Town/City: 

Kingston

State/Province: 

Kingston & St-Andrew

Country: 

Jamaica

Latitude/Longitude: 

18N, 76.8W

Information supplied by

Isabelle Drouin-Brisebois

drouin@scar.utoronto.ca

255 Shaw St., Toronto, Ontario, M6J 2W7

 

 
 
 

Dated Tue Dec 14 04:20:44 1999


Information Topics:


City Description:

Kingston, which is the capital of Jamaica, is located on the south-eastern coast of the island. It had a population of 97,000 people in 1991, and is situated in the most densely populated region on the island. To the north of Kingston lie the Blue Mountains which trend along the west-north-west to east-south-east axis of the island.

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Climate:

Jamaica is subject to tropical marine climate with mean daily temperatures ranging from a 26 C low in February to a 28 C high in August. The number of hours of sunshine does not vary very much from 8.2 hours. Most of the annual precipitation in Jamaica falls on the northern slopes of the mountain ranges, with southern coastal plains receiving less than 1,500 mm per year. Much of the precipitation in Jamaica falls in a few very high intensity and high magnitude events; tropical storms and hurricanes occur quite often between the months of July and November. The mean relative humidity on the southern coast ranges from a 71% low in August and a 77% high in October.

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Basic Hydrogeology:

Jamaican geology greatly affects the occurrence and availability of water resources. Due to the location of the Blue Mountains, the southern half of the island contains major alluvial lowlands representing 15 % of the total area of the island. Kingston is located over a thick bed of quaternary permeable to moderately permeable alluvium which is underlain by tertiary limestones which have variable degrees of karstification. Because groundwater is the dominant water resource in coastal alluvial plains, the most important hydrostratigraphic unit in Kingston is the alluvium aquifer. The aquifer gets recharge from both rainfall and from rivers like the Rio Cobre which descends from the mountainous areas and flows over the alluvium region where seeping and channel losses occur.

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Water Use:

Due to the very high population density, the tourist attractions and the lack of important agricultural activities in Kingston, the water use is almost entirely for domestic, industrial and tourism industry purposes.

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Groundwater Issues:

There are many groundwater issues in Kingston. Because of the lack of fresh water in the form of lakes and rivers in the area, there is a great dependence on groundwater as a resource. The more prominent issues are: groundwater supply and resource management, water quality and health related issues as well as environmental issues.

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Groundwater Problems:

The main groundwater problems in Kingston are:

1. Lack of recharge areas due to urbanisation without proper groundwater resource planning.

2. Contamination by sewage which can lead to outbreaks of dysentery and cholera.

3. Pumping at a rate that results in recurring water shortages in dry seasons causing economic losses and conflicts among water users

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Solutions:

In 1995, the Water Resource Act (WRA) was passed in Jamaica. The WRA has as a mission:

- the continual assessment and proper management of water resources

- the promotion of conservation and protection

- the promotion of optimal development

- ensuring that the water supply is adequate and resolve conflict between industry and other water users


The WRA has resulted in a detailed proposed plan of action which includes:

- taking an inventory of resources and demands for domestic, industrial and touristic use

- establishing water quality control areas

- abstraction licensing

- groundwater risk mapping (mapping groundwater vulnerability to contamination)

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References and Other Author(s):

Bryce, R., 1986,  A geotechnical classification of Jamaican rocks; in Proceedings of a workshop on the status of Jamaican geology, Kingston March 1984, (ed.) Ahmad, R.,  The Geological Society of Jamaica.

Jackson, T. A., 1986, The petrology of Jamaican cretaceous and tertiary volcanic rocks and their tectonic significance; in Proceedings of a workshop on the status of Jamaican geology, Kingston March 1984, (ed.) Ahmad, R.,  The Geological Society of Jamaica.

Kurian, G. T., 1992, Atlas of the Third World Second Edition, Facts on File, NY.

Walters, M. O. and Herbert, T., 1998, Application of a linked watershed waterbody model to Kingston Harbour in Jamaica; in Hydrology in the Humid Tropic Environment, (ed.) Johnson, A. I. and Fernandez-Jauregui, C. A., IAHS Publication no. 253.

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Contacts:

For interesting historical facts on Jamaica:
www.rootsweb.com/~jamwgw/map1.htm

For information on the Water Resource Act and geological and hydrogeological information on the regions of Jamaica:
www.wra.ja.org/act.htm
www.wra.ja.org/devplan.htm#plan
www.wra.ja.org/jamaica.htm
www.wra.ja.org/riskmap.htm
www.wra.ja.org/policy.htm
www.wra.ja.org/policy.htm#2

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