Capillary action alone cannot lift water to a height of 10 meters; instead, it is the negative pressure created at the top of trees that facilitates this elevation. Water reaches the tops of 100-meter tall trees due to a combination of capillary action in tiny leaf pores and tension in the thicker xylem tubes. The tiny pores (2-5 nm) allow sufficient capillary action to counterbalance the weight of the water column below. The xylem tubes, which are much wider (20000-200000 nm), cannot solely achieve this height through capillary action. Understanding this phenomenon involves recognizing the role of negative pressure and the metastable state of water at great heights.