laugrandadel tagasivooluhoovustest tingitud rida regulaarselt (mõni m kuni 60 m) rannajoonega risti paiknevaid nooljaid maasääri, mis on omavahel rannajoone poolt kaarjalt ühinenud; on reeglina vähepüsivad, are shoreline formations of regularly spaced (few to 60 m distance) horns and embayments connected in arc pattern and made up of various grades of sediment; formed due to pachy character of the wave induced off-shore directed bottom (rip) currents