Armed conflicts in the post-Soviet region: Present situation, prospects for settlement, consequences. OSW Study 9/2003

Unresolved conflicts continue to smoulder in Transnistria, Chechnya, Abkhazia, Nagorno-Karabakh and South Ossetia. "Para-states" have formed in most conflict-affected areas. These have grown to become permanent players in the region. In Chechnya, guerrilla fights continue in the wake of the Russian army's siege of the republic. The conflict in Tajikistan ended in 1997 and the normalisation process is currently under way. Each of these conflicts has entailed profound political, social, ethnic and economic changes, as well as affecting other spheres of life. Presently, it is impossible to return to the pre-conflict situation. The "para-states" have fortified their independence and are no longer controlled by the external powers on which they depended in the initial phases of the conflicts.

Abkhazia’s ‘creeping’ incorporation. The end of the experiment of a separatist democracy. OSW Commentary 164, 2015-03-12

On 5 March 2015 a Russian-Abkhazian treaty on alliance and strategic partnership came into effect; it had been signed on 24 November 2014. In fact, the treaty provides a “roadmap” for the incorporation of Abkhazia into the Russian area of defence and economic and social affairs: as soon as the transition periods defined in the treaty expire, Russian standards and legal regulations will be rolled out in these areas. Despite maintaining the formal status of the Abkhazian government institutions and attributes of statehood (which, however, is a fact of minor importance, as Abkhazia is not internationally recognised as a state), the treaty’s entry into force will de facto bring the current model of functioning of this para-state to an end.

The Bumpy Road to Democracy: Success and Failure in the Integration of Ethnic Armenians in the Republic of Georgia

Thesis (Master's)--University of Washington, 2016-06

Pollen profile AMTKEL, Amtkel, Georgia

The rock mass of fluvial and fluvioglacial deposits of the Late Holocene has been studied at the altitude of 1830 m a.s.l. using the palynologic, carpologic, geomorphologic, and geochronologic methods. It was ascertained that in the mid-Subatlantic period the area of the present-day beech elfin woodland was occupied by a belt of alpine meadows. Thus, the lower border of alpine meadows ran 370-400 m lower than the recent level, pointing to a rather significant cooling of the climate that occurred from ca 2nd cent. A.D.