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Rila Monastery Nature Park Management Plan - part - usaid

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February 2004<br />

<strong>Rila</strong> <strong>Monastery</strong> <strong>Nature</strong> <strong>Park</strong><br />

Geology<br />

The map indicates the location of the 6 most important geological formations<br />

within <strong>Rila</strong> <strong>Monastery</strong> <strong>Nature</strong> <strong>Park</strong>, as described in the Descriptive Section of the<br />

<strong>Management</strong> <strong>Plan</strong>, which characterize the main geological periods. The map shows a<br />

clear predomination of biotite gneisses and schists dating from the Proterozoic. Other<br />

common types of rock are the biotite granites and granodiorites, which occupy the<br />

northwestern, eastern and some areas of the southern portion of the <strong>Park</strong>. Almost the<br />

entire northeastern portion of RMNP is made up of fine-grained biotite granites.<br />

The remaining object categories are as per the Base Map.<br />

Digital models by Agrolesproject PLC, as well as data provided by consultants<br />

to the BCEG Project, have served as the basis for compiling this map.<br />

Note: The map shows also the territory along Rilska River neighboring the<br />

<strong>Nature</strong> <strong>Park</strong><br />

<strong>Rila</strong> <strong>Monastery</strong> <strong>Nature</strong> <strong>Park</strong><br />

<strong>Management</strong> <strong>Plan</strong> - Draft<br />

2004 - 2013

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