View allAll Photos Tagged Splash_Pool
splash pool
Pool
Aloft Washington National Harbor
156 Waterfront Street
National Harbor, Maryland (MD), 20745
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
(301) 749-9000
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.
Photos of Pompeii
San Marco, Italy hamlet, Busch Gardens Williamsburg, Williamsburg, VA
Each boat that passes through Escape from Pompeii is photographed just as the boat makes its' descent down the hill outside and into the splash pool. Said photo can be purchased here at this stand outside of the ride's exit.
splash pool
Pool
Aloft Chesapeake
1454 Crossways Boulevard
Chesapeake, Virginia (VA), 23320
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
(757) 410-9562
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 (for example, see: www.youtube.com/watch?v=BzE2z1ew-KE) - 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.
The Sawmill Group significantly changed in early 2017. Sawmill Geyser, the dominant member of the group, was last seen erupting at the end of January 2017, and has been dormant ever since. Sawmill Geyser's dormancy has been accompanied by changes in other Sawmill Group features, including Tardy Geyser. Some features are inactive or near-inactive, others have become more active, or are engaging in atypical behavior.
Shown above is Tardy Geyser in near-dormancy in summer 2017. The splash pools and runoff channels are water-filled but relatively cool. Colorful microbial mats cover most surfaces. Water drains from Tardy in both runoff channels. Reported and observed eruptions since early 2017 have been brief, with diminutive, splashing water columns.
Senior KG students of Apple Kids International Pre-school enjoying the hot chilling day in Splash Pool.
splash pool
Pool
Aloft Charleston Airport & Convention Center
4875 Tanger Outlet Boulevard
North Charleston, South Carolina (SC), 29418
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
(843) 566-7300
The spot this man is standing at would normally be about half way into the splash pool. Due to the cold snap the base of the fall piled up like a big snow drift. However the water was still running underneath it. I thought it was a little crazy walking this close out on the pile.
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.
Splash Pool
Pool
Aloft Portland Airport at Cascade Station
9920 NE Cascades Parkway
Portland, Oregon (OR), 97220
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
(503) 200-5678
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.
Horrible shooting conditions (shafts of sunlight on the waterfall), meant that I didn't even bother shooting Adams Falls. Instead, I concentrated on the splash pool, which was a little bit more manageable.
Adams Falls splash pool. Ricketts Glen, Pennsylvania. (Mar 26, 2011)
Splash Pool
Pool
Aloft Winchester
1055 Millwood Pike
Winchester, Virginia (VA), 22602
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
540-678-1368
During a stop-over by Princess Cruises vessel, "Star Princess" on our cruise to Alaska from Vancouver via the “Inside Passage”, we have returned aboard the ship after our shore visit at our first port of call, Ketchikan, AK.
We are on the Sports Deck (Level 16) near the stern of the ship. At left is the Oasis Bar, with the Splash Pool in the foreground and a hot tub behind it. The inclined covered bridge above, goes up to the highest point of the ship, the Skywalkers Nightclub, which sits high above the stern at the Sky Deck (Level
Looking down-canyon from the splash pool. Unknown hiker contemplating the falls. Photo and caption courtesy of Bill Ashworth ’65
Your Private Splash Pool, the Poolside Bar & Grill, Movie Theatre, Fitness Center & Sauna, Games Arcade, Sundry Shop, Tennis & Basketball Courts, Sand Volleyball & Playground assure that you and your guests will enjoy every moment of the stay.
Booking Now: tinyurl.com/y78j8nx8
Senior KG students of Apple Kids International Pre-school enjoying the hot chilling day in Splash Pool.
LEGOLAND Windsor a theme park dedicated to children aged 3-12 years old and of course big kid adults.
An inspirational land where the kids are the hero and adults relive their childhood.
The fun never stops and imagination knows no bounds, a family attraction like no other.
Set in 150 acres of beautiful parkland, LEGOLAND Windsor is a unique family theme park with over 55 interactive rides, live shows, building workshops, driving schools and attractions.
It's amazing what can be built with LEGO bricks - nearly 55 million of them!
From comical camels to fearsome fire-breathing dragons, world landmarks to musical pirates, young and old alike will be fascinated by the incredible LEGO models throughout the park.
Fun Facts about LEGOLAND Windsor
There are 34 LEGO pieces in an average Miniland figure.
The largest model in Miniland is the Canary Wharf Tower which is 5.2 metres tall and took 3 model makers 850 hours to complete using 200,000 LEGO Bricks!
The smallest models are the pigeons in Trafalgar Square which contain 5 LEGO bricks each
New in 2011 - Atlantis Submarine Voyage
Take a deep breath and submerge yourself in an underwater adventure.
Plunge into the depths with this world-first LEGO® submarine ride and immerse yourself in a magical underwater adventure.
