2010
DOI: 10.1111/j.1745-5871.2010.00642.x
|View full text |Cite
|
Sign up to set email alerts
|

Experiencing Waterholes in an Arid Environment, with Particular Reference to the Lake Eyre Basin, Australia: a Review

Abstract: The distribution and permanence of waterholes have dictated human activity and settlement patterns in the arid zone for millennia. At a fundamental level, waterholes are vital to survival in a harsh climate. The recreational value and use of waterholes are widely recognised; however, the less tangible aspects of 'waterhole experience' have received scant attention. This review, written whilst compiling an inventory of permanent waterbodies across the Lake Eyre Basin of Queensland and South Australia, aimed to … Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
5
0

Year Published

2017
2017
2022
2022

Publication Types

Select...
3
1
1

Relationship

0
5

Authors

Journals

citations
Cited by 6 publications
(5 citation statements)
references
References 15 publications
0
5
0
Order By: Relevance
“…The last process predominates in rainfall-limited climates. In contrast to the more widely studied surface oases that are also mostly groundwater-derived [Fitzsimmons et al, 2005;Silcock, 2010], TFLs are less detectable subterranean oases that are at least partially shielded from evaporative losses, and that coexist with saline groundwater. Figure 1 identifies large bodies (>10 9 m 3 ) of known terrestrial saline (>1000 mg/L) groundwater at depths of <500 m, as identified by the UNESCO International Groundwater Resources Assessment Centre [Van Weert et al, 2009].…”
Section: Introductionmentioning
confidence: 67%
“…The last process predominates in rainfall-limited climates. In contrast to the more widely studied surface oases that are also mostly groundwater-derived [Fitzsimmons et al, 2005;Silcock, 2010], TFLs are less detectable subterranean oases that are at least partially shielded from evaporative losses, and that coexist with saline groundwater. Figure 1 identifies large bodies (>10 9 m 3 ) of known terrestrial saline (>1000 mg/L) groundwater at depths of <500 m, as identified by the UNESCO International Groundwater Resources Assessment Centre [Van Weert et al, 2009].…”
Section: Introductionmentioning
confidence: 67%
“…These waterholes and channels are an important part of Aboriginal culture, having formed the center of trade and culture for millennia (Constable et al, 2015). The last 100 years have been dominated by extensive pastoralism and tourism enterprises centered on the regions' unique natural and wilderness values, in which water points still hold significant cultural value (Silcock, 2010). The capacity for these ecosystems to continue to provide these services is contingent on the maintenance of ecosystem health.…”
Section: Methodsmentioning
confidence: 99%
“…Ubiquitous waterholes along the main rivers ( Fig. 1.6), some permanent, are the most reliable (and iconic) natural aquatic habitats in this system, despite varying considerably in their ephemerality (Silcock 2010). They are usually 4-6 m deep, although some can be up to 25 m deep (McMahon et al 2008;.…”
Section: Booms and Busts And 'In Between' Flows Drive This 'Water Envmentioning
confidence: 99%
“…People have a strong connection to waterholes (Silcock 2010), which is manifested in increasing tourist visitation leading to pollution around waterholes and damage to vegetation through the felling of logs for camp fires and trampling of sensitive riparian groundcover plants. Livestock grazing may also contribute to some loss of plant cover, as well as increased sedimentation of waterholes, although there remains relatively little evidence of widespread change in over more than a century (Silcock et al 2013).…”
Section: Development and Other Threats To The Riversmentioning
confidence: 99%
See 1 more Smart Citation