View allAll Photos Tagged Splash_Pool
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.
June 2021: Closeup of the splash pool underneath the Grotto waterfall. // Prints: ericsmith.smugmug.com / Instagram: @eric.s.images
Kampong Thom Grasslands, Cambodia
On a birding trip that my wife and I took to Cambodia in early 2023
A coffee cup near the splash pool at the base of Horsetail Falls gets encased in ice just like everything else. Trying to retrieve would be a very dangerous proposition at this point.
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.
THE SPLASH - Pool Party Camping Le Camarguais
Le 02 Juillet 2023 de 12h à 00h
Lien Event :
www.facebook.com/events/104867795969550
Lien Page Facebook :
www.facebook.com/thexprojectevent
Lien Page Instagram :
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.
Clip 1 - Big Anemone Geyser’s 11:59 AM to 12 noon eruption on 3 June 2014.
Clip 2 - Big Anemone Geyser’s 11:30 to 11:31 AM eruption on 8 July 2014.
Clip 3- Big Anemone Geyser’s 11:36 AM eruption on 8 July 2014.
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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.
ASPAM Scottish School is one of the best Schools in Noida that ensures the better future of your kids. We have best-in-class infrastructure that includes smart classrooms, library, vast playground, splash pool, language lab and so on. We also encourage our students to engage in different fun activities.
The serpentine were 3 open-topped slides with no drops but lots of twists. This tower still exists but the name, theming and slide configuration has changed.
The bridge crosses over the connection between the slide splash pool and the surrounding lazy river.
Splash
Pool
Aloft San Francisco Airport
401 East Millbrae Avenue
Millbrae, California (CA), 94030
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
AloftSFO.GeneralInfo@AloftHotels.com
650-443-5500
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.
Emaar Gurgaon Green 3/4 bhk apratment oil bound distamber wall and verify tiles
Landscaped Area approximately 6 acres.
· Efficient Floor plans.
· All towers Facing Greens.
· Two apartments on each floor, with 2 elevators.
· Jogging Track and Club House with Modern Amenities, Health Club and Tennis Courts.
· Swimming Pool with Splash pool and dedicated Play areas for children.
· Efficient Power Back-up.
The Radisson Hotel At Toronto Harbourfront/ Rooftop Pool
Another adventure to my “life is what you make it summer”. Just because you don't own a cottage does not mean you can't life it up and have a taste of the marine life. With stunning views of Lake Ontario and downtown, the Radisson Admiral Hotel Toronto-Harbourfront offers a beautiful setting for work and leisure. This hard-to-beat location offers two transportation hubs, Union Station and Billy Bishop Toronto City Airport ), less than two kilometres from the hotel. The double decker bus can offer trips to key destinations and a view of the city. I soaked up the sun at the on-site SPLASH Pool Patio and Terrace overlooking Lake Ontario and the CN Tower, one of the modern Seven Wonders of the World. There are plenty of pool chairs for lounging between dips and catching a cool lake breeze. The one's in the sun are coveted so you will have to make like a sundial and move around. You can order food and drinks. Day passes cost $40 and each pass includes two towels and access to shower and locker facilities, but you will need to bring your own lock which I didn't. Things were safe on the deck. The police marine unit is below, so a safe place to be. The scene from the balcony is constantly changing with the crowd, watercraft and weather. The staff was professional and courteous. I went by myself but my trusty Nikon is my sidekick and old friend.
Brand new in sealed box. £3.75. (rrp £4.99). Quantity: 6
Have some fun in the sun with Emma’s Splash Pool!
Summertime is finally here in Heartlake City and everyone’s favorite place to be is Emma’s Splash Pool. Head over to Emma’s place to work on your tan in the lounge chair, cool off in the pool or have an ice cream in the fresh air! Invite all of the LEGO® Friends over for a pool party and some fun in the sun! Includes Emma mini-doll figure.
Includes Emma mini-doll figure
Features Splash Pool, lounge chair, umbrella, ice cream dish and small plant
Splash around in the pool!
Host a pool party for all of the LEGO® Friends!
Serve up cold ice cream to the girls!
LEGO Friends pieces are fully compatible with all LEGO bricks
Collect all of the LEGO Friends sets for a whole world of LEGO Friends fun!
LEGO mini-dolls are LEGO minifigures made especially for the world of LEGO Friends with thousands of customizable hair and fashion combinations
Measures over 2” (7cm) tall, 3” (9cm) wide and 2” (6cm) long
© Copyright Paul Marsden. All rights reserved www.f29.co.uk
Heard about this place whilst up in Moab. A beautiful waterfall hemmed into a canyon, it made for a welcome sight and some waterfall photography wasn’t what i had immediately had in mind from the desert Southwest.
I’d have liked to get a shot of the falls face on and filled the bottom of the frame solely with the veils of water, as I’m not mad keen with the rock at the edge of the bottom left of the frame. But, … alas I’m ankle deep in the river, and on the edge of the tier of the falls. An inch back, i’d have plummeted off the 30ft down into the splash-pool below :)
If the rains hadn’t been so heavy of late, i think i’d have been able to stand more to the left, but the current was stong and getting traction on the sandstone bed of the river wasn’t easy.
After the inaugural day, the Summer Camp took a full swing to ignite the fire of all the participants to let them learn what they desire for. Splash pool activity concluded the day with cheers.
For more details contact- mapsvasundhara.edu.in
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.
The "main event" at Mill Creek is this 30 foot waterfall. the hike down to it is rather intimidating if you are afraid of such things. After my hike up to the upper Catawba Falls it was a piece of cake. Notice the rope hanging on the left. Maybe at higher water levels the splash pool is more substantial, but from what I saw I could figure out why you would try swinging into it LOL
The rocks here was interesting too. I have several different angles of this coming...
BLOG I I I WSM photography I I I Eastern Waterfalls Database
© Scott Moore 2012 - All rights reserved
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.
Splash
Pool
Aloft Charlotte Uptown at the EpiCentre
210 East Trade Street
Charlotte, North Carolina (NC), 28202
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
(704) 333-1999
finally got around to getting my first holga roll to rob for scanning.
this is the scanned version of this previously posted pic.
Triple exposure of dappled light falling onto a kid's splashing pool.
The film was also advanced a few clicks for the third exposure which explains the non square format, this was the last shot in the roll so the right edge has been cut off.
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.
Wham-o Slip N Slide Wave Rider Double With 2 Slide Boogies
The original backyard slide, trust Wham-o quality
Easy set-up with 1 step connect-n-go with self filling bumper
Super fast slide with Hydro-Glide technology
Includes Splash Pool for hydroplaning
15′ slide area
64120 Features:...
www.appliances.adikit.com/wham-o-slip-n-slide-wave-rider-...
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.
25 14th Street, San Francisco, CA
www.waghotels.com/pet-care-boarding-hotels-san-francisco/...
"Nestled off the 101 freeway near the Mission and SOMA districts, our San Francisco hotel is a state-of-the-art facility that offers a variety of innovative services and amenities for dogs and cats. Guests can enjoy hotel-style boarding with private Wag Rooms and luxurious Ultra Suites for our canine guests and Kitty Condos for our feline guests.
With over 14,000 square feet of play space, our All Day Play program (supervised doggie daycare) offers your canine companion the opportunity to hang out, meet new friends, exercise and have fun — the Wag way. Your furry friend can also take advantage of other amenities like evening strolls on our 9,000 sq.ft rooftop deck or a dip in the splash pool."
Splash
Pool
Aloft San Antonio Airport
838 NW Loop 410
San Antonio, Texas (TX), 78216
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
info@aloftsanantonioairport.com
210-541-8881
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 Lexington
727 Marrett Road - A
Lexington, Massachusetts (MA), 02421
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
aloftlexington@alofthotels.com
(781) 761-1700