Southwest of mainland Jamaica lies Pedro Bank, an area of shallow seas, with a number of cays (low islands or reefs), extending generally east to west for over 160 km (99 mi).
Jamaica (which is a very mountainous country) and the other islands of the Antilles evolved from an arc of ancient volcanoes that rose from the sea millions of years ago.
[1] These eastern mountains are formed by a central ridge of metamorphic rock running northwest to southeast from which many long spurs jut to the north and south.
[1] The Blue Mountains rise to these elevations from the coastal plain in the space of about 16 kilometres (9.9 mi), thus producing one of the steepest general gradients in the world.
[1] To the west, in the central part of the country, are two high rolling plateaus: the Dry Harbour Mountains to the north and the Manchester Plateau to the south.
[1] Sinkholes, caves and caverns, disappearing streams, hummocky hills, and terra rosa (residual red) soils in the valleys are distinguishing features of a karst landscape; all these are present in Jamaica.
[1] The Cockpit Country is pockmarked with steep-sided hollows, as much as 15 metres (49 ft) deep in places, which are separated by conical hills and ridges.
[1] On the north, the main defining feature is the fault-based "Escarpment", a long ridge that extends from Flagstaff in the west, through Windsor in the centre, to Campbells and the start of the Barbecue Bottom Road (B10).
[citation needed] The Barbecue Bottom Road, which runs north-south, high along the side of a deep, fault-based valley in the east, is the only drivable route across the Cockpit Country.
[citation needed] In the southwest, near Quick Step, is the district known as the "Land of Look Behind," so named because Spanish horsemen venturing into this region of hostile runaway slaves were said to have ridden two to a mount, one rider facing to the rear to keep a precautionary watch.
[1] Where the ridges between sinkholes in the plateau area have dissolved, flat-bottomed basins or valleys have been formed that are filled with terra rosa soils, some of the most productive on the island.
[1] Since the southwestern half of the island lies in the rain shadow of the mountains, it has a semiarid climate and receives fewer than 760 millimetres (29.9 in) of rainfall annually.
[1] Jamaica lies in the Main Development Region for tropical cyclone activity in the Atlantic, and as a result, it sometimes experiences significant storm damage.
[10] Although most of Jamaica's native vegetation has been stripped in order to make room for cultivation, some areas have been left virtually undisturbed since the time of European colonization.
[1] Indigenous vegetation can be found along the northern coast, from Rio Bueno to Discovery Bay, in the highest parts of the Blue Mountains, and in the heart of the Cockpit Country.
Over-building, driven by powerful market forces as well as poverty among some sectors of the population, and destructive exploitation contribute to the decline of ocean and coastal resources.
This study aims to inform the relevant stakeholders of the feasibility of implementing environmental fees as well as the likely impact of such revenue generating instruments on the current tourist visitation rates to the island.
The findings of the study show that the "label" of the tax and as well as the respondent's awareness of the institutional mechanisms for environmental protection and tourism are important to their decision framework.
It has been shown that if an environmental tax of $1 per person were introduced it would not cause a significant decline in visitation rates and would generate revenues of US$1.7M per year.