She makes small parathas in her toy plate...and a moment of greatest happiness can be felt around her...the moment she could get one..done:)special moment of wonderful kids....are not to be missed..Mar 2010

This model features very slight modifications to set 31048 (Lakeside Lodge) to turn an already old-style log cabin into a more Wild Western style building. I simply removed the chair from the dock and cooking fire from out front of the dwelling.

 

The good thing about having two of this set is I get to use the one from a while ago that I had torn apart to make changes to the later finished one. (Such as taking most of the "glass" windows out and replacing them with opening frames and shutters. This works beautifully except in the one spot where the space was too small to make it work.)

 

The inside features a rifle on the wall, a bottle of moonshine, a cup, wood stove, table with letter and pen, and a simple bed.

 

BONUS: I now have two moose for the layout! (mooses? moosi? what the plural of "moose" anyway!?)

Captured @ Villa Heil, Belgium.

The newest location to D.N.R !

donotresuscitate.co.uk/

TAIL FEATURES : BLBR VS CACG

very similar with differing emphasis

 

BLBR

Rump :Black is more pointed (wedge angle more acute)

White mid stripe :have a thicker white band

Tail : band of black shows less on tail

  

CACG

Rump :Black is more blunt (wedge angle more obtuse)

White mid stripe :have a thinner white band

Tail : band of black shows more on tail

 

STUDY SHOT

DSCN4291 heavily cropped

This photo features a woman with long black hair, wearing a red shirt, standing next to a motorcycle. She appears to be posing for the camera, possibly for a portrait. The motorcycle is positioned to the left of the woman, taking up a significant portion of the scene.

In the background, there are a few other people visible, but they are not the main focus of the image. The woman's outfit and the presence of the motorcycle create a sense of style and adventure in the scene.

The Huntress Fountain features a bronze figure of Diana the goddess of hunting shooting an arrow. The fountain was installed in 1906 and made by Countess Feodora Gleichen the first woman member of the Royal Society of British Sculptors. The Rose Garden Hyde Park London established by Henry VIII in 1536

Features a spring-loaded mace, turning Gatling gun.

This head representing a man of regular features has been discovered on 1901, August. It must have come from a statue about 2 m tall.

The forehead of the portrayed man is low; his hair is arranged in a raw of short locks regularly arched from a “pincers” motif at the inner corner of the right eye. This detail is present on the portraits of Augustus, and was adopted, with some variations, by his successors.

Some small locks turned in the direction of the center of the face are reminiscent of representations of Gaius Caesar (20 BCE - 4 CE), the adopted son of Augustus and his intended heir, and other private portraits from the same period.

This hairstyle and the classical features of the portrait suggest its assignment to the years 25 BC – 35 AD during the reigns of Augustus and Tiberius. It resembles their portraits, but the face is not theirs.

One may suppose that the subject was a member of the local aristocracy whose loyalty to the values of the “Principatus” was equally proclaimed by deliberate imitation of the appearance and coiffure of the men of the imperial family.

 

Source: Museum information note

 

Roman bronze portrait

About 25 BC – 35 AD

From Torino

Torino, “Museo di antichità”

 

This photo features a woman with black hair, wearing a brown shirt, standing on a beach. She is posing for the camera, with her hair blowing in the wind. The woman is also wearing a necklace and a watch on her wrist.

In the background, there are several other people scattered around the beach, enjoying the outdoor environment. A handbag can be seen placed on the ground near the woman, possibly belonging to her.

BERLIN, GERMANY - NOVEMBER 30: Team Crazy Raccoon's Teppei "ade" Kuno poses at the VALORANT Champions Features Day on November 30, 2021 in Berlin, Germany. (Photo by Lance Skundrich/Riot Games)

Features of the TerraMax 5 include the SuperLift grapple/crane articulating arm, the MegaBlade terrain manipulator, a large dumping/storage bucket, an onboard crushing and proment/cement plant and distributer, a spacious internal hangar, a capable communication, weather, and rader surveillance array, and living quarters for 15. The TerraMax 5 can establish your presence on a new world, and provide a mobile command and construction center until facilities are completed.

Features:

Railgun

Opening roof hatch

Retractable communications mast

360-degree rotating turret

90-degree lifting railgun

Dimensions:

7x3x2.5 studs

 

Built for the 2012 LMABC.

The Fllying Dragon features these interchangeable attachments inspired by Lego Grandad ( www.youtube.com/watch?v=hNON7evryBE ). They are driven by a "Dog Gear" on a front-facing EV3 Medium Motor. The green items are optional braces to help secure an attachment onto the robot. The attachments can do the common FLL tasks, such as "hooking" and "grabbing". The black attachment is a variation on the "grab-and-lift" Lego FAR Gripper Arm Tool by Orlando_2k ( www.flickr.com/photos/42988571@N08/19387617039/in/album-7... ); it is driven by yellow Knob Wheels instead of Dog Gears. See the three adjacent renders in this Flickr Photostream to see various views of the robot. The Lego Digital Designer (LDD) .lxf Building Instructions file for the attachments are on Bricksafe: bricksafe.com/files/dluders/Fllying%20Dragon%20EV3%20Robo... .

2024 Longines Spirit Zulu Time 39mm

Scottish Hebrides.

This photo features a woman standing behind a counter in a food stand, possibly a coffee shop or a food truck. She is wearing a yellow apron and appears to be preparing food or coffee for customers. The counter is filled with various items, including multiple cups, bottles, and a bowl.

There are several cups placed on the counter, with some closer to the woman and others further away. Additionally, there are multiple bottles scattered around the counter, likely containing beverages or condiments. The woman seems to be focused on her task, ready to serve customers as they approach the food stand.

Various water features at the Orange County Arboretum

Keria (L) and Gumayusi of T1 at League of Legends Worlds 2025 Semifinal Features on October 27, 2025 in Shanghai, China. (Photo by David Lee/Riot Games)

The customer has got a lot riding on this recovery job, which is why they went with Western.

 

1:64 DCP by First Gear:

Peterbilt 389

Century 1150 Rotator Wrecker

Western Distributing Transportation Company

Towing & Recovery

First Gear #60-1175

 

#1stPixTowTruck

 

Olympus OM-D E-M1 Mark III

Olympus M.14-42mm F3.5-5.6 II R

 

For more info about the dioramas, check out the FAQ:

(Updated June 2023) 1stPix FAQ

Original Caption: A Greased Pig Contest Was One of the Features of the Tennessee Consolidated Coal Company First Annual Picnic Held at a Tennessee Valley Authority Lake near Jasper and Chattanooga Tennessee. Youngsters Are Shown Surrounding the Box Containing the Pig. Miners and Their Families Gathered to Talk, Eat Barbecue Participate in Sports and Listen to the Company President Discuss Health and Retirement Benefits 08/1974

 

U.S. National Archives’ Local Identifier: 412-DA-14081

 

Photographer: Corn, Jack, 1929-

 

Subjects:

Tennessee (United States) state

Environmental Protection Agency

Project DOCUMERICA

 

Persistent URL: catalog.archives.gov/id/556533

 

Repository: Still Picture Records Section, Special Media Archives Services Division (NWCS-S), National Archives at College Park, 8601 Adelphi Road, College Park, MD, 20740-6001.

 

For information about ordering reproductions of photographs held by the Still Picture Unit, visit: www.archives.gov/research/order/still-pictures.html

 

Reproductions may be ordered via an independent vendor. NARA maintains a list of vendors at www.archives.gov/research/order/vendors-photos-maps-dc.html

   

Access Restrictions: Unrestricted

Use Restrictions: Unrestricted

 

SAO PAULO, BRAZIL - FEBRUARY 18: Yuma "Dep" Hashimoto of ZETA DIVISION poses during the VALORANT Champions Tour 2023: LOCK//IN features day on February 18, 2023 in Sao Paulo, Brazil. (Photo by Lance Skundrich/Riot Games)

ATLANTA, GEORGIA - OCTOBER 26: Jeong "Chovy" Ji-hoon of Gen.G poses at the League of Legends World Championship Semifinals Features Day on October 26, 2022 in Atlanta, GA. (Photo by Fernando Decillis/Riot Games)

ATLANTA, GEORGIA - OCTOBER 26: Hwang "Kingen" Seong-hoon of DRX poses at the League of Legends World Championship Semifinals Features Day on October 26, 2022 in Atlanta, GA. (Photo by Fernando Decillis/Riot Games)

TOKYO, JAPAN - JUNE 09: Kim "MaKo" Myeong-kwan of DRX at VALORANT Masters Tokyo Features Day on June 9, 2023 in Tokyo, Japan. (Photo by Lee Aiksoon/Riot Games)

A monitor lizard on Pulau Perhentian Besar.

