Step 1: Understanding the Concept:
The ruggedness number is a dimensionless geomorphic index combining watershed elevation steepness with dissection intensity.
Key Formula or Approach:
\[ R_n = H_b \times D_d \]
where \(H_b\) is total basin relief (m), and \(D_d\) is drainage density (\(\text{km/km}^2\) or \(\text{m}^{-1}\)).
Step 2: Detailed Explanation:
Strahler (1957) defined the Ruggedness Number (\(R_n\)) of a watershed as the product of maximum basin relief (\(H_b\), elevation difference between highest ridge point and basin outlet) and drainage density (\(D_d\), total stream length per unit basin area):
\[ R_n = H_b \times D_d \]
High ruggedness numbers occur in mountainous, deeply dissected regions subject to severe flash flooding and soil erosion.
Step 3: Final Answer:
Therefore, ruggedness number is given as Basin relief \(\times\) Drainage density, matching option (A).