Management of Subterranean Ecosystems in Extreme Environments
Monte Neva Hot Springs

Map coordinates:  39.0303, -116.666
Water temperature:   140.9°F
Site ID:   nv_dpb

Diana's Punch Bowl & Pott's Ranch

Diana's Punch Bowl & Pott's Ranch. Image courtesy of the Nevada Commission on Tourism.

Dianas Punch Bowl (Dianna's, Devils) (Sec. 22, T14N, R47E) is a cup-shaped depression about 15 m in diameter at the top of a domelike hill of travertine about 183 m in diameter. Warm water in the pool of the bowl is about 9 m below the rim, while the top of the hill is about 23 m above the level of Monitor Valley.

A small warm spring, about 43-49°C in temperature, issues from the southwest corner of the travertine dome (Fiero, 1968). Temperatures up to 59°C have been reported, and the estimated minimum reservoir temperature by several chemical geothermometers is 88-97.7°C (Mariner and others, 1974; Hose and Taylor, 1974).

Very slightly anomalous radioactivity (16 μR/hr) is reported by Wollenberg (1974b). The thermal area lies on a north-trending, concealed fault in the central part of Monitor Valley (Stewart and Carlson, 1974; Fiero, 1968). Spurr (1905, p. 257) describes a report by J.L. Butler that the water level had lowered and water became cooler in the years prior to 1905. Also, he reported that more gas was formerly emitted and occasional flames were seen.

Dianas_Punch_Bowl.pdf Get Topo Map On the Web New Hotspring Search

Diana's Punch Bowl & Pott's Ranch


Geochemistry


  1. Sample date:1966-12-09
  2. Sodium (Na):55
  3. Potassium (K):16
  4. Lab-test pH:7.3
  5. Calcium (Ca):52
  6. Total dissolved solids:399
  7. Magnesium (Mg):11
  8. Iron (Fe):n/a
  9. Strontium (Sr):n/a
  10. Lithium (Li):0.09
  11. Boron (B):0.32
  12. Silica (SiO2):43
  13. Bicarbonate (HCO3):300
  14. Sulfate (SO4):62
  15. Chloride (Cl):10
  16. Fluoride (F):n/a

Resources


Image by Dr. Jean K. Krejca, Zara Environmental LLC

Cave ecosystems are often dependent on organic material carried in by water, which serves as the primary food source for the environment. In arid climates with minimal surface rainfall, the input of organic matter and nutrients into caves becomes limited, affecting the overall energy flow within these environments. The intricate interplay between surface conditions and cave biota presents unique management challenges for modern cave biologists. Image courtesy of Dr. Jean K. Krejca, Zara Environmental LLC.

Ancient Bristlecone Pines

Bristlecone Pine

Many of Great Basin National Park's bristlecone pines were growing at the time the Egyptians were building the pyramids. Not only are the trees themselves old, but the needles alone can be 25-40 yrs old!

Symposium Merchandise

h2go Essen Vacuum Food Container

It's a double-wall, stainless steel, 17 oz capacity thermos from h2go®. This thing is more rugged than your cave pack! We've been trying to beat up the manufacturer's sample, but it keeps winning. Hot things stayed hot, cold things stayed cold... and ours will have cool cave art printed on it.

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JUNE 29, 2023
NCKMS Steering Committee Chooses Ely, Nevada as Host City for 2025 Symposium
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