පහත දැක්වෙන්නේ වර්ගය අනුව දිය ඇලි ලැයිස්තුවක් වෙයි.
සමහර දිය ඇලි අඛණ්ඩව ගලා යෑමක් සිදු නොවේ. Ephemeral දිය ඇලි ගලා යන්නේ වර්ශාවකට පසුව හෝ සැලකිය යුතු මට්ටමේ හිම දියවීමකට පසුව වෙයි.
Water descends vertically, losing contact with the bedrock surface.
Descending water maintains some contact with bedrock.
A large, powerful waterfall.
A series of waterfalls one after another of roughly the same size each with its own sunken plunge pool.
Water descends from a relatively wide stream or river.
Water descends a series of rock steps.
Distinctly separate flows of water form as it descends.
Water drops in a series of distinct steps or falls.
Water descends in a constricted form and then spreads out in a wider pool.
Water spreads horizontally as it descends while remaining in contact with bedrock.
Ephemeral waterfalls flow only after periods of heavy rain or significant snowmelt.
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