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The map extract shows the River Cree in south-west Scotland. By following the route of the river, it is possible to describe the main physical features. When describing river features we mean natural features not man-made ones.

In this OS map extract:

• At 400670 the River Cree joins the map. It is flowing in a south-easterly direction. We know this because the river gets wider as it nears the estuary/mouth of the river.
• At 410664 a tributary joins the river at a confluence. The river now flows south around an island. The valley is relatively narrow (you can see contour lines close to the river on both sides).
• At 416647 the river becomes tidal. We know this because the edge of the river changes from blue to black.
• At 417642 there is a meander. The river valley now broadens out to more than two kilometres wide, covering two grid squares.
• At 422641 the river begins a series of large meanders. There is an embankment on the south bank of the river - this could be a natural ����é��.
• The neck of the meander at 425637 could eventually be broken through by the river to form an oxbow lake.
• At 429640 the river starts to widen and mud/silt is showing in its bed.
• Many tributaries now join the river – 434623 (the Brushy Burn) 441627 (The Lane) 453624 (Palnure Burn).
• The river is now flowing in a very flat, wide and low-lying valley (7m and 5m spot heights). This has resulted in marsh land at 452612, 456606 and 465590.
• The river enters its estuary at 467580.