SLOW CHANGES:
Changes that take place in hours,days,years etc are slow changes EXAMPLE:
1)GERMINATION OF SEEDS
2)GROWTH OF A CHILD
3)CURDLING OF MILK
4)RIPENING OF FRUITS etc.
FAST CHANGES:
Changes that take place in a minute,second etc are called fast changes.EXAMPLE:
1)BURNING OF PAPER
2)BURSTING OF CRACKERS
3)OPENING OF DRAWERS
4)DROPPING AN OBJECT FROM THE TOP OF A BUILDING etc.
Slow changes to Earth's surface, like erosion and weathering, occur gradually over time due to processes like wind and water erosion. Fast changes, like volcanic eruptions and earthquakes, can reshape the landscape in a short period by releasing energy stored within the Earth's crust. Both slow and fast changes play significant roles in shaping Earth's surface over time.
slow
Fast weathering processes include physical weathering from frost action and chemical weathering from acid rain, leading to the quick breakdown of rocks. Slow weathering processes involve gradual decomposition of rocks over time due to factors like temperature changes and slight chemical reactions, resulting in erosion and soil formation.
Creep and solifluction are examples of slow mass movement processes. Creep is the slow, continuous movement of soil and rock downhill, while solifluction is the slow movement of thawed soil over frozen ground in areas with permafrost.
Changes on Earth can occur at different speeds depending on the specific processes involved. Some changes, like the movement of tectonic plates, can be relatively slow, taking millions of years to significantly impact the planet's surface. On the other hand, natural events like volcanic eruptions or earthquakes can lead to rapid changes in a short period of time.
Floods, volcanic eruptions, and landslides are all examples of rapid changes at the surface.
In a business presentation the points of interest change through the presentation. How fast the screen presentation changes depends on whether you use fast fade between slides or slow fade
Both. floods will erode soil and rock and also deposit soil and rock there by changing the surface of the earth ... this is generally slow. eruptions, earth quakes are fast and will also change the surface of the earth by substantially removing, changing the location or depositing magma . these are generally fast changes tectonic plate movements are generally slow in a gloobal perspective and this incorperates the volcano and earthquake model. it all depends on the scale of what you call slow and if you are looking at a micro environment or a macro environment - local or global.
not a fast but slow
One advantage of slow change is that it allows for better adaptation and planning, while a advantage of fast change is its ability to quickly address urgent issues or capitalize on opportunities. Both types of change can be valuable depending on the situation.
Slow changes to Earth's surface, like erosion and weathering, occur gradually over time due to processes like wind and water erosion. Fast changes, like volcanic eruptions and earthquakes, can reshape the landscape in a short period by releasing energy stored within the Earth's crust. Both slow and fast changes play significant roles in shaping Earth's surface over time.
Slow changes are gradual alterations or developments that occur over an extended period of time. These changes typically unfold at a gradual pace and may not be immediately noticeable. Examples include climate change, aging, or shifts in societal norms.
slow-fast-slow (Apex)
acceleration is a measurement of increased speed change (deceleration being that of decreased speed change). your current speed (Whether fast, or slow) is irrelevant, as long as it changes, and increases, which means you are accelerating.
fast and slow
slow
kinkajous are not very fast animals or very slow animals actually they are very slow and fast animals