View allAll Photos Tagged Splash_Pool
The good thing is, you can now see the splash pool in the corner, opposite the Keepers house, very easily, as you could always hear it but not see it when you passed.
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.
Tardy Geyser is a frequently-erupting member of the Sawmill Group in Yellowstone’s Upper Geyers Basin. It is located 19 meters southeast of Sawmill Geyser. They geyser has a subcircular basin with a centrally-located, funnel-like vent surrounded by a nicely pustulose geyserite platform. Ringing the platform is a splash pool that contains discoidal geyser beads, many of which have become cemented together. Tardy Geyser has two runoff channels. The more frequently used channel runs roughly southwest toward the Firehole River. The other channel extends northeast from Tardy’s basin, then heads east, then heads roughly south toward the Firehole River. This geyser usually has short-duration eruptions that last a few seconds to several minutes - this happens when nearby Sawmill Geyser is active. During a “Tardy Cycle”, the geyser will erupt continuously for 1 to 3 hours with no Sawmill activity. At such times, Tardy Geyser is the dominant member of the Sawmill Group. The northeast-to-east-to-south runoff channel is used during Tardy Cycle activity.
Beautiful New 1 Bedroom + Den Unit! South Views On Balcony. Laminate Flooring With Stainless Steel Whirlpool Appliances, With Granite Countertop. Open Concept Dining/Living Room With Walkout To Balcony. Ensuite Washer/Dryer & 1 Parking Included. Occupancy Is Immediate. Amazing Amenities Including Pool + Baby Splash Pool, Whirlpool, Sauna, Games & Party Room. Movie & Kids Play Room. Modern Gym & Much More.
No Smoking Inside Unit, $200 Key Deposit Required, No Pets Allowed, Credit Check, References, Post Dated Chqs, Rental Application Required. 1 Or 2 Year Term Available. *Approval Subject To Interview*
Geysers are hot springs that episodically erupt columns of water. They occur in few places on Earth. The highest concentration of geysers anywhere is in Yellowstone’s Upper Geyser Basin (northwestern Wyoming, USA).
Big Anemone Geyser is a frequently erupting small geyser in the southern 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 of the feature, as measured from the outer edge of its 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 activity at adjacent Little Anemone Geyser has a delaying affect on Big Anemone’s eruption frequency. Eruption cessations at Big Anemone Geyser are impressive, 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.
At the end of the trail lies Wahclella Falls, a 350-foot two-tiered plunge. The upper falls are 15-25 feet, while the lower 60-foot "horsetail" style falls plummets into an enormous splash pool.
Photo taken by my wife, Claire, while hiking the trail on a rainy day.
Douglas Falls. The gorgeous red color of the rocks was due to tannins from vegetation such as red spruce, rhododendrons and mountain laurel that covered the hillsides.
Blackwater Canyon, Monongahela National Forest, West Virginia. (Nov 1, 2009)
Wet & Splash Pool Parties during Girls in Wonderland at the Sheraton Lake Buena Vista Resort in Orlando, FL.
Wet & Splash Pool Parties during Girls in Wonderland at the Sheraton Lake Buena Vista Resort in Orlando, FL.
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.
Tardy Geyser is a frequently-erupting member of the Sawmill Group in Yellowstone’s Upper Geyers Basin. It is located 19 meters southeast of Sawmill Geyser. They geyser has a subcircular basin with a centrally-located, funnel-like vent surrounded by a nicely pustulose geyserite platform. Ringing the platform is a splash pool that contains discoidal geyser beads, many of which have become cemented together. Tardy Geyser has two runoff channels. The more frequently used channel runs roughly southwest toward the Firehole River. The other channel extends northeast from Tardy’s basin, then heads east, then heads roughly south toward the Firehole River. This geyser usually has short-duration eruptions that last a few seconds to several minutes - this happens when nearby Sawmill Geyser is active. During a “Tardy Cycle”, the geyser will erupt continuously for 1 to 3 hours with no Sawmill activity. At such times, Tardy Geyser is the dominant member of the Sawmill Group. The northeast-to-east-to-south runoff channel is used during Tardy Cycle activity.
While in Monterey we visited the famous Monterey Bay Aquarium, which is well worth seeing.
This Star Fish was hanging on to the glass in the splash pool and I captured this shot just as the wave broke against the glass.
