Rila Monastery Nature Park Management Plan - part - usaid

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February 2004 Fig. 4: 3D model of Rila Monastery NP – view from the east towards the Rilska River Valley. Legend - altitude in meters above sea level; green line – park boundary. The highest point in Rila Monastery NP is Riletz Peak (2,713 m). Malyovitsa Peak (2,729 m) is higher, but it is located on the boundary with Rila National Park. The average altitude of terrains within RMNP is 1,750m asl In this section of Rila Mountain is the principal orographic and hydrographic junction of the entire massif: Kanarata Peak (2,691 m), defining both the Main Balkan Watershed (between the Aegean and the Black Sea basins), and the watershed between the two principal drainage areas of the Aegean Basin, those of Belishka and Rilska Rivers. Residual relief The shaping of Rila as a solid, high mountain started as early as the Paleozoic, when the metamorphic rocks were intruded by granites and the formation of the batolite body as a dome-anticline took place. The latter represents a dome-like morphostructure shaped by deep peripheral faults, clearly visible in the present-day relief. The large dome-shaped body has been subjected over time to constant, spatially differentiated, mostly positive tectonic movements, whereby it has grown in Rila Monastery Nature Park Management Plan -Draft 2004 - 2013 28
February 2004 height, reaching towards the end of the Early Tertiary a significant altitude which defines it as a high-mountain plutonic morphostructure. The shaping up of the present-day relief started in the Neogene. During that period, as well as, subsequently, during the Pliocene and later on, differentiated tectonic movements (stages of arch-like rising alternating with stages of repose) triggered the occurrence of denudation and planation processes of different intensity. This combination of endogenetic and exogenetic earth forces acting as relief-forming factors has produced the present-day traces of the oldest landscape forms in the area of the Nature Park, observed as level surfaces of denudation. So far, the presence of four clearly defined levels of denudation has been established, the oldest and the highest of which is the one dating from the Old Miocene, formed along the ridges of the 2,200-2,450 meter altitude zone, and subsequently reactivated and transformed by Pleistocene glaciation. Some cirques and cirque lakes remain preserved in its surface. The mountain peaks rising above it are mostly jagged, representing erosional remnants on the Lower Miocene peneplain, re-shaped later on by glacial activity. The best-preserved denudation surface is that of the Early Miocene. It extends over most of the rolling ridges and rounded peaks in the 1,700 to 1,900 m altitude zone. It has an even more pronounced denudation peneplain appearance, since large remains of it are preserved today, despite the bedrock petrographic differences. Within the park territory, this denudation surface is largely displaced as a result of crisscrossing concentric and radial faults, rising therefore, at places to altitudes of 2,000 m. Owing to its rhythmic repetitiveness, Tectonic activity during the Pliocene has formed two denudation surfaces. Against a backdrop of the all-round arch-like rise of Rila Mountain, two stages of tectonic repose are identified, contributing to a marked peneplanation activity. As base-level for these processes served the existing Pliocene (Pontian and Levantine) lakes in the neighboring territories, negative vis-à-vis Rila Mountain. The remains of the older, and higher, Pliocene (early Pliocene) surface are found at different levels within the 1,100 to 1,300 m altitude zone, where they extend over the flat ridges or occur as slope steps. The Early Miocene denudation surface is observed in the lower parts of slopes in the area, occurring in the form of small slope terraces, usually situated at altitudes between 750 and 850 m. In these, cases of fault-induced vertical drop are also observed. This denudation surface is poorly preserved due to fragmentation by the river network going downstream to the neighboring piedmonts. Such fragmentation increases the aggregate area of eroded slopes at the expense of the Early Miocene denudation surface. These processes are most clearly expressed where the surface consists of weaker Paleogene sediments. Especially characteristic of all denudation surfaces in the area is their relatively large altitudinal gradient. It is due to the concentric/step-like and radial faulting, closely related to the permanent dome-like rise of the mountain bulk. Most of the present-day river valleys in Rila run parallel to the direction of radial faulting. Their geomorphologic appearance, however, with the exception of the lowest portions, is mostly influenced by the erosional and accretionary activity of the descending glaciers during the Quaternary. A typical example is the valley of the Rilska River and its tributaries. Rila Monastery Nature Park Management Plan -Draft 2004 - 2013 29
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The Minister of the Environment and
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February 2004 Contents List of Appe
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February 2004 2.5 Sustainable Fores
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February 2004 17. Macromycettes of
Page 9 and 10: February 2004 List of Abbreviations
Page 11 and 12: February 2004 MV Motor Vehicles NAT
Page 13 and 14: February 2004 Glossary of professio
Page 15 and 16: February 2004 extent or playing a s
Page 17 and 18: February 2004 and included in the w
Page 19 and 20: February 2004 Brown-Blanque School
Page 21 and 22: February 2004 assistance the latest
Page 23 and 24: February 2004 and the state institu
Page 25 and 26: February 2004 Conservation signific
Page 27 and 28: February 2004 The Management Plan a
Page 29 and 30: February 2004 (Nature Park) in the
Page 31 and 32: February 2004 Creative Group, the U
Page 33 and 34: February 2004 Subcontractors to the
Page 35 and 36: February 2004 1.0 General informati
Page 37 and 38: February 2004 (Manastirska). The Re
Page 39 and 40: February 2004 Administratively, Ril
Page 41 and 42: February 2004 The St. Luke Hermitag
Page 43 and 44: February 2004 Table 4: Distribution
Page 45 and 46: February 2004 Cultures Act. EFACA c
