The flux of dissolved material from a given river then depends on the geographical distribution of lithologies relative to climate patterns, rates of tectonic activity (uplift), vegetational donations, and heterogene- ities in the intensity of physical weathering processes that produce reactive materials.
(The flux of dissolved material from a given river; depends; on the geographical distribution of lithologies relative to climate patterns, rates of tectonic activity (uplift), vegetational donations, and heterogene- ities in the intensity of physical weathering processes; T:then) (physical weathering processes; produce; reactive materials)
The flux of dissolved material from a given river physical weathering processes
depends produce
on the geographical distribution of lithologies relative to climate patterns, rates of tectonic activity (uplift), vegetational donations, and heterogene- ities in the intensity of physical weathering processes T:then
reactive materials