the Earth 's surface(passive) caused bythe Earth 's surface

in narrow winding cobbled streets that run along , and rise away from the waterfronthas resultedin narrow winding cobbled streets that run along , and rise away from the waterfront

in " sink holesresultingin " sink holes

to changes in cell - substratum adhesionledto changes in cell - substratum adhesion

in the complex structures of the underground rivers and cavesalso resultsin the complex structures of the underground rivers and caves

from the erosion of this limestoneresultingfrom the erosion of this limestone

from the dissolution of carbonate rocks by groundwaterresultsfrom the dissolution of carbonate rocks by groundwater

from the erosion of limestone ( which dissolves in water washresultingfrom the erosion of limestone ( which dissolves in water wash

The area(passive) is composedThe area

in sinkholescan resultin sinkholes

areas(passive) influenced byareas

several springsoriginatesseveral springs

to a large number of sinkholeshas contributedto a large number of sinkholes

Site development in Southwest Missouri(passive) is heavily influenced bySite development in Southwest Missouri

it to shiftcausedit to shift

variations in the pull of gravity(passive) caused byvariations in the pull of gravity

susceptibility of Salmonella Enteritidis biofilmsinfluencessusceptibility of Salmonella Enteritidis biofilms

current flowsinfluencescurrent flows

to local variationsleadsto local variations

nutrient - rich waterscausesnutrient - rich waters

as geologists call itleadsas geologists call it

both isolation and climatic variationcausesboth isolation and climatic variation

susceptibility of Salmonella enteritidis biofilms to trisodium phosphateinfluencessusceptibility of Salmonella enteritidis biofilms to trisodium phosphate

secular variations in subglacial discharge(passive) are influenced bysecular variations in subglacial discharge

complex streamflow and rainfall patterns ... governing the atmospheric transport of pollutants and the intensity and spatial variability of depositioncausescomplex streamflow and rainfall patterns ... governing the atmospheric transport of pollutants and the intensity and spatial variability of deposition

society , not only in terms of slow processes of landscape change and earthquakes , but also in terms of how it affects climateinfluencessociety , not only in terms of slow processes of landscape change and earthquakes , but also in terms of how it affects climate

The circulation patterns driven by wind and density differences(passive) are strongly influenced byThe circulation patterns driven by wind and density differences

wind patterns in an areainfluenceswind patterns in an area

precipitation and temperature in soil formationinfluencesprecipitation and temperature in soil formation

precipitation and temperature in soil formationinfluencesprecipitation and temperature in soil formation

an area s climateinfluencesan area s climate

The local climate(passive) is noticeably influenced byThe local climate

the distribution of plants and animals , weather patterns , rainfall patterns and the movement of surface watercan influencethe distribution of plants and animals , weather patterns , rainfall patterns and the movement of surface water

key natural processes , such as the distribution of plant communities and the associated animals that depend upon them , weather and rainfall patterns , and the flow and storage of surface waterinfluenceskey natural processes , such as the distribution of plant communities and the associated animals that depend upon them , weather and rainfall patterns , and the flow and storage of surface water

The climate of the region(passive) is influenced byThe climate of the region

in the heart of the Aravallis with its steep rock faces and steep cliffssetin the heart of the Aravallis with its steep rock faces and steep cliffs

a high spatial variability of microclimatic conditions and slope dynamicscausesa high spatial variability of microclimatic conditions and slope dynamics

Soil formation process(passive) is greatly influenced bySoil formation process

surface erosion and depositional processes(passive) are influenced bysurface erosion and depositional processes

The vegetation distribution trend(passive) is strongly influenced byThe vegetation distribution trend