Apart from the many features of this dial, including accurate representations of the phases of the Moon, position of the Sun above the horizon, equinoxes, various time measurements, including Babylonian and Sidereal time, the four figures either side perform on each hour. The skeleton dates back to the completion of the clock in 1410 and rings a death toll each hour while the Turk to his right turns and the representation of Avarice on the other side of the dial shakes his bag of money and Vanity at the far left looks in his mirror.

 

Peter

SAO PAULO, BRAZIL - FEBRUARY 18: Shota "SugarZ3ro" Watanabe of ZETA DIVISION poses during the VALORANT Champions Tour 2023: LOCK//IN features day on February 18, 2023 in Sao Paulo, Brazil. (Photo by Lance Skundrich/Riot Games)

iphone SE Features After the launch of iPhone SE, now the Apple is looking for its next flagship smartphone in 2016. We all know how much people have craziness towards the apple devices. The Recent launched 6s series is already booming in the market. So now the wait for the next device Apple iPhone 7 has been already started, people always expects something more and high-end from upcoming iphones series Smartphones, 2016 is the destination where expectancy will get over this time. The device will be first available in (USA) America, China, Australia, UK, New Zealand, japan, France, Germany, Puerto Rico, Singapore, Hong Kong and other countries. This time we are really gonna see the best iPhone ever created in the history, as from now this device become the best upcoming smartphone that the people are eager to know about, so without wasting our time we should start talking about its specifications. And we are sure it will be the winner of best phone 2016 crown, let’s talk about the rumoured specifications below. iphone SE Features

ATLANTA, GEORGIA - OCTOBER 26: Kim "Zeka" Geon-woo of DRX poses at the League of Legends World Championship Semifinals Features Day on October 26, 2022 in Atlanta, GA. (Photo by Fernando Decillis/Riot Games)

© All rights reserved

 

Japanese maple - Acer palmatum dissectum 'Garnet'

Dwarf rhododendron - Yakushimanum rhododendron

 

Fun Rain Challlenge (Fuji HS50 EXR Users Group).

 

Although it was a grey wet day the saturated colours of the maples and rhododendron almost shone out in the garden.

Today's new airbrushed style pinup photo features Kelsey in this Western themed pinup! Kelsey is on the lamb evading the local sheriff after robbing the town bank. Be on the lookout for her, she's not hard to miss but when it comes to turning her in you might face yourself with a tough decision!

 

Did you know you can order many of the pinups you see posted on here? Check out the Dietz Dolls online store where you can find military pinups, classic pinups, the propaganda pinup poster series, and lots more in sizes ranging from 8x10 prints to 24x36 posters! www.dietzdolls.com/catalog

 

Model: Kelsey

Photographer: Britt Dietz

Online Pinup Print and Poster Store: www.dietzdolls.com/catalog

© Dietz Dolls Vintage Pinup Photography: www.dietzdolls.com

Facebook Fan Page: www.facebook.com/DietzPinupPhotography

 

TOKYO, JAPAN - JUNE 09: Timofey "Chronicle" Khromov of Fnatic at VALORANT Masters Tokyo Features Day on June 9, 2023 in Tokyo, Japan. (Photo by Lee Aiksoon/Riot Games)

We have the latest banner and one-sheets from the magical 3D stop-motion fantasy from Laika Studios and Focus Features. THE BOXTROLLS comes from the animation studio are known for their similar-styled animation efforts CORALINE and PARANORMAN, using a cinematic art form that many see as dying out...

 

bit.ly/1wa1572

astle is an utterly enchanting and captivating property. The tower (1430s) and the farmhouse (early 1800s) are linked by doors allowing guests to wander freely between two periods of history.

 

A mixture of simplicity and rustic charm, Clomantagh also features a Sheela-na-gig - a symbolic pagan nude carved on one of the stones.

 

Clonmantagh Castle is of outstanding importance because of the collection of buildings spanning the period from the 12th - 18th Century, the complex at Clomantagh includes a 12th Century parish church, an early 15th Century tower house, an almost intact boundary or bawn wall with a medieval dovecote, and a 19th Century farmhouse.

 

High on the tower house, above the roof of the farmhouse, there is evidence on an external wall, of an earlier attached structure. This is most likely the banqueting hall, which we know from contemporary descriptive accounts of Irish life was used for entertaining, the lord and his family only returning to the safety of the stone castle to sleep.

 

On the site of this banqueting hall stands the Victorian farmhouse, which is a fine example of this building type retaining most of its original features, apart from the roofing material which was changed from thatch to slate c.1850.

The geothermal areas of Yellowstone include several geyser basins in Yellowstone National Park as well as other geothermal features such as hot springs, mud pots, and fumaroles. The number of thermal features in Yellowstone is estimated at 10,000. A study that was completed in 2011 found that a total of 1,283 geysers have erupted in Yellowstone, 465 of which are active during an average year. These are distributed among nine geyser basins, with a few geysers found in smaller thermal areas throughout the Park. The number of geysers in each geyser basin are as follows: Upper Geyser Basin (410), Midway Geyser Basin (59), Lower Geyser Basin (283), Norris Geyser Basin (193), West Thumb Geyser Basin (84), Gibbon Geyser Basin (24), Lone Star Geyser Basin (21), Shoshone Geyser Basin (107), Heart Lake Geyser Basin (69), other areas (33). Although famous large geysers like Old Faithful are part of the total, most of Yellowstone's geysers are small, erupting to only a foot or two. The hydrothermal system that supplies the geysers with hot water sits within an ancient active caldera. Many of the thermal features in Yellowstone build up sinter, geyserite, or travertine deposits around and within them.

 

The various geyser basins are located where rainwater and snowmelt can percolate into the ground, get indirectly superheated by the underlying Yellowstone hotspot, and then erupt at the surface as geysers, hot springs, and fumaroles. Thus flat-bottomed valleys between ancient lava flows and glacial moraines are where most of the large geothermal areas are located. Smaller geothermal areas can be found where fault lines reach the surface, in places along the circular fracture zone around the caldera, and at the base of slopes that collect excess groundwater. Due to the Yellowstone Plateau's high elevation the average boiling temperature at Yellowstone's geyser basins is 199 °F (93 °C). When properly confined and close to the surface it can periodically release some of the built-up pressure in eruptions of hot water and steam that can reach up to 390 feet (120 m) into the air (see Steamboat Geyser, the world's tallest geyser). Water erupting from Yellowstone's geysers is superheated above that boiling point to an average of 204 °F (95.5 °C) as it leaves the vent. The water cools significantly while airborne and is no longer scalding hot by the time it strikes the ground, nearby boardwalks, or even spectators. Because of the high temperatures of the water in the features it is important that spectators remain on the boardwalks and designated trails. Several deaths have occurred in the park as a result of falls into hot springs.

 

Prehistoric Native American artifacts have been found at Mammoth Hot Springs and other geothermal areas in Yellowstone. Some accounts state that the early people used hot water from the geothermal features for bathing and cooking. In the 19th century Father Pierre-Jean De Smet reported that natives he interviewed thought that geyser eruptions were "the result of combat between the infernal spirits". The Lewis and Clark Expedition traveled north of the Yellowstone area in 1806. Local natives that they came upon seldom dared to enter what we now know is the caldera because of frequent loud noises that sounded like thunder and the belief that the spirits that possessed the area did not like human intrusion into their realm. The first white man known to travel into the caldera and see the geothermal features was John Colter, who had left the Lewis and Clark Expedition. He described what he saw as "hot spring brimstone". Beaver trapper Joseph Meek recounted in 1830 that the steam rising from the various geyser basins reminded him of smoke coming from industrial smokestacks on a cold winter morning in Pittsburgh, Pennsylvania. In the 1850s famed trapper Jim Bridger called it "the place where Hell bubbled up".

