Interlocking spurs are formed as either a river or stream cuts its valley into local bedrock.
2.
While similar in general appearance, the mechanism behind the formation of interlocking spurs is different from that behind meanders, which arise out of a combination of lateral erosion and deposition.
3.
It meets the Inachos east of the city, from whence the Inachos flows into the Argolic Gulf at Nea Kios, but an interlocking spur continues east and winds around the village of Merbaka.
4.
From here it flows southwards, for about through the Lower Himalayas and the Shivalik Hills Range and morainic deposited are found in its steep Upper Yamuna village, highlighted with geomorphic features such as interlocking spurs, steep rock benches, gorges and stream terraces.
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