Ljubov Danilovna Kiprijanova’s scientific contributions

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Publications (1)


Fig. 1. The pillars of the Middle Lena.
Fig. 2. Location of the Lena Pillars. Legend: 1. river, 2. pillars, 3. road, 4. settlement.
Fig. 3. Distribution of the fracture directions of the bearing rock (a) measuring site: at the mouth of the Labiya Valley and at the Lena bank opposite the mouth, distribution of the direction of closes (giant grikes) (b) measuring site: at the mouth of the Labiya Valley.
Fig. 4. Distribution of the grain of the frost weathering debris and the distribution of bed thickness measuring site: at the mouth of the Labiya Valley and at the Lena bank opposite the mouth, Legend: 1. layer thickness, 2. debris thickness, 3. width of the debris.
Fig. 5. A plan view of the types of pillars. Legend: 1. step body, 2. margin of step body, 3. slope with debris, 4. cliff, 5. valley, creek, 6. crevice, 7. giant grike, 8. top of pillar, 9. small step, 10. step body, 11. scarp front (slope with pillar). (I) Half cylinder-like pillar type, (II) mass pillar type, (III) ridge pillar type, (IV) type of ridge with steps, and (V) type of the pinnacle pillar.

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The development of the pinnacles (Lena pillars) along Middle Lena (Sakha Republic, Siberia, Russia)
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September 2014

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296 Reads

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4 Citations

Proceedings of the Geologists Association

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Kálmán Péntek

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Ljubov Danilovna Kiprijanova

The study deals with the Lena Pillars (Sakha Republic, Russia, Siberia). The Lena Pillars are pinnacle features which are characteristic on karsts. The importance of these features is that they are extremely large and occur on very large areas. Their occurrence is interesting because they do not appear on tundra karst. We investigated the veneers of cliffs, the fracture density of the building rock, the distribution and dispersion of the fracture directions, direction distribution and dispersion of the giant grikes between the pillars, the layer thickness of the building rock, the size and dispersion of debris. We distinguished pillar types, and then we classified the features on the area of the pillars from a morphogenetical point of view. According to investigations and morphological analyses, the pillars developed from palaeokarsts. During the former karstification grikes and caverns developed close to the surface. These features coalesced into each other. The giant grikes of great size became filled and the pillars were covered. After the cut of the Lena River these features were revealed and became exhumed. Now the pillars are destroyed and continue developing by frost weathering.

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