It is a deep waterway containing numerous islands, the largest of which are Laut Island and Sebuku.
The clash of civilizations can be seen along the Massacre River, a muddy, waist-deep waterway that divides them.
Heading south along the western shoreline of Staten Island, the deep waterway is lined with old industrial buildings and with active oil refineries and storage facilities.
The resultant deep waterway, navigable by oceangoing ships, extends about 2,300 miles from the Atlantic Ocean to the head of the Great Lakes in the heart of North America.
A continuous, navigable, deep waterway from the Atlantic to the Great Lakes was the obvious route for opening up the interior of North America; but natural obstacles, such as the Lachine Rapids north of Montreal, had prevented its realization.
The Deep Waterway Project (DWP) and reclamation projects were responsible for the polarization of seaward erosion and landward accretion, respectively.
Deep waterway project (DWP) dominates area increase of JDS by inducing accretion in north edge and south edge of Lower Shoal between 1998 and 2014.
To improve navigability of the major access channel into Shanghai Harbor, a large-scale Deep Waterway Project was carried out in the North Passage (NP) of the Yangtze Estuary.
As an example, this module is applied to the Changjiang Estuary where a dike groyne structure was constructed in the Deep Waterway channel in the inner shelf of the East China Sea (ECS).
The latter is accumulated by land subsidence from underground water depletion, water level fall caused by the erosion of riverbeds from a sediment supply decline attributed to the construction of watershed dams, artificial sand excavation, water level raise by engineering projects including land reclamation, deep waterway regulation, and fresh water reservoirs.
