Defining exactly what constitutes a tree requires blending botanical precision with structural observation, a foundational concept for tree identification.
At its core, a tree is a long-lived, perennial plant that features secondary thickening—the development of a hard, woody skeleton composed of lignin and cellulose produced by the active cell division of the vascular cambium. Unlike herbaceous plants that die back in winter, or woody plants that produce multiple low-growing stems from ground level, a tree concentrates its early growth into a single, dominant, self-supporting main stem known as a trunk. This trunk serves the dual purpose of elevating the photosynthetic leaf canopy high above competing ground vegetation and acting as a massive vascular pipeline.
Some guidebooks try to define a difference between a shrub and a small tree, but in reality it is often difficult to distinguish them in practice. Factors such as environmental stress, high-altitude exposure, or historical management practices like coppicing can cause a single-stemmed tree species to develop a multi-stemmed, bushy growth form. It is much simpler and less prone to error to avoid the term shrub altogether and simply refer to trees and consider their size and form.
Understanding the basic anatomical layout of a tree provides the structural baseline required to explore finer identification keys, allowing observers to classify specimens not just by their immediate size, but by the permanent architectural framework they build within a woodland or landscape.
Note that all trees are dicotyledons (plants which have two seed leaves), compared to monocotyledons (single seed leaves, like grasses). This is why a palm tree is not technically a tree at all, because it is a monocotyledon!