Currents, tides, and waves are horizontal water movements.
surface currents are horizontal, steamlike movements of water that are found at or near the surface of the ocean
A seismometer is the instrument used to measure horizontal movements along faults. It records the seismic waves generated by these movements.
A flexion preformed across the horizontal plane.
Tidal currents are not quite the same thing as tides. Tidal currents are horizontal movements of water caused by the tides.
GPS and interferometric synthetic aperture radar monitor both vertical and horizontal movements along the fault.
Horizontal movements of water caused by wind and occurring at or near the ocean's surface are called surface currents. They play a significant role in redistributing heat around the Earth and influencing global climate patterns.
Horizontal sideways movements.
A seismometer, which is a device that measures ground movements, can detect both vertical and horizontal movements along a fault. These instruments are crucial for monitoring seismic activity and predicting potential earthquakes.
Dextral fault movements involve horizontal displacement where the right side of the fault moves horizontally relative to the left side. Sinistral fault movements involve horizontal displacement where the left side of the fault moves horizontally relative to the right side. These movements are determined based on the direction of horizontal displacement across the fault plane.
Forward and backwards, right and left can be horizontal movements. The ocean waves moves horizontally. Up and down are vertical movements. A rocket that's been recently fired moves vertically. So the answer to your question is no.
The movements of water are often referred to as water currents or water circulation. These movements can include processes such as evaporation, condensation, precipitation, melting, freezing, and flow in rivers and oceans.
wind-induced turbulence, which can drive the mixing of water within the mixed layer. This turbulence occurs as wind energy is transferred into the water column, causing vertical and horizontal movements that mix different water masses together.