JEB logo

Journal of Environmental Biology

pISSN: 0254-8704 ; eISSN: 2394-0379 ; CODEN: JEBIDP

About Journal
    Home
    Editor in Chief
    Editorial Board
    Reviewer Panel
    Publication Policies
    Guidelines for Editors
    Guidelines for Reviewers
    Abstracting and Indexing
    Subscription and Payments
    Contact Journal
 
Read Journal
    Current Issue
    Journal Archives
 
For Authors
    Guidelines for Authors
    Terms and Conditions
    Fees and Payments
    Track Paper Status
 
Announcements
    JEB Awards
 

Google Search the Journal web-site:


    Abstract - Issue Apr Supplement 2012, 33 (2)                                     Back


nstantaneous and historical temperature effects on a-pinene

The relief formed by the descent phenomenon in the north-east part of Kosova

 

Author Details

 

Shpejtim Bulliqi

(Corresponding author)

Faculty of Mathematical-Natural Science, University of Prishtina, Prishtina, 10 000 Kosovo

e-mail: shpejtim.bulliqi@ks.gov.net

Florim Isufi

Faculty of Mathematical-Natural Science, University of Prishtina, Prishtina, 10 000 Kosovo

Ibrahim Ramadani

Faculty of Mathematical-Natural Science, University of Prishtina, Prishtina, 10 000 Kosovo

Gani Gashi

Faculty of Mathematical-Natural Science, University of Prishtina, Prishtina, 10 000 Kosovo

 

Publication Data

Paper received:

30 October 2010

 

Revised received:

02 July 2011

 

Accepted:

20 July 2011

 

Abstract

In  the  diverse  relief of north-east part of Kosova  a  relatively  wide  range  occupies  the  relief  modelled? by the descent phenomenon, which  is conditioned by morph-structural and climatic factors quite suitable for their development. The morphogenesis activity of descent phenomenon is conditioned by the types of rocks, tectonic process of this region and climatic conditions. These factors condition horizontal and vertical relief fragmentation, slope, especially in Gollaku mountains and in SE part of Kopaonik mountain. Along the tectonic descents, the steepness is detaching and the detaching lines consisting of magmatic rocks show overthrows, demolitions and stony torrents, but the Teri gene composition formations are modelled by sliding and muddy torrents, depending upon the presence of clayey and alevrolite belts on these Teri gene ones. The impact of factors and conditions on the relief of this part, the phenomena like demolitions, overthrows, sliding, muddy torrents, stony torrents, etc, operate here, which play an important morphological role in the modelling of? relief.

?

Key words

Kosova, Descent phenomenon, Morphogenesis activity, Sliding, Stony torrents, Kopaonik ?

 

Copyright ? 2012 Triveni Enterprises. All rights reserved. No part of the Journal can be reproduced in any form without prior permission. Responsibility regarding the authenticity of the data, and the acceptability of the conclusions enforced or derived, rest completely with the author(s).