What type of ocean current is characterized as being slower and typically found along the continents?

Eastern Boundary Currents are characterized as being slower and typically found along the continents. These currents are located on the eastern side of ocean basins and flow in a direction that is usually opposite to the prevailing winds. They are generally broad and shallow, associated with regions of upwelling and nutrient enrichment, which supports marine ecosystems.

In contrast to Eastern Boundary Currents, Western Boundary Currents, which are fast-moving and concentrated near the western sides of ocean basins, often contribute to the formation of warm ocean features like the Gulf Stream. Surface currents, on the other hand, are generally faster and influenced by wind patterns, while Transverse Currents typically connect the eastern and western boundaries of ocean basins but do not specifically refer to the slower currents found near coasts.

The distinction of Eastern Boundary Currents reflects their unique role in coastal oceanography and their impact on local climates and marine habitats.