Step 1: Recall the pore structure of loose materials.
Unconsolidated sand and gravel formations have large, well connected pore spaces since the grains are not cemented together.
Step 2: Link this structure to permeability.
Large connected pores let groundwater pass through with little resistance, giving these formations high permeability.
Step 3: Bring in transmissivity.
Transmissivity is essentially permeability multiplied by aquifer thickness, so a highly permeable unconsolidated formation naturally shows high transmissivity rather than low yield, low porosity, or zero storage.
\[ \boxed{\text{High transmissivity}} \]