also thin ridges of land over 25 degrees with steep sided scarps that are part of the terrace-like topography of the region. A large percentage of the land is in upland forests. Further, a significant portion is comprised of marshes and mesic and swamp forests. Riverine systems are particulary distinct throughout the RBCMA and the New River Lagoon is a unique ecological feature. Finally, the two large tracts of Savannah habitat are significant, especially on a regional scale of ecosystem diversity.

The climate of the area is described as dry tropical and subtropical moist according to the Holdrige Life Zones. There is a clear seasonal precipitation gradient in the Rio Bravo area resulting in a dry season from February through April with evaporation rates higher than precipitation and a wet season from June through January. The total average annual rainfall is approximately 60 inches. The temperature is somewhat constant throughout the year with some seasonal fluctuation between cooler and warmer months with a range from 50 degrees F to 95 degrees F with an average of 79 degrees F. All of these data vary greatly from year to year.

The eastern portion of the area lies on the north Belizean coastal plain, being low-lying and underlain by limestone and soft marl blanketed over extensive areas by Pleistocene alluvial deposits. The principal topographical features consist of escarpments aligned SW-NE across the landscape that guide the drainage of the New River, Booth’s River, and Rio Bravo. The escarpments become more pronounced from east to west and above the most westerly the subdued relief of the coastal plain changes abruptly to the more broken, locally rugged, landscape of the Bravo Hills land system.