 

The heat that drives geothermal activity in the Yellowstone area comes from brine (salty water) that is 1.5–3 miles (7,900–15,800 ft; 2,400–4,800 m) below the surface. This is actually below the solid volcanic rock and sediment that extends to a depth of 3,000 to 6,000 feet (900 to 1,800 m) and is inside the hot but mostly solid part of the pluton that contains Yellowstone's magma chamber. At that depth the brine is superheated to temperatures that exceed 400 °F (204 °C) but is able to remain a liquid because it is under great pressure (like a huge pressure cooker).

 

Convection of the churning brine and conduction from surrounding rock transfers heat to an overlaying layer of fresh groundwater. Movement of the two liquids is facilitated by the highly fractured and porous nature of the rocks under the Yellowstone Plateau. Some silica is dissolved from the fractured rhyolite into the hot water as it travels through the fractured rock. Part of this hard mineral is later redeposited on the walls of the cracks and fissures to make a nearly pressure-tight system. Silica precipitates at the surface to form either geyserite or sinter, creating the massive geyser cones, the scalloped edges of hot springs, and the seemingly barren landscape of geyser basins.

 

There are at least five types of geothermal features found at Yellowstone:

 

Fumaroles: Fumaroles, or steam vents, are the hottest hydrothermal features in the park. They have so little water that it all flashes into steam before reaching the surface. At places like Roaring Mountain, the result is loud hissing of steam and gases.

Geysers: Geysers such as Old Faithful are a type of geothermal feature that periodically erupt scalding hot water. Increased pressure exerted by the enormous weight of the overlying rock and water prevents deeper water from boiling. As the hot water rises it is under less pressure and steam bubbles form. They, in turn, expand on their ascent until the bubbles are too big and numerous to pass freely through constrictions. At a critical point the confined bubbles actually lift the water above, causing the geyser to splash or overflow. This decreases the pressure of the system and violent boiling results. Large quantities of water flash into tremendous amounts of steam that force a jet of water out of the vent: an eruption begins. Water (and heat) is expelled faster than the geyser's recharge rate, gradually decreasing the system's pressure and eventually ending the eruption.

Hot springs: Hot springs such as Grand Prismatic Spring are the most common hydrothermal features in the park. Their plumbing has no constrictions. Superheated water cools as it reaches the surface, sinks, and is replaced by hotter water from below. This circulation, called convection, prevents water from reaching the temperature needed to set off an eruption. Many hot springs give rise to streams of heated water.

Mudpots: Mudpots such as Fountain Paint Pots are acidic hot springs with a limited water supply. Some microorganisms use hydrogen sulfide (rotten egg smell), which rises from deep within the earth, as an energy source. They convert the gas into sulfuric acid, which breaks down rock into clay.

Travertine terraces: Travertine terraces, found at Mammoth Hot Springs, are formed from limestone (a rock type made of calcium carbonate). Thermal waters rise through the limestone, carrying high amounts of dissolved carbonate. Carbon dioxide is released at the surface and calcium carbonate deposited as travertine, the chalky white rock of the terraces. These features constantly and quickly change due to the rapid rate of deposition.

Geyser basins

 

The Norris Geyser Basin 44°43′43″N 110°42′16″W is the hottest geyser basin in the park and is located near the northwest edge of Yellowstone Caldera near Norris Junction and on the intersection of three major faults. The Norris-Mammoth Corridor is a fault that runs from Norris north through Mammoth to the Gardiner, Montana, area. The Hebgen Lake fault runs from northwest of West Yellowstone, Montana, to Norris. This fault experienced an earthquake in 1959 that measured 7.4 on the Richter scale (sources vary on exact magnitude between 7.1 and 7.8; see 1959 Hebgen Lake earthquake). Norris Geyser Basin is so hot and dynamic because these two faults intersect with the ring fracture zone that resulted from the creation of the Yellowstone Caldera of 640,000 years ago.

 

The Basin consists of three main areas: Porcelain Basin, Back Basin, and One Hundred Springs Plain. Unlike most of other geyser basins in the park, the waters from Norris are acidic rather than alkaline (for example, Echinus Geyser has a pH of ~3.5). The difference in pH allows for a different class of bacterial thermophiles to live at Norris, creating different color patterns in and around the Norris Basin waters.

 

The Ragged Hills that lie between Back Basin and One Hundred Springs Plain are thermally altered glacial kames. As glaciers receded the underlying thermal features began to express themselves once again, melting remnants of the ice and causing masses of debris to be dumped. These debris piles were then altered by steam and hot water flowing through them. Madison lies within the eroded stream channels cut through lava flows formed after the caldera eruption. The Gibbon Falls lies on the caldera boundary as does Virginia Cascades.

 

Algae on left bacteria on right at the intersection of flows from the Constant & Whirlgig Geysers at Norris Geyser Basin

The tallest active geyser in the world, Steamboat Geyser,[11] is located in Norris Basin. Unlike the slightly smaller but much more famous Old Faithful Geyser located in Upper Geyser Basin, Steamboat has an erratic and lengthy timetable between major eruptions. During major eruptions, which may be separated by intervals of more than a year (the longest recorded span between major eruptions was 50 years), Steamboat erupts over 300 feet (90 m) into the air. Steamboat does not lie dormant between eruptions, instead displaying minor eruptions of approximately 40 feet (12 m).

 

Norris Geyser Basin periodically undergoes a large-scale, basin-wide thermal disturbance lasting a few weeks. Water levels fluctuate, and temperatures, pH, colors, and eruptive patterns change throughout the basin. During a disturbance in 1985, Porkchop Geyser continually jetted steam and water; in 1989, the same geyser apparently clogged with silica and blew up, throwing rocks more than 200 feet (61 m). In 2003 a park ranger observed it bubbling heavily, the first such activity seen since 1991. Activity increased dramatically in mid-2003. Because of high ground temperatures and new features beside the trail much of Back Basin was closed until October. In 2004 the boardwalk was routed around the dangerous area and now leads behind Porkchop Geyser.

 

North of Norris, Roaring Mountain is a large, acidic hydrothermal area (solfatara) with many fumaroles. In the late 19th and early 20th centuries, the number, size, and power of the fumaroles were much greater than today. The fumaroles are most easily seen in the cooler, low-light conditions of morning and evening.

 

The Gibbon Geyser Basin 44°41′58″N 110°44′34″W includes several thermal areas in the vicinity of the Gibbon River between Gibbon Falls and Norris. The most accessible feature in the basin is Beryl Spring, with a small boardwalk right along the Grand Loop Road. Artists' Paintpots is a small hydrothermal area south of Norris Junction that includes colorful hot springs and two large mudpots.

 

The Monument Geyser Basin 44°41′03″N 110°45′14″W has no active geysers, but its 'monuments' are siliceous sinter deposits similar to the siliceous spires discovered on the floor of Yellowstone Lake. Scientists hypothesize that this basin's structures formed from a hot water system in a glacially dammed lake during the waning stages of the Pinedale Glaciation. The basin is on a ridge reached by a very steep one-mile (1.6 km) trail south of Artists' Paint Pots. Other areas of thermal activity in Gibbon Geyser Basin lie off-trail.

 

South of Norris along the rim of the caldera is the Upper Geyser Basin 44°27′52″N 110°49′45″W, which has the highest concentration of geothermal features in the park. This complement of features includes the most famous geyser in the park, Old Faithful Geyser, as well as four other predictable large geysers. One of these large geysers in the area is Castle Geyser which is about 1,400 feet (430 m) northwest of Old Faithful. Castle Geyser has an interval of approximately 13 hours between major eruptions, but is unpredictable after minor eruptions. The other three predictable geysers are Grand Geyser, Daisy Geyser, and Riverside Geyser. Biscuit Basin and Black Sand Basin are also within the boundaries of Upper Geyser Basin.

 

The hills surrounding Old Faithful and the Upper Geyser Basin are reminders of Quaternary rhyolitic lava flows. These flows, occurring long after the catastrophic eruption of 640,000 years ago, flowed across the landscape like stiff mounds of bread dough due to their high silica content.