Page 47 and 48: February 2004 facilities, restauran
Page 49 and 50: February 2004 According to FI 2000,
Page 51 and 52: February 2004 affect the water outl
Page 53 and 54: February 2004 2.0 Description of ab
Page 55 and 56: February 2004 2.1.4 Solar radiation
Page 57 and 58: February 2004 There is a clearly de
Page 59: February 2004 In the granites of th
Page 63 and 64: February 2004 Periglacial relief It
Page 65 and 66: February 2004 in a westward directi
Page 67 and 68: February 2004 Ribni Lakes and the t
Page 69 and 70: February 2004 2.3.5 River water qua
Page 71 and 72: February 2004 The above-cited findi
Page 73 and 74: February 2004 2.4.2 Soil erosion In
Page 75 and 76: February 2004 Ecosystems of the tre
Page 77 and 78: February 2004 The alpine treeless z
Page 79 and 80: February 2004 The following territo
Page 81 and 82: February 2004 Table 11: Distributio
Page 83 and 84: February 2004 Distribution of fores
Page 85 and 86: February 2004 Table 19: Distributio
Page 87 and 88: February 2004 photophilic character
Page 89 and 90: February 2004 брой видове
Page 91 and 92: February 2004 protoroburoides). The
Page 93 and 94: February 2004 number species 800 60
Page 95 and 96: February 2004 Group IV The fourth g
Page 97 and 98: February 2004 Of the highest conser
Page 99 and 100: February 2004 alpine zone. The larg
Page 101 and 102: February 2004 Neuroptera: Libelloid
Page 103 and 104: February 2004 that can be encounter
Page 105 and 106: February 2004 European, and 151 of
Page 107 and 108: February 2004 B. Species endangered
Page 109 and 110: February 2004 its annexes. Of these
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February 2004 to the Directive on H
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February 2004 4.0 Cultural and Soci
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February 2004 The residence of Arch
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February 2004 Infrastructure relate
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February 2004 Table 22: General inf
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February 2004 Dairy farming was ano
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February 2004 leaves for fodder. Th
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February 2004 According to data fro
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February 2004 awe and fascination w
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February 2004 % 100 Rila Monastery
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February 2004 Hiking and mountain c
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February 2004 Type/name of the faci
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February 2004 Type/name of the faci
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February 2004 4.1.8 Public awarenes
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February 2004 or emergency, since t
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February 2004 Monastery Forest Rese
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February 2004 The BAS Institute of
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February 2004 The average annual wa
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February 2004 Table 29: List of the
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February 2004 Dependence of the pop
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February 2004 includes the followin
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February 2004 Such proximity enable
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February 2004 (living quarters) are
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February 2004 The St. Luke Hermitag
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February 2004 On the whole, both va
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February 2004 round qualities, func
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February 2004 5.0 First assessment:
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February 2004 - breeding ground of
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February 2004 The proposed sustaina
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February 2004 Non-timber natural re
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February 2004 Tourism Tourism is on
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February 2004 Transportation expens
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February 2004 1.0 Ideal (long-term)
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February 2004 populations (reintrod
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February 2004 1.5 Interpretation an
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February 2004 roads, hydro technica
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February 2004 (a similar process ha
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February 2004 2.2 Anthropogenic thr
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February 2004 Similar in its destru
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February 2004 Increased tourist pre
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February 2004 Pollution with solid
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February 2004 overuse of non-timber
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February 2004 2.3 Limitations The l
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February 2004 The presence of a set
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February 2004 The impact of threats
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February 2004 4.2 Conservation of n
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February 2004 Long-term goal 4.2.5
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February 2004 • To implement a pr
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February 2004 - To develop and impl
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February 2004 1.0 General Regimes a
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February 2004 1.1.2. Pursuant to PA
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February 2004 2.0 Zones, Regimes an
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February 2004 Purpose of the Buffer
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February 2004 Description, physical
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February 2004 Purpose of the Enviro
