Uploaded January 2026 | Updated September 2026, 2 weeks ago
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Jagged Spring (16 August 2025)
Geysers are hot springs that episodically erupt columns of water. They occur in few places on Earth. The highest concentration of geysers anywhere is at the Yellowstone Hotspot Volcano in northwestern Wyoming, USA.
Jagged Spring is located next to a modern tourist boardwalk in the Black Sand Basin of Yellowstone’s Upper Geyser Basin. The feature is 5 to 6 meters east of Ragged Spring. Jagged’s basin is about 3 to 3.5 by 1.5 to 2 meters in size and irregularly elongated in shape. The pool’s margin is scalloped and undercut - overhangs are present on the western and southern edges. The pool is deepest on the western side and shallows to the east. Multiple vents are present - some vents are beneath overhangs and have eroded blowholes in the overlying geyserite platform. Jagged Spring is never completely calm. It frequently cycles from low water levels with small, mild splashing to high water levels with fiercely enegetic splashing, which can result in relatively brief eruptions a couple meters high (even up to ~5 meters). Jagged Spring’s subterranean plumbing system is connected with nearby Ragged Spring - these two geysers have concerted energetic eruptions.
Black Sand Basin videos:
youtube.com/playlist?list=PL8dL6UmmXTBVwmCwqDQXjddb1pn82Whbf
All clips - Jagged Spring’s energetic eruptions in the afternoon of 16 August 2025.
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Jagged Spring (16 August 2025)
Geysers are hot springs that episodically erupt columns of water. They occur in few places on Earth. The highest concentration of geysers anywhere is at the Yellowstone Hotspot Volcano in northwestern Wyoming, USA.
Jagged Spring is located next to a modern tourist boardwalk in the Black Sand Basin of Yellowstone’s Upper Geyser Basin. The feature is 5 to 6 meters east of Ragged Spring. Jagged’s basin is about 3 to 3.5 by 1.5 to 2 meters in size and irregularly elongated in shape. The pool’s margin is scalloped and undercut - overhangs are present on the western and southern edges. The pool is deepest on the western side and shallows to the east. Multiple vents are present - some vents are beneath overhangs and have eroded blowholes in the overlying geyserite platform. Jagged Spring is never completely calm. It frequently cycles from low water levels with small, mild splashing to high water levels with fiercely enegetic splashing, which can result in relatively brief eruptions a couple meters high (even up to ~5 meters). Jagged Spring’s subterranean plumbing system is connected with nearby Ragged Spring - these two geysers have concerted energetic eruptions.
Black Sand Basin videos:
youtube.com/playlist?list=PL8dL6UmmXTBVwmCwqDQXjddb1pn82Whbf
All clips - Jagged Spring’s energetic eruptions in the afternoon of 16 August 2025.
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![Big Anemone Geyser (2024)
Big Anemone Geyser (2024)
Geysers are hot springs that episodically erupt columns of water. They occur in few places on Earth. The highest concentration of geysers anywhere is at the Yellowstone Hotspot Volcano in northwestern Wyoming, USA.
Big Anemone Geyser is a frequently erupting small geyser in the southern Geyser Hill Group of Yellowstones Geyser Hill Group. It is immediately adjacent to Little Anemone Geyser - together they make up “Anemone Geyser”. Big Anemone has a nearly circular basin with a central vent and lacks a well-defined border. Encircling the cream-colored to grayish, smooth geyserite-floored vent area is abundant, well-formed, closely spaced nodules of grayish geyserite (columnar geyserite & pseudocolumnar geyserite), similar in appearance to cave popcorn (coralloids). Some small biscuit-like masses of grayish geyserite are present on the northern side of the geyser, often with apical puckered structures. The geyserite biscuits are in and along a small, irregularly-shaped, eruption splash pool. The diameter of Big Anemone Geyser, as measured across its nodulose geyserite area, is about 2.5 meters. The diameter, as measured from the outer edge of the colorful, encircling microbial mats, is about 4.5 to 5 meters.
Big Anemone’s geyserite is especially well-formed and attractive. Geyserite is a friable to solid chemical sedimentary rock composed of opal (hydrous silica, a.k.a. opaline silica: SiO2•nH2O), It forms by precipitation of hydrous silica from hot spring water. Geyserite is the dominant material at & around Yellowstone hot springs and geysers (the Mammoth Hot Springs area is a major exception to this). The silica in the geyserite is ultimately derived from leaching of subsurface, late Cenozoic-aged rhyolitic rocks by superheated groundwater. Rhyolite is an abundant rock at Yellowstone.
Big Anemone Geyser has frequent, moderately low to medium-sized, splashing eruptions. Eruption durations are about half a minute long. Intervals between eruptions starts range from about 7 minutes to almost half-an-hour. Eruption cessations at Big Anemone Geyser consist of rapid pool drains. Most of the erupted water ends up back in its own vent. Some eruption splash water enters Little Anemone’s basin or its runoff channel.
Geyser Hill Group videos:
https://www.youtube.com/playlist?list=PL8dL6UmmXTBUMW6oQAafxBFkkAvXyDrE3
Clip 1 - Big Anemone Geyser’s 4:32 PM eruption on 11 June 2024.
Clip 2 - Big Anemone Geyser’s 4:41 to 4:42 PM eruption on 11 June 2024. [time stamp 0:47]
Clip 3 - Big Anemone Geyser’s 4:52 PM eruption on 11 June 2024. [time stamp 1:32] Big Anemone Geyser (2024)](https://i.ytimg.com/vi/QtY6k2dMhhU/mqdefault.jpg)