So what’s New in 2012
STAR WARS MINILAND EXPERIENCE - The Force has arrived at LEGOLAND
Take a trip to a galaxy far, far away at the UK’s only indoor LEGO® Star Wars™ Miniland Experience at the LEGOLAND® Windsor Resort. Enjoy seven of the most famous scenes from the six live-action Star Wars movies, as well as a scene from the animated series Star Wars: The Clone Wars™ all made out of 1.5 million LEGO® bricks built in 1:20 scale. Follow the chronological path through the Star Wars timeline and retrace the major events of the beloved Saga featuring 2,000 LEGO® models, authentic sounds and lighting effects in the ultimate LEGO® Star Wars experience.
LEGOLAND WINDSOR RESORT HOTEL - Now open
An exciting LEGO adventure awaits you, as the amazing 150 room, fully themed LEGOLAND Hotel opens at LEGOLAND Windsor RESORT!
Staying overnight at the new LEGOLAND Windsor Resort Hotel is a must for all LEGO fans. From the spectacular dragon-guarded entrance and interactive LEGO features through to the brightly coloured pirate splash pool and fully themed bedrooms, the new hotel will inspire imaginations and create laugh-out loud memories. With dedicated indoor play areas, entertainment and a buffet-style restaurant serving child-friendly meals, it’s the perfect family treat.
Splash
Pool
Aloft Baltimore Washington International Airport
1741 West Nursery Road
Linthicum, Florida (FL), 21090
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
410-691-6969
Get ready for our Great design minion water slide with pool! Yes, for sure, it is new design with splash pool in the front.Minion Despicable Me themed inflatables is always popular and is great for all ages. Features safety netting over climbing area and at the top.Our inflatable minion Despicable Me series slide looks like the real thing and its a ton of fun!
More Info:http://www.qiqi-toys.com/Slide/Minion-Inflatable-Slide-With-Pool-1223.html
The Legacy Park trail system, in Lee’s Summit, Mo., is part of a 700-acre multi-use area. It features more than 10 miles of trails through a pastoral environment, along a lakeshore and in and out of forest groves. While the majority of these trail miles are paved, the 1014 Loop is a single-track mountain bike trail of hard-packed dirt. The 1014 loop includes a spectacular waterfall, splash pool and limestone outcroppings. Wildlife is also abundant. The 22-acre Legacy Lake is surrounded by a trail loop and features canoes and stand-up paddleboards. Learn more about Legacy Park and trails in Lee’s Summit: bit.ly/2NOvvje
Senior KG students of Apple Kids International Pre-school enjoying the hot chilling day in Splash Pool.
Senior KG students of Apple Kids International Pre-school enjoying the hot chilling day in Splash Pool.
Attending the re-opening of the 'Norman S. Johnson Aquatic Center' at the Arcadia Community Regional County Park is Los Angeles County Parks & Recreation Director Russ Guiney, County Supervisor Michael Antonovich, Public Works Director Gail Farber, LA County Arts Commission Laura Zucker and Parks & Recreation Chief Deputy John Wicker (L-R) kick off the ceremony pool side on Wednesday Aug 1st 2012. At a cost of almost $10 million, this facelift includes a 6150 sq ft competition pool and a 6300 sq ft recreation/swimming pool with an integrated "splash-pool' and bath house building.
Photo By : Scott Harms
The coolest girl in town on a sweltering hot day in Budapest.
Seen near Matthias Church and Fisherman's Bastion.
Children and families gather at Rollingcrest-Chillum Splash Pool to take the Pool Safely Pledge and learn how to swim.
splash
Pool
Aloft Nanhai Foshan
Boai Road, Shishan Town, Nanhai
Foshan, 528225
China
www.starwoodhotels.com/alofthotels/property/overview/inde...
86-757-8878-8888
This tower featured 2 fast moving, enclosed slides on either side of a large group slide in the middle.
This slide's splash pool was connected to the lazy river. The river also had a few little side pools for relaxing. One of those is seen in the foreground here.
"Root Rock"
While exploring the east side of Kauai and it's waterfalls we came across this section that looked like the tree root just kept continuing as rock. Pretty unique and gave me an Indiana Jones feel. The bit of blue/green at the bottom is the splash pool from the waterfall (will post later).
Thanks!
aF
Thursday, May 22nd
Grabbed coffee with Rachel this morning then headed to my field trip at the Atlantic City wastewater treatment plant, which is powered by 5 1.5-MW turbines. It was very interesting, very smelly, and a good bit of fun, too. Although we were there to see the turbines, the main chunk of the tour was the wastewater treatment aspects -- like scenes straight from "Dirty Jobs" -- activated sludge being aerated in a rapidly splashing pool of brown. There were also solar panels on site. I didn't learn a ton, but overall it was a good trip, and Shawn and I got to wear hard hats :) Went to Iron Hill to celebrate Bobby and Steph's engagement when we got back before chilling with Apt 3 chicas for a bit.
The temperature scale is in degrees Fahrenheit.
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.