Field Guide to Aquatic Phenomena
Color of the water
Stuff in the water
On the surface
 
Along the shoreline
 
Winter phenomena
 


Why is water different colors?

When we think of a lake or river, we picture clear, blue water. But water color can range from red to brown to green to gray. The color you see is the result of material in the water that reflects back different wavelengths of the light spectrum. This material can be either dissolved or suspended. Dissolved material may make water look clear and blue or clear and brown. Suspended particles in the water intercept light and reflect back color to our eyes, making water look muddy brown, cloudy green, or gray.

 
blue       green  

 

 
                             

Blue water

Clear, blue water does not contain a lot of the particles or dissolved, colored material that intercepts and reflects light. (Think of a clear blue sky versus a hazy, smoggy sky--the hazy air has more particles in it). As a result, the longer wavelengths of light toward the blue part of the light spectrum penetrate into the water, and the blue is reflected back to our eyes. The darker the blue, the deeper the water. Shallow areas appear lighter blue or greenish blue.

 

 
blue lake        
                               

Clear water

Why do some lakes and rivers have no color? Clear water has less dissolved and suspended material. Mountain streams that start as snowmelt or runoff are often clear, because they run over bare rock without sediment or vegetation. Seepage lakes in sand and gravel settings may also look clear, and shallow water is clear because there is not enough depth for the long, blue wavelengths of light to travel and be reflected back.

                 
  clear water in a stream  
                               

Crystal clear Roaring Brook drains the rocky slopes of Katahdin.

 

 

Clear brown or reddish water

Sometimes water is clear but brown like tea or root beer. The color is the result of dissolved organic material from the breakdown of plants and animals. The material leaches into slow moving streams and lakes from surrounding forests, bogs and wetlands, and stains the water brown or reddish brown.

 
reddish water     clear brown water  

This stream flows out of a cedar swamp (Appleton Bog) in midcoast Maine.

    Rocky Brook drains a small wetland in forested downeast Maine.  

Muddy or murky brown water

Suspended material causes water to look murky or cloudy (this is sometimes referred to as turbidity). Eroding soil can make water muddy brown in color. Strong winds and waves may stir up sediment from a lake bottom, and water near shore may look cloudy as a result. During spring snowmelt, rivers may appear brown as heavy rains and snowmelt send a pulse of sediment, grit, and dust into streams.

 
               

 

Gray or cloudy water

Runoff from urban areas can make water look gray, as in this stream that drains an area that has a lot of commercial and industrial development (parking lots, buildings, roads).

     
cloudy gray water        
                                 
                     
Green water                  
green water   Suspended particles of living material can impart a hue to the water. Green water probably has a large population of algae (microscopic plants).     a green lake    
                       
Photo courtesy Somerset Co. SWCD
Photo courtesy Somerset Co. SWCD  
   

Algae and other microscopic organisms have colored pigments. When they grow in large numbers ("bloom"), they can color certain areas or entire lakes and streams. Blooms of an organism called Euglena may appear red. A bloom of diatoms, a kind of algae, can look brown. (See the section on Algae for more about blooms.)

 
About
 
Index
   
Links
 
DEP logo

 

A project of the Senator George J. Mitchell Center for Environmental & Watershed Research and Maine Department of Environmental Protection.

 

UMaine logo

Member of the University of Maine System
All text and photos copyright of C. Schmitt unless otherwise indicated.