 

Evidence of glacial activity is common, and it is one of the keys that allows geysers to exist. Glacier till deposits underlie the geyser basins providing storage areas for the water used in eruptions. Many landforms, such as Porcupine Hills north of Fountain Flats, are made up of glacial gravel and are reminders that 70,000 to 14,000 years ago, this area was buried under ice.

 

Signs of the forces of erosion can be seen everywhere, from runoff channels carved across the sinter in the geyser basins to the drainage created by the Firehole River. Mountain building is evident on the drive south of Old Faithful, toward Craig Pass. Here the Rocky Mountains reach a height of 8,262 feet (2,518 m), dividing the country into two distinct watersheds.

 

Midway Geyser Basin 44°31′04″N 110°49′56″W is much smaller than the other basins found alongside the Firehole River. Despite its small size, it contains two large features, the 200-by-300-foot-wide (60 by 90 m) Excelsior Geyser which pours over 4,000 U.S. gallons (15,000 L; 3,300 imp gal) per minute into the Firehole River. The largest hot spring in Yellowstone, the 370-foot-wide (110 m) and 121-foot-deep (37 m) Grand Prismatic Spring is found here. Also in the basin is Turquoise Pool and Opal Pool.

 

Lower Geyser Basin

Blue spring with steam rising from it; irregular blotches of red and orange residue are on the banks, along with dead tree trunks.

Silex Spring at Fountain Paint Pot

 

Farther north is the Lower Geyser Basin 44°32′58″N 110°50′09″W, which is the largest geyser basin in area, covering approximately 11 square miles. Due to its large size, it has a much less concentrated set of geothermal features, including Fountain Paint Pots. Fountain Paint Pots are mud pots, that is, a hot spring that contains boiling mud instead of water. The mud is produced by a higher acidity in the water which enables the spring to dissolve surrounding minerals to create an opaque, usually grey, mud. Also there is Firehole Spring, Celestine Pool, Leather Pool, Red Spouter, Jelly spring, and a number of fumaroles.

 

Geysers in Lower Geyser Basin include Great Fountain Geyser, whose eruptions reach 100 to 200 feet (30–61 m) in the air, while waves of water cascade down its sinter terraces., the Fountain group of Geysers (Clepsydra Geyser which erupts nearly continuously to heights of 45 feet (14 m), Fountain Geyser, Jelly Geyser, Jet Geyser, Morning Geyser, and Spasm Geyser), the Pink Cone group of geysers (Dilemma Geyser, Labial Geyser, Narcissus Geyser, Pink Geyser, and Pink Cone Geyser), the White Dome group of geysers (Crack Geyser, Gemini Geyser, Pebble Geyser, Rejuvenated Geyser, and White Dome Geyser), as well as Sizzler Geyser.

 

Clepsydra Geyser erupting. July 2019

Fountain Paint Pots

White Dome Geyser

West Thumb Geyser Basin

Several pools of blue water in ashen rock basin.

West Thumb Geyser Basin

Blackened basin with orange streaks; steam is rising from it with fir trees in the background.

Overflow areas of Silex springs

 

The West Thumb Geyser Basin 44°25′07″N 110°34′23″W, including Potts Basin to the north, is the largest geyser basin on the shores of Yellowstone Lake. The heat source of the thermal features in this location is thought to be relatively close to the surface, only 10,000 feet (3,000 m) down. West Thumb is about the same size as another famous volcanic caldera, Crater Lake in Oregon, but much smaller than the great Yellowstone Caldera which last erupted about 640,000 years ago. West Thumb is a caldera within a caldera.

 

West Thumb was created approximately 162,000 years ago when a magma chamber bulged up under the surface of the earth and subsequently cracked it along ring fracture zones. This in turn released the enclosed magma as lava and caused the surface above the emptied magma chamber to collapse. Water later filled the collapsed area of the caldera, forming an extension of Yellowstone Lake. This created the source of heat and water that feed the West Thumb Geyser Basin today.

 

The thermal features at West Thumb are not only found on the lake shore, but extend under the surface of the lake as well. Several underwater hydrothermal features were discovered in the early 1990s and can be seen as slick spots or slight bulges in the summer. During the winter, the underwater thermal features are visible as melt holes in the icy surface of the lake. The surrounding ice can reach three feet (one yard) in thickness.

 

Perhaps the most famous hydrothermal feature at West Thumb is a geyser on the lake shore known as Fishing Cone. Walter Trumbull of the 1870 Washburn-Langford-Doane Expedition described a unique event while a man was fishing adjacent to the cone: "...in swinging a trout ashore, it accidentally got off the hook and fell into the spring. For a moment it darted about with wonderful rapidity, as if seeking an outlet. Then it came to the top, dead, and literally boiled." Fishing Cone erupted frequently to the height of 40 feet (12 m) in 1919 and to lesser heights in 1939. One fisherman was badly burned in Fishing Cone in 1921. Fishing at the geyser is now prohibited.

 

Early visitors would arrive at West Thumb via stagecoach from the Old Faithful area. They had a choice of continuing on the stagecoach or boarding the steamship Zillah to continue the journey by water to Lake Hotel. The boat dock was located near the south end of the geyser basin near Lakeside Spring.

 

Backcountry Geyser Basins

The Heart Lake 44°18′00″N 110°30′56″W, Lone Star 44°24′50″N 110°49′04″W, and Shoshone Geyser Basins 44°21′16″N 110°47′57″W are located away from the road and require at least several miles of hiking to reach. These areas lack the boardwalks and other safety features of the developed areas. As falling into geothermal features can be fatal, it is usually advisable to visit these areas with an experienced guide or at the very least, travelers need to ensure they remain on well-marked trails.

 

The Heart Lake Geyser Basin contains several groups of geysers and deep blue hot springs near Heart Lake in the south-central portion of Yellowstone, southeast of most of the main geyser basins. Lying in the Snake River watershed east of Lewis Lake and south of Yellowstone Lake, Heart Lake was named sometime before 1871 for Hart Hunney, a hunter. Other explorers in the region incorrectly assumed that the lake's name was spelled 'heart' because of its shape. The Heart Lake Geyser Basin begins a couple miles from the lake and descends along Witch Creek to the lakeshore. Five groups of hydrothermal features comprise the basin, and all of them contain geysers, although some are dormant.

 

Between Shoshone Lake and Old Faithful is the Lone Star Geyser Basin, of which the primary feature is Lone Star Geyser, named for its isolation from the nearby geysers of the Upper Geyser Basin. The basin is reachable on foot or bicycle via a 3 mile road that is closed to vehicles.

 

The Shoshone Geyser Basin, reached by hiking or by boat, contains one of the highest concentrations of geysers in the world – more than 80 in an area 1,600 by 800 feet (490 by 240 m). Hot springs and mudpots dot the landscape between the geyser basin and Shoshone Lake.

 

Hot Spring Basin is located 15 miles (24 km) north-northeast of Fishing Bridge and has one of Yellowstone's largest collections of hot springs and fumaroles. The geothermal features there release large amounts of sulfur. This makes water from the springs so acidic that it has dissolved holes in the pants of people who sit on wet ground and causes mounds of sulfur three feet (1 m) high to develop around fumaroles. The very hot acidic water and steam have also created voids in the ground that are only covered by a thin crust.

 

Mammoth Hot Springs is a large complex of hot springs on a hill of travertine in Yellowstone National Park adjacent to Fort Yellowstone and the Mammoth Hot Springs Historic District. It was created over thousands of years as hot water from the spring cooled and deposited calcium carbonate (over two tons flow into Mammoth each day in a solution). Because of the huge amount of geothermal vents, travertine flourishes. Although these springs lie outside the caldera boundary, their energy has been attributed to the same magmatic system that fuels other Yellowstone geothermal areas.

 

The thermal features at Mud Volcano and Sulphur Caldron are primarily mud pots and fumaroles because the area is situated on a perched water system with little water available. Fumaroles or "steam vents" occur when the ground water boils away faster than it can be recharged. Also, the vapors are rich in sulfuric acid that leaches the rock, breaking it down into clay. Because no water washes away the acid or leached rock, it remains as sticky clay to form a mud pot. Hydrogen sulfide gas is present deep in the earth at Mud Volcano and is oxidized to sulfuric acid by microbial activity, which dissolves the surface soils to create pools and cones of clay and mud. Along with hydrogen sulfide, steam, carbon dioxide, and other gases explode through the layers of mud.