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February 2004 2.4 The Technical Inf
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February 2004 2.5 The Sustainable F
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February 2004 Conditions 1. The Sus
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February 2004 2.7 The Tourism Zone
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February 2004 1. Construction of an
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February 2004 1. Building and diffe
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February 2004 - Tiha Rila - Lake Sm
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PART IV OPERATIONAL/WORK PLAN
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February 2004 facilities in the par
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February 2004 natural environment.
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February 2004 natural re-growth of
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February 2004 • Project: Restorat
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February 2004 supporting and ensuri
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February 2004 2.4 Management of tou
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February 2004 • Project: Setting
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February 2004 • Project: Involvem
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February 2004 • Project: Building
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February 2004 2.7.8 Program for pro
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February 2004 Contractor Duration C
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PART V MONITORING OF THE IMPLEMENTA
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February 2004 1.2.2 Revising the Ma
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February 2004 Bibliography A classi
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February 2004 Hilton-taylor, C. - c
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February 2004 Simeonovski, М. 1965
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APPENDICES
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February 2004 Environment Protectio
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February 2004 Order No. 114 Dated F
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February 2004 II. High mountain pas
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February 2004 The Reserve shall inc
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February 2004 Appendix 3 List of in
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February 2004 Appendix 3 Object typ
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February 2004 Appendix 3 List of ab
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February 2004 Rila Monastery Nature
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February 2004 133 - а, и, к, л,
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February 2004 а, б, в, г, д, 1
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February 2004 ZONE B The Zone B reg
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February 2004 Ministry of Environme
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February 2004 List of the Documents
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February 2004 No Institution Contac
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February 2004 Appendix 8 Geological
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February 2004 Appendix 10 No Code L
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February 2004 Appendix 10 43 37.872
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February 2004 Appendix 11 Station N
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February 2004 Appendix 11 Station N
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February 2004 Appendix 13 List of h
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February 2004 Appendix 13 No Taxon
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February 2004 No Taxa Species diver
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February 2004 No Taxons Established
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February 2004 No Taxons Established
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February 2004 Appendix 15 Endemic N
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February 2004 Appendix 15 Key: Ende
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February 2004 No Species 26. Thymus
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February 2004 List of edible mushro
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February 2004 Appendix 20 List of v
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February 2004 Appendix 20 Key: Ende
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February 2004 Common species Number
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February 2004 Crafts Fulling mill,
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February 2004 Auxiliary infrastruct
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February 2004 Handling of fecal was
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February 2004 Auxiliary infrastruct
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February 2004 Appendix 24 Natural P
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February 2004 405 Rila Monastery Na
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Form No February 2004 Appendix 27 S
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Form No February 2004 Appendix 27 3
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Form No Studied area February 2004
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Form No Studied area February 2004
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February 2004 416 The paths of thes
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February 2004 418 4. Ribni lakes ch
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February 2004 Appendix 31 Goal Perf
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February 2004 Appendix 31 Goals Ind
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February 2004 Appendix 31 Goals par
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February 2004 9. 36.3921 Oro-Moesia
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