Sketches of springs spheres of discharge: a cave, b exposure, c fountain, d geyser, e gushet, f hanging garden, g helocrene, h hillslope, i hypocrene, j limnocrene, k mound form, l rheocrene. A aquifer, I impermeable stratum, S spring source. The inverted triangle represents the water table or piezometric surface. Fault lines are also shown, where appropriate
( 2008 ) expanded these historical schemes to include 12 spheres of
discharge of springs, including: (1) springs that emerge in caves,
(2) exposure springs, (3) artesian fountains, (4) geysers, (5)
gushets, (6) contact hanging gardens, (7) helocrene wet meadows,
(8) hillslope springs, (9) hypocrene buried springs, (10)
limnocrene surficial lentic pools, (11) mound forms, and (12)
rheocrene lotic channel floors (Figs. 1 and 2 ; Table 1
Cave springs are those that emerge entirely within a cave
environment and are not directly connected to surface flow
(Figs. 1 a and 2 a).
( 2008 ; Figs. 1 b and 2 b).
Fountain springs are cool-water artesian springs that are forced
above the land surface by stratigraphic head-driven pressure or CO
2 (e.g., Crystal Geyser; Glennon and Pfaff 2005 ;
Figs. 1 c and 2 c).
Geysers are globally rare, geothermal springs that emerge
explosively and usually erratically (Figs. 1 d and 2 d).
( 2008 ; Figs. 1 e and 2 e).
Hanging gardens are complex, multi-habitat springs that emerge
along geologic contacts and seep, drip, or pour onto underlying
walls (Figs. 1 f and 2 f).
Helocrene springs usually emerge in a diffuse fashion in cienega
(marshy, wet meadow) settings (Figs. 1 g and 2 g).
Hillslope springs emerge from confined or unconfined aquifers on
non-vertical hillslopes at 30–60° slopes, and usually have
indistinct or multiple sources (Figs. 1 h and 2 h).
Hypocrene springs are springs in which groundwater levels come
near, but do not reach the surface (Figs. 1 i and 2 i).
Limnocrene springs occur where discharge from confined or
unconfined aquifers emerge as one or more lentic pools (Figs.
1 j and 2 j).
Mound-form springs emerge from (usually carbonate) precipitate
mounds or peat mounds (Figs. 1 k and 2 k).
The term rheocrene was first coined by Bornhauser ( 1913 ) to
describe springs where discharge emerges as flowing streams
(Figs. 1 l and 2 l).
Viewing this image requires a subscription. If you are a subscriber, please log in.
This image is from the article titled "Spheres of discharge of springs"
(from Hydrogeology Journal), which is copyrighted by Springer-Verlag. For more information on the
copyright for this image, please refer to the full image caption and to the
The image is being made available for non-commercial purposes for subscribers to SpringerImages. For more information on what you are allowed to do with this image, please see our copyright policy.
To request permissions to use any copyrighted material, please visit the source document.
Report a copyright concern regarding this image.
Log in or register to save your favorite images and download them as high-quality PowerPoint or PDF files.
Log in or register to save your search criteria.
© Springer, part of Springer Science+Business Media.
Remote Address: 18.104.22.168 Server: 19