 

A series of shallow earthquakes associated with the volcanic activity in Yellowstone struck this area in 1978. Soil temperatures increased to nearly 200 °F (93 °C). The slope between Sizzling Basin and Mud Geyser, once covered with green grass and trees, became a barren landscape of fallen trees known as "the cooking hillside".

 

Yellowstone National Park is a national park located in the western United States, largely in the northwest corner of Wyoming and extending into Montana and Idaho. It was established by the 42nd U.S. Congress with the Yellowstone National Park Protection Act and signed into law by President Ulysses S. Grant on March 1, 1872. Yellowstone was the first national park in the U.S. and is also widely held to be the first national park in the world. The park is known for its wildlife and its many geothermal features, especially the Old Faithful geyser, one of its most popular. While it represents many types of biomes, the subalpine forest is the most abundant. It is part of the South Central Rockies forests ecoregion.

 

While Native Americans have lived in the Yellowstone region for at least 11,000 years, aside from visits by mountain men during the early-to-mid-19th century, organized exploration did not begin until the late 1860s. Management and control of the park originally fell under the jurisdiction of the U.S. Department of the Interior, the first Secretary of the Interior to supervise the park being Columbus Delano. However, the U.S. Army was eventually commissioned to oversee the management of Yellowstone for 30 years between 1886 and 1916. In 1917, the administration of the park was transferred to the National Park Service, which had been created the previous year. Hundreds of structures have been built and are protected for their architectural and historical significance, and researchers have examined more than a thousand archaeological sites.

 

Yellowstone National Park spans an area of 3,468.4 sq mi (8,983 km2), comprising lakes, canyons, rivers, and mountain ranges. Yellowstone Lake is one of the largest high-elevation lakes in North America and is centered over the Yellowstone Caldera, the largest super volcano on the continent. The caldera is considered a dormant volcano. It has erupted with tremendous force several times in the last two million years. Well over half of the world's geysers and hydrothermal features are in Yellowstone, fueled by this ongoing volcanism. Lava flows and rocks from volcanic eruptions cover most of the land area of Yellowstone. The park is the centerpiece of the Greater Yellowstone Ecosystem, the largest remaining nearly intact ecosystem in the Earth's northern temperate zone. In 1978, Yellowstone was named a UNESCO World Heritage Site.

 

Hundreds of species of mammals, birds, fish, reptiles, and amphibians have been documented, including several that are either endangered or threatened. The vast forests and grasslands also include unique species of plants. Yellowstone Park is the largest and most famous megafauna location in the contiguous United States. Grizzly bears, cougars, wolves, and free-ranging herds of bison and elk live in this park. The Yellowstone Park bison herd is the oldest and largest public bison herd in the United States. Forest fires occur in the park each year; in the large forest fires of 1988, nearly one-third of the park was burnt. Yellowstone has numerous recreational opportunities, including hiking, camping, boating, fishing, and sightseeing. Paved roads provide close access to the major geothermal areas as well as some of the lakes and waterfalls. During the winter, visitors often access the park by way of guided tours that use either snow coaches or snowmobiles.

 

Teton County is a county in the U.S. state of Wyoming. As of the 2020 United States Census, the population was 23,331. Its county seat is Jackson. Its west boundary line is also the Wyoming state boundary shared with Idaho and the southern tip of Montana. Teton County is part of the Jackson, WY-ID Micropolitan Statistical Area.

 

Teton County contains the Jackson Hole ski area, all of Grand Teton National Park, and 40.4% of Yellowstone National Park's total area, including over 96.6% of its water area (largely in Yellowstone Lake).

 

Wyoming is a state in the Mountain West subregion of the Western United States. It borders Montana to the north and northwest, South Dakota and Nebraska to the east, Idaho to the west, Utah to the southwest, and Colorado to the south. With a population of 576,851 in 2020, Wyoming is the least populous state despite being the 10th largest by area, with the second-lowest population density after Alaska. The state capital and most populous city is Cheyenne, which had an estimated population of 63,957 in 2018.

 

Wyoming's western half consists mostly of the ranges and rangelands of the Rocky Mountains; its eastern half consists of high-elevation prairie, and is referred to as the High Plains. Wyoming's climate is semi-arid in some parts and continental in others, making it drier and windier overall than other states, with greater temperature extremes. The federal government owns just under half of Wyoming's land, generally protecting it for public uses. The state ranks sixth in the amount of land—-and fifth in the proportion of its land—-that is owned by the federal government. Its federal lands include two national parks (Grand Teton and Yellowstone), two national recreation areas, two national monuments, and several national forests, as well as historic sites, fish hatcheries, and wildlife refuges.

 

Indigenous peoples inhabited the region for thousands of years. Historic and currently federally recognized tribes include the Arapaho, Crow, Lakota, and Shoshone. Part of the land that is now Wyoming came under American sovereignty via the Louisiana Purchase, part via the Oregon Treaty, and, lastly, via the Mexican Cession. With the opening of the Oregon Trail, the Mormon Trail, and the California Trail, vast numbers of pioneers travelled through parts of the state that had once been traversed mainly by fur trappers, and this spurred the establishment of forts, such as Fort Laramie, that today serve as population centers. The Transcontinental Railroad supplanted the wagon trails in 1867 with a route through southern Wyoming, bringing new settlers and the establishment of founding towns, including the state capital of Cheyenne. On March 27, 1890, Wyoming became the union's 44th state.

 

Farming and ranching, and the attendant range wars, feature prominently in the state's history. Today, Wyoming's economy is largely based on tourism and the extraction of minerals such as coal, natural gas, oil, and trona. Its agricultural commodities include barley, hay, livestock, sugar beets, wheat, and wool.

 

Wyoming was the first state to allow women the right to vote (not counting New Jersey, which had allowed it until 1807), and the right to assume elected office, as well as the first state to elect a female governor. In honor of this part of its history, its most common nickname is "The Equality State" and its official state motto is "Equal Rights". It is among the least religious states in the country, and is known for having a political culture that leans towards libertarian conservatism. The Republican presidential nominee has carried the state in every election since 1968.

REYKJAVIK, ICELAND - APRIL 7: Team OpTic poses for the VALORANT Masters Features Day on April 7, 2022 in Reykjavik, Iceland. (Photo by Lance Skundrich/Riot Games)

Features working catapult to throw the sanctum key.

SAO PAULO, BRAZIL - FEBRUARY 18: Tyson "TenZ" Ngo of the Sentinels poses during the VALORANT Champions Tour 2023: LOCK//IN features day on February 18, 2023 in Sao Paulo, Brazil. (Photo by Lance Skundrich/Riot Games)

Wells Cathedral is an Anglican cathedral in Wells, Somerset, England, dedicated to St Andrew the Apostle. It is the seat of the Bishop of Bath and Wells, whose cathedra it holds as mother church of the Diocese of Bath and Wells. Built as a Roman Catholic cathedral from around 1175 to replace an earlier church on the site since 705, it became an Anglican cathedral when King Henry VIII split from Rome. It is moderately sized for an English cathedral. Its broad west front and large central tower are dominant features. It has been called "unquestionably one of the most beautiful" and "most poetic" of English cathedrals.

 

Its Gothic architecture is mostly inspired from Early English style of the late 12th to early 13th centuries, lacking the Romanesque work that survives in many other cathedrals. Building began about 1175 at the east end with the choir. Historian John Harvey sees it as Europe's first truly Gothic structure, breaking the last constraints of Romanesque. The stonework of its pointed arcades and fluted piers bears pronounced mouldings and carved capitals in a foliate, "stiff-leaf" style. Its Early English front with 300 sculpted figures is seen as a "supreme triumph of the combined plastic arts in England". The east end retains much ancient stained glass. Unlike many cathedrals of monastic foundation, Wells has many surviving secular buildings linked to its chapter of secular canons, including the Bishop's Palace and the 15th-century residential Vicars' Close It is a Grade I listed building.

 

The earliest remains of a building on the site are of a late-Roman mausoleum, identified during excavations in 1980. An abbey church was built in Wells in 705 by Aldhelm, first bishop of the newly established Diocese of Sherborne during the reign of King Ine of Wessex. It was dedicated to St Andrew and stood at the site of the cathedral's cloisters, where some excavated remains can be seen. The font in the cathedral's south transept is from this church and is the oldest part of the present building. In 766 Cynewulf, King of Wessex, signed a charter endowing the church with eleven hides of land. In 909 the seat of the diocese was moved from Sherborne to Wells.

 

The first bishop of Wells was Athelm (909), who crowned King Æthelstan. Athelm and his nephew Dunstan both became Archbishops of Canterbury. During this period a choir of boys was established to sing the liturgy. Wells Cathedral School, which was established to educate these choirboys, dates its foundation to this point. There is, however, some controversy over this. Following the Norman Conquest, John de Villula moved the seat of the bishop from Wells to Bath in 1090. The church at Wells, no longer a cathedral, had a college of secular clergy.

 

The cathedral is thought to have been conceived and commenced in about 1175 by Reginald Fitz Jocelin, who died in 1191. Although it is clear from its size that from the outset, the church was planned to be the cathedral of the diocese, the seat of the bishop moved between Wells and the abbeys of Glastonbury and Bath, before settling at Wells. In 1197 Reginald's successor, Savaric FitzGeldewin, with the approval of Pope Celestine III, officially moved his seat to Glastonbury Abbey. The title of Bishop of Bath and Glastonbury was used until the Glastonbury claim was abandoned in 1219.

 

Savaric's successor, Jocelin of Wells, again moved the bishop's seat to Bath Abbey, with the title Bishop of Bath. Jocelin was a brother of Hugh (II) of Lincoln and was present at the signing of the Magna Carta. Jocelin continued the building campaign begun by Reginald and was responsible for the Bishop's Palace, the choristers' school, a grammar school, a hospital for travellers and a chapel. He also had a manor house built at Wookey, near Wells. Jocelin saw the church dedicated in 1239 but, despite much lobbying of the Pope by Jocelin's representatives in Rome, did not live to see cathedral status granted. The delay may have been a result of inaction by Pandulf Verraccio, a Roman ecclesiastical politician, papal legate to England and Bishop of Norwich, who was asked by the Pope to investigate the situation but did not respond. Jocelin died at Wells on 19 November 1242 and was buried in the choir of the cathedral; the memorial brass on his tomb is one of the earliest brasses in England. Following his death the monks of Bath unsuccessfully attempted to regain authority over Wells.

 

In 1245 the ongoing dispute over the title of the bishop was resolved by a ruling of Pope Innocent IV, who established the title as the "Bishop of Bath and Wells", which it has remained until this day, with Wells as the principal seat of the bishop. Since the 11th century the church has had a chapter of secular clergy, like the cathedrals of Chichester, Hereford, Lincoln and York. The chapter was endowed with 22 prebends (lands from which finance was drawn) and a provost to manage them. On acquiring cathedral status, in common with other such cathedrals, it had four chief clergy, the dean, precentor, chancellor and sacristan, who were responsible for the spiritual and material care of the cathedral.

 

The building programme, begun by Reginald Fitz Jocelin, Bishop in the 12th century, continued under Jocelin of Wells, who was a canon from 1200, then bishop from 1206. Adam Locke was master mason from about 1192 until 1230. It was designed in the new style with pointed arches, later known as Gothic, which was introduced at about the same time at Canterbury Cathedral. Work was halted between 1209 and 1213 when King John was excommunicated and Jocelin was in exile, but the main parts of the church were complete by the time of the dedication by Jocelin in 1239.

 

By the time the cathedral, including the chapter house, was finished in 1306, it was already too small for the developing liturgy, and unable to accommodate increasingly grand processions of clergy. John Droxford initiated another phase of building under master mason Thomas of Whitney, during which the central tower was heightened and an eight-sided Lady chapel was added at the east end by 1326. Ralph of Shrewsbury followed, continuing the eastward extension of the choir and retrochoir beyond. He oversaw the building of Vicars' Close and the Vicars' Hall, to give the men who were employed to sing in the choir a secure place to live and dine, away from the town and its temptations. He had an uneasy relationship with the citizens of Wells, partly because of his imposition of taxes, and he surrounded his palace with crenellated walls, a moat and a drawbridge.

 

John Harewell raised money for the completion of the west front by William Wynford, who was appointed as master mason in 1365. One of the foremost master masons of his time, Wynford worked for the king at Windsor, Winchester Cathedral and New College, Oxford. At Wells, he designed the western towers of which north-west was not built until the following century. In the 14th century, the central piers of the crossing were found to be sinking under the weight of the crossing tower which had been damaged by an earthquake in the previous century. Strainer arches, sometimes described as scissor arches, were inserted by master mason William Joy to brace and stabilise the piers as a unit.

 

By the reign of Henry VII the cathedral was complete, appearing much as it does today (though the fittings have changed). From 1508 to 1546, the eminent Italian humanist scholar Polydore Vergil was active as the chapter's representative in London. He donated a set of hangings for the choir of the cathedral. While Wells survived the Dissolution of the Monasteries better than the cathedrals of monastic foundation, the abolition of chantries in 1547 resulted in a reduction in its income. Medieval brasses were sold, and a pulpit was placed in the nave for the first time. Between 1551 and 1568, in two periods as dean, William Turner established a herb garden, which was recreated between 2003 and 2010.

 

Elizabeth I gave the chapter and the Vicars Choral a new charter in 1591, creating a new governing body, consisting of a dean and eight residentiary canons with control over the church estates and authority over its affairs, but no longer entitled to elect the dean (that entitlement thenceforward belonged ultimately to the Crown). The stability brought by the new charter ended with the onset of the Civil War and the execution of Charles I. Local fighting damaged the cathedral's stonework, furniture and windows. The dean, Walter Raleigh, a nephew of the explorer Walter Raleigh, was placed under house arrest after the fall of Bridgwater to the Parliamentarians in 1645, first in the rectory at Chedzoy and then in the deanery at Wells. His jailor, the shoe maker and city constable, David Barrett, caught him writing a letter to his wife. When he refused to surrender it, Barrett ran him through with a sword and he died six weeks later, on 10 October 1646. He was buried in an unmarked grave in the choir before the dean's stall. During the Commonwealth of England under Oliver Cromwell no dean was appointed and the cathedral fell into disrepair. The bishop went into retirement and some of the clerics were reduced to performing menial tasks.

 

In 1661, after Charles II was restored to the throne, Robert Creighton, the king's chaplain in exile, was appointed dean and was bishop for two years before his death in 1672. His brass lectern, given in thanksgiving, can be seen in the cathedral. He donated the nave's great west window at a cost of £140. Following Creighton's appointment as bishop, the post of dean went to Ralph Bathurst, who had been chaplain to the king, president of Trinity College, Oxford and fellow of the Royal Society. During Bathurst's long tenure the cathedral was restored, but in the Monmouth Rebellion of 1685, Puritan soldiers damaged the west front, tore lead from the roof to make bullets, broke the windows, smashed the organ and furnishings, and for a time stabled their horses in the nave.

 

Restoration began again under Thomas Ken who was appointed by the Crown in 1685 and served until 1691. He was one of seven bishops imprisoned for refusing to sign King James II's "Declaration of Indulgence", which would have enabled Catholics to resume positions of political power, but popular support led to their acquittal. Ken refused to take the oath of allegiance to William III and Mary II because James II had not abdicated and with others, known as the Nonjurors, was put out of office. His successor, Richard Kidder, was killed in the Great Storm of 1703 when two chimney stacks on the palace fell on him and his wife, while they were asleep in bed.

 

By the middle of the 19th century, a major restoration programme was needed. Under Dean Goodenough, the monuments were moved to the cloisters and the remaining medieval paint and whitewash removed in an operation known as "the great scrape". Anthony Salvin took charge of the extensive restoration of the choir. Wooden galleries installed in the 16th century were removed and the stalls were given stone canopies and placed further back within the line of the arcade. The medieval stone pulpitum screen was extended in the centre to support a new organ.

 

In 1933 the Friends of Wells Cathedral were formed to support the cathedral's chapter in the maintenance of the fabric, life and work of the cathedral. The late 20th century saw an extensive restoration programme, particularly of the west front. The stained glass is currently under restoration, with a programme underway to conserve the large 14th-century Jesse Tree window at the eastern terminal of the choir.

 

In January 2014, as part of the Bath film festival, the cathedral hosted a special screening of Martin Scorsese's The Last Temptation of Christ. This provoked some controversy, but the church defended its decision to allow the screening.

 

In 2021, a contemporary sculpture by Anthony Gormley was unveiled on a temporary plinth outside the cathedral.

 

Since the 13th century, Wells Cathedral has been the seat of the Bishop of Bath and Wells. Its governing body, the chapter, is made up of five clerical canons (the dean, the precentor, the canon chancellor, the canon treasurer, and the archdeacon of Wells) and four lay members: the administrator (chief executive), Keeper of the Fabric, Overseer of the Estate and the chairman of the cathedral shop and catering boards. The current bishop of Bath and Wells is Peter Hancock, who was installed in a service in the cathedral on 7 June 2014. John Davies has been Dean of Wells since 2016.

 

Employed staff include the organist and master of choristers, head Verger archivist, librarian and the staff of the shop, café and restaurant. The chapter is advised by specialists such as architects, archaeologists and financial analysts.

 

More than a thousand services are held every year. There are daily services of Matins, Holy Communion and Choral Evensong, as well as major celebrations of Christian festivals such as Christmas, Easter, Pentecost and saints' days. The cathedral is also used for the baptisms, weddings and funerals of those with close connections to it. In July 2009 the cathedral undertook the funeral of Harry Patch, the last British Army veteran of World War I, who died at the age of 111.

 

Three Sunday services are led by the resident choir in school terms and choral services are sung on weekdays. The cathedral hosts visiting choirs and does outreach work with local schools as part of its Chorister Outreach Project. It is also a venue for musical events such as an annual concert by the Somerset Chamber Choir.

 

Each year about 150,000 people attend services and another 300,000 visit as tourists. Entry is free, but visitors are encouraged to make a donation towards the annual running costs of around £1.5 million in 2015.

 

Construction of the cathedral began in about 1175, to the design of an unknown master-mason. Wells is the first cathedral in England to be built, from its foundation, in Gothic style. According to art historian John Harvey, it is the first truly Gothic cathedral in the world, its architects having entirely dispensed with all features that bound the contemporary east end of Canterbury Cathedral and the earlier buildings of France, such as the east end of the Abbey of Saint Denis, to the Romanesque. Unlike these churches, Wells has clustered piers rather than columns and has a gallery of identical pointed arches rather than the typically Romanesque form of paired openings. The style, with its simple lancet arches without tracery and convoluted mouldings, is known as Early English Gothic.

 

From about 1192 to 1230, Adam Lock, the earliest master-mason at Wells for whom a name is known, continued the transept and nave in the same manner as his predecessor. Lock was also the builder of the north porch, to his own design.

 

The Early English west front was commenced around 1230 by Thomas Norreys, with building and sculpture continuing for thirty years. Its south-west tower was begun 100 years later and constructed between 1365 and 1395, and the north-west tower between 1425 and 1435, both in the Perpendicular Gothic style to the design of William Wynford, who also filled many of the cathedral's early English lancet windows with delicate tracery.

 

The undercroft and chapter house were built by unknown architects between 1275 and 1310, the undercroft in the Early English and the chapter house in the Geometric style of Decorated Gothic architecture. In about 1310 work commenced on the Lady Chapel, to the design of Thomas Witney, who also built the central tower from 1315 to 1322 in the Decorated Gothic style. The tower was later braced internally with arches by William Joy. Concurrent with this work, in 1329–45 Joy made alterations and extensions to the choir, joining it to the Lady Chapel with the retrochoir, the latter in the Flowing Decorated style.

 

Later changes include the Perpendicular vault of the tower and construction of Sugar's Chapel, 1475–1490 by William Smyth. Also, Gothic Revival renovations were made to the choir and pulpitum by Benjamin Ferrey and Anthony Salvin, 1842–1857.

 

Wells has a total length of 415 feet (126 m). Like Canterbury, Lincoln and Salisbury cathedrals, it has the distinctly English arrangement of two transepts, with the body of the church divided into distinct parts: nave, choir, and retro-choir, beyond which extends the Lady Chapel. The façade is wide, with its towers extending beyond the transepts on either side. There is a large projecting porch on the north side of the nave forming an entry into the cathedral. To the north-east is the large octagonal chapter house, entered from the north choir aisle by a passage and staircase. To the south of the nave is a large cloister, unusual in that the northern range, that adjacent the cathedral, was never built.

 

In section, the cathedral has the usual arrangement of a large church: a central nave with an aisle on each side, separated by two arcades. The elevation is in three stages, arcade, triforium gallery and clerestory. The nave is 67 feet (20 m) in height, very low compared to the Gothic cathedrals of France. It has a markedly horizontal emphasis, caused by the triforium having a unique form, a series of identical narrow openings, lacking the usual definition of the bays. The triforium is separated from the arcade by a single horizontal string course that runs unbroken the length of the nave. There are no vertical lines linking the three stages, as the shafts supporting the vault rise above the triforium.

 

The exterior of Wells Cathedral presents a relatively tidy and harmonious appearance since the greater part of the building was executed in a single style, Early English Gothic. This is uncommon among English cathedrals where the exterior usually exhibits a plethora of styles. At Wells, later changes in the Perpendicular style were universally applied, such as filling the Early English lancet windows with simple tracery, the construction of a parapet that encircles the roof, and the addition of pinnacles framing each gable, similar to those around the chapter house and on the west front. At the eastern end there is a proliferation of tracery with repeated motifs in the Reticulated style, a stage between Geometric and Flowing Decorated tracery.

 

The west front is 100 feet (30 m) high and 147 feet (45 m) wide, and built of Inferior Oolite of the Middle Jurassic period, which came from the Doulting Stone Quarry, about 8 miles (13 km) to the east. According to the architectural historian Alec Clifton-Taylor, it is "one of the great sights of England".

 

West fronts in general take three distinct forms: those that follow the elevation of the nave and aisles, those that have paired towers at the end of each aisle, framing the nave, and those that screen the form of the building. The west front at Wells has the paired-tower form, unusual in that the towers do not indicate the location of the aisles, but extend well beyond them, screening the dimensions and profile of the building.

 

The west front rises in three distinct stages, each clearly defined by a horizontal course. This horizontal emphasis is counteracted by six strongly projecting buttresses defining the cross-sectional divisions of nave, aisles and towers, and are highly decorated, each having canopied niches containing the largest statues on the façade.

 

At the lowest level of the façade is a plain base, contrasting with and stabilising the ornate arcades that rise above it. The base is penetrated by three doors, which are in stark contrast to the often imposing portals of French Gothic cathedrals. The outer two are of domestic proportion and the central door is ornamented only by a central post, quatrefoil and the fine mouldings of the arch.

 

Above the basement rise two storeys, ornamented with quatrefoils and niches originally holding about four hundred statues, with three hundred surviving until the mid-20th century. Since then, some have been restored or replaced, including the ruined figure of Christ in the gable.

 

The third stages of the flanking towers were both built in the Perpendicular style of the late 14th century, to the design of William Wynford; that on the north-west was not begun until about 1425. The design maintains the general proportions, and continues the strong projection of the buttresses.

 

The finished product has been criticised for its lack of pinnacles, and it is probable that the towers were intended to carry spires which were never built. Despite its lack of spires or pinnacles, the architectural historian Banister Fletcher describes it as "the highest development in English Gothic of this type of façade."

 

The sculptures on the west front at Wells include standing figures, seated figures, half-length angels and narratives in high relief. Many of the figures are life-sized or larger. Together they constitute the finest display of medieval carving in England. The figures and many of the architectural details were painted in bright colours, and the colouring scheme has been deduced from flakes of paint still adhering to some surfaces. The sculptures occupy nine architectural zones stretching horizontally across the entire west front and around the sides and the eastern returns of the towers which extend beyond the aisles. The strongly projecting buttresses have tiers of niches which contain many of the largest figures. Other large figures, including that of Christ, occupy the gable. A single figure stands in one of two later niches high on the northern tower.

 

In 1851 the archaeologist Charles Robert Cockerell published his analysis of the iconography, numbering the nine sculptural divisions from the lowest to the highest. He defined the theme as "a calendar for unlearned men" illustrating the doctrines and history of the Christian faith, its introduction to Britain and its protection by princes and bishops. He likens the arrangement and iconography to the Te Deum.

 

According to Cockerell, the side of the façade that is to the south of the central door is the more sacred and the scheme is divided accordingly. The lowest range of niches each contained a standing figure, of which all but four figures on the west front, two on each side, have been destroyed. More have survived on the northern and eastern sides of the north tower. Cockerell speculates that those to the south of the portal represented prophets and patriarchs of the Old Testament while those to the north represented early missionaries to Britain, of which Augustine of Canterbury, St Birinus, and Benedict Biscop are identifiable by their attributes. In the second zone, above each pair of standing figures, is a quatrefoil containing a half-length angel in relief, some of which have survived. Between the gables of the niches are quatrefoils that contain a series of narratives from the Bible, with the Old Testament stories to the south, above the prophets and patriarchs, and those from the New Testament to the north. A horizontal course runs around the west front dividing the architectural storeys at this point.

 

Above the course, zones four and five, as identified by Cockerell, contain figures which represent the Christian Church in Britain, with the spiritual lords such as bishops, abbots, abbesses and saintly founders of monasteries on the south, while kings, queens and princes occupy the north. Many of the figures survive and many have been identified in the light of their various attributes. There is a hierarchy of size, with the more significant figures larger and enthroned in their niches rather than standing. Immediately beneath the upper course are a series of small niches containing dynamic sculptures of the dead coming forth from their tombs on the Day of Judgement. Although naked, some of the dead are defined as royalty by their crowns and others as bishops by their mitres. Some emerge from their graves with joy and hope, and others with despair.

 

The niches in the lowest zone of the gable contain nine angels, of which Cockerell identifies Michael, Gabriel, Raphael and Uriel. In the next zone are the taller figures of the twelve apostles, some, such as John, Andrew and Bartholomew, clearly identifiable by the attributes that they carry. The uppermost niches of the gable contained the figure of Christ the Judge at the centre, with the Virgin Mary on his right and John the Baptist on his left. The figures all suffered from iconoclasm. A new statue of Jesus was carved for the central niche, but the two side niches now contain cherubim. Christ and the Virgin Mary are also represented by now headless figures in a Coronation of the Virgin in a niche above the central portal. A damaged figure of the Virgin and Christ Child occupies a quatrefoil in the spandrel of the door.

 

The central tower appears to date from the early 13th century. It was substantially reconstructed in the early 14th century during the remodelling of the east end, necessitating the internal bracing of the piers a decade or so later. In the 14th century the tower was given a timber and lead spire which burnt down in 1439. The exterior was then reworked in the Perpendicular style and given the present parapet and pinnacles. Alec Clifton-Taylor describes it as "outstanding even in Somerset, a county famed for the splendour of its church towers".

 

The north porch is described by art historian Nikolaus Pevsner as "sumptuously decorated", and intended as the main entrance. Externally it is simple and rectangular with plain side walls. The entrance is a steeply arched portal framed by rich mouldings of eight shafts with stiff-leaf capitals each encircled by an annular moulding at middle height. Those on the left are figurative, containing images representing the martyrdom of St Edmund the Martyr. The walls are lined with deep niches framed by narrow shafts with capitals and annulets like those of the portal. The path to the north porch is lined by four sculptures in Purbeck stone, each by Mary Spencer Watson, representing the symbols of the Evangelists.

 

The cloisters were built in the late 13th century and largely rebuilt from 1430 to 1508 and have wide openings divided by mullions and transoms, and tracery in the Perpendicular Gothic style. The vault has lierne ribs that form octagons at the centre of each compartment, the joints of each rib having decorative bosses. The eastern range is of two storeys, of which the upper is the library built in the 15th century.

 

Because Wells Cathedral was secular rather than monastic, cloisters were not a practical necessity. They were omitted from several other secular cathedrals but were built here and at Chichester. Explanations for their construction at these two secular cathedrals range from the processional to the aesthetic. As at Chichester, there is no northern range to the cloisters. In monastic cloisters it was the north range, benefiting most from winter sunlight, that was often used as a scriptorium.

 

In 1969, when a large chunk of stone fell from a statue near the main door, it became apparent that there was an urgent need for restoration of the west front. Detailed studies of the stonework and of conservation practices were undertaken under the cathedral architect, Alban D. R. Caroe and a restoration committee formed. The methods selected were those devised by Eve and Robert Baker. W. A. (Bert) Wheeler, clerk of works to the cathedral 1935–1978, had previously experimented with washing and surface treatment of architectural carvings on the building and his techniques were among those tried on the statues.

 

The conservation was carried out between 1974 and 1986, wherever possible using non-invasive procedures such as washing with water and a solution of lime, filling gaps and damaged surfaces with soft mortar to prevent the ingress of water and stabilising statues that were fracturing through corrosion of metal dowels. The surfaces were finished by painting with a thin coat of mortar and silane to resist further erosion and attack by pollutants. The restoration of the façade revealed much paint adhering to the statues and their niches, indicating that it had once been brightly coloured.

 

The particular character of this Early English interior is dependent on the proportions of the simple lancet arches. It is also dependent on the refinement of the architectural details, in particular the mouldings.

 

The arcade, which takes the same form in the nave, choir and transepts, is distinguished by the richness of both mouldings and carvings. Each pier of the arcade has a surface enrichment of 24 slender shafts in eight groups of three, rising beyond the capitals to form the deeply undulating mouldings of the arches. The capitals themselves are remarkable for the vitality of the stylised foliage, in a style known as "stiff-leaf". The liveliness contrasts with the formality of the moulded shafts and the smooth unbroken areas of ashlar masonry in the spandrels. Each capital is different, and some contain small figures illustrating narratives.

 

The vault of the nave rises steeply in a simple quadripartite form, in harmony with the nave arcade. The eastern end of the choir was extended and the whole upper part elaborated in the second quarter of the 14th century by William Joy. The vault has a multiplicity of ribs in a net-like form, which is very different from that of the nave, and is perhaps a recreation in stone of a local type of compartmented wooden roof of which examples remain from the 15th century, including those at St Cuthbert's Church, Wells. The vaults of the aisles of the choir also have a unique pattern.

 

Until the early 14th century, the interior of the cathedral was in a unified style, but it was to undergo two significant changes, to the tower and to the eastern end. Between 1315 and 1322 the central tower was heightened and topped by a spire, which caused the piers that supported it to show signs of stress. In 1338 the mason William Joy employed an unorthodox solution by inserting low arches topped by inverted arches of similar dimensions, forming scissors-like structures. These arches brace the piers of the crossing on three sides, while the easternmost side is braced by a choir screen. The bracing arches are known as "St Andrew's Cross arches", in a reference to the patron saint of the cathedral. They have been described by Wim Swaan – rightly or wrongly – as "brutally massive" and intrusive in an otherwise restrained interior.

 

Wells Cathedral has a square east end to the choir, as is usual, and like several other cathedrals including Salisbury and Lichfield, has a lower Lady Chapel projecting at the eastern end, begun by Thomas Witney in about 1310, possibly before the chapter house was completed. The Lady Chapel seems to have begun as a free-standing structure in the form of an elongated octagon, but the plan changed and it was linked to the eastern end by extension of the choir and construction of a second transept or retrochoir east of the choir, probably by William Joy.

 

The Lady Chapel has a vault of complex and somewhat irregular pattern, as the chapel is not symmetrical about both axes. The main ribs are intersected by additional non-supporting, lierne ribs, which in this case form a star-shaped pattern at the apex of the vault. It is one of the earliest lierne vaults in England. There are five large windows, of which four are filled with fragments of medieval glass. The tