Refer to the figure.
Figure 1
You are studying a river in its natural state, unaffected by human activities. Your data are graphed in Figure 1. You began collecting data at the source of the river ("0 km" on the figure) and continued to sample the river every 1 km.
-What type of succession would you expect to see in this high cation exchange capacity area, and why? How would the rate of soil formation and succession differ from what you would expect in a terrestrial area disturbed by a lava flow?
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