1. Stream Drainage

2. THE INFLUENCE OF BEDROCK IN AN AREA WILL CAUSE STREAMS TO DRAIN IN SEVERAL DIFFERENT PATTERNS.

3. A UNIQUE PATTERN CAN BE SEEN FROM OVER-HEAD
THESE PATTERNS ARE CALLED:
DRAINAGE PATTERNS
They are created because water always flows from higher elevations to lower elevations. Water tends to collect in lower areas creating rivers. The water that feeds into the rivers are known as the tributaries.

5. THE ROCK RESISTANCE IS SIMILAR
THIS OCCURS WHEN
THE ROCK RESISTANCE IS SIMILAR

6. WATER FLOWS DOWN HILL
FOLLOWING THE PATH OF
LEAST RESISTANCE

7. THE ROCK RESISTANCE IS DIFFERENT WATER FLOWS IN THE PATH OF
THIS OCCURS WHEN
THE ROCK RESISTANCE IS DIFFERENT
WATER FLOWS IN THE PATH OF
LEAST RESISTANCE

8. FOLLOWING THE PATH OF
LEAST RESISTANCE