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Geology and Resource Assessment of the Venezuelan ... - USGS

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CAUTIONS RELATING TO USE OF THE MAPS<br />

One <strong>of</strong> <strong>the</strong> advantages <strong>of</strong> digital maps is <strong>the</strong> ability to change <strong>the</strong> map scale.<br />

However, <strong>the</strong> users <strong>of</strong> this disc should respect <strong>the</strong> intentions <strong>of</strong> <strong>the</strong> authors <strong>and</strong><br />

recognize certain limitations <strong>of</strong> digital maps. The <strong>Venezuelan</strong> MF series maps on this<br />

disc are intended to be used at a scale <strong>of</strong> 1:500,000; <strong>the</strong>y are not intended to be used at<br />

a more detailed (larger) scale. A Venezuela 2°x3° degree quadrangle measures about<br />

17 inches high by 26 inches wide at 1:500,000 scale.<br />

The "quadrangle" maps in this publication cover somewhat more or less than<br />

2°x3° depending on <strong>the</strong> specific map. For instance, <strong>the</strong> Guri map (Cox <strong>and</strong> o<strong>the</strong>rs,<br />

1993) contains all <strong>of</strong> <strong>the</strong> Guri quadrangle <strong>and</strong> <strong>the</strong> sou<strong>the</strong>rn part <strong>of</strong> <strong>the</strong> Tucupita<br />

quadrangle. The entire study area in <strong>the</strong> sou<strong>the</strong>ast part <strong>of</strong> Venezuela, known as <strong>the</strong><br />

<strong>Venezuelan</strong> Guayana Shield, is about 36 inches tall at 1:1 million scale, which is <strong>the</strong><br />

published scale for Bulletin 2062 (<strong>USGS</strong> <strong>and</strong> Corporación Venezolana de Guayana,<br />

Técnica Minera, C.A., 1993).<br />

Fur<strong>the</strong>rmore, <strong>the</strong> geologic map is primarily a bedrock map, which depicts<br />

geologic materials present beneath <strong>the</strong> soil or relatively thin mantles <strong>of</strong> surficial<br />

deposits, not necessarily <strong>the</strong> surficial materials <strong>the</strong>mselves. Indeed, <strong>the</strong> study area<br />

contains so much surficial cover <strong>and</strong> st<strong>and</strong>ing water that much <strong>of</strong> <strong>the</strong> mapping was<br />

accomplished with geophysical methods as opposed to directly examining rock<br />

outcrops.

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