Abstract
Springs as groundwater outflows onto the surface belong to permanent elements in Knyszyn Forest Landscape Park which occurrence results from geological structure of Bialystok High Plain. Research included 5 springs located in 3 reserves (Krzemianka, Jalowka, Budzisk) in Knyszyn Forest Landscape Park. During research there have been described classification of springs with water analyses of physico-chemical properties as well as flora verification in spring niches. The surveys has shown that in studied area the springs belong to ascending or descending outflows with erosion scarp and rheocrenes at one time. Due to lack of anthropogenic changes as well as location of springs in forest area they possess good water quality here what was proved by water analyses.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