Wet & Splash Pool Parties during Girls in Wonderland at the Sheraton Lake Buena Vista Resort in Orlando, FL.
splash pool
Pool
Aloft Bangkok - Sukhumvit 11
35 Sukhumvit Soi11, Sukhumvit Road
Klongtoey-nua,Wattana
Bangkok, 10110
Thailand
www.starwoodhotels.com/alofthotels/property/overview/inde...
(66)(2) 207 7000
splash
Pool
Aloft Chapel Hill
1001 South Hamilton Road
Chapel Hill, North Carolina (NC), 27517
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
aloftchapelhill@aloftchapelhill.com
919-932-7772
Artist: Tom Grimsey
Title: The Flowering of the Lort Burn, 2005
Material: Terrazzo, ceramic, stainless steel, planting
The Florid Burn, the Hidden Rivers Project
Leazes Park
Newcastle upon Tyne, Tyne and Wear, England, UK
Text from the Newcastle City Council web page:
The work is a direct response to the Lort Burn that flows beneath Leazes Park and through the lake. The work consists of a stream made from blue terrazzo and planting. Stainless steel flowers are set into the paths where to mark where the burn flows. A playful splash-pool, situated at the top of the park suggests the source of the Lort Burn.
Geysers are hot springs that episodically erupt columns of water. They occur in few places on Earth. The highest concentration of geysers anywhere is in Yellowstone’s Upper Geyser Basin (northwestern Wyoming, USA).
Big Anemone Geyser is a frequently erupting small geyser in the southern 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 of the feature, as measured from the outer edge of its 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 activity at adjacent Little Anemone Geyser has a delaying affect on Big Anemone’s eruption frequency. Eruption cessations at Big Anemone Geyser are impressive, 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.
Friday the 29th April 2011 was spent around Mid Wales taking photos of waterfalls well when we got there virtually dried up waterfalls.
This shows some colourful rocks and also shows how dry these waterfalls were on a set of waterfalls in Cwm Dwfn a deep valley in the hills near to the small village of Staylittle.
Senior KG students of Apple Kids International Pre-school enjoying the hot chilling day in Splash Pool.
Champaign County Postcard collection, postcard 218, Champaign County Historical Archives, Urbana, Illinois.
All images are provided for personal and educational use. Users planning to reproduce/publish images in books, articles, exhibits, videos, electronic transmission or other media must request permission. For more information please contact the Champaign County Historical Archives at The Urbana Free Library: archives@urbanafree.org
Fantástico SPLASH POOL. Piscinas dinámicas y llenas de sorpresas
Fantastic splash pool. Dynamic pools full of surprises.
splash pool
Pool
Aloft Lexington
727 Marrett Road - A
Lexington, Massachusetts (MA), 02421
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
aloftlexington@alofthotels.com
(781) 761-1700
Wet & Splash Pool Parties during Girls in Wonderland at the Sheraton Lake Buena Vista Resort in Orlando, FL.
Geysers are hot springs that episodically erupt columns of water. They occur in few places on Earth. The highest concentration of geysers anywhere is in Yellowstone’s Upper Geyser Basin (northwestern Wyoming, USA).
Big Anemone Geyser is a frequently erupting small geyser in the southern 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 of the feature, as measured from the outer edge of its 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 activity at adjacent Little Anemone Geyser has a delaying affect on Big Anemone’s eruption frequency. Eruption cessations at Big Anemone Geyser are impressive, 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.
Wet & Splash Pool Parties during Girls in Wonderland at the Sheraton Lake Buena Vista Resort in Orlando, FL.
Artist: Tom Grimsey
Title: The Flowering of the Lort Burn, 2005
Material: Terrazzo, ceramic, stainless steel, planting
The Florid Burn, the Hidden Rivers Project
Leazes Park
Newcastle upon Tyne, Tyne and Wear, England, UK
Text from the Newcastle City Council web page:
The work is a direct response to the Lort Burn that flows beneath Leazes Park and through the lake. The work consists of a stream made from blue terrazzo and planting. Stainless steel flowers are set into the paths where to mark where the burn flows. A playful splash-pool, situated at the top of the park suggests the source of the Lort Burn.
Wet & Splash Pool Parties during Girls in Wonderland at the Sheraton Lake Buena Vista Resort in Orlando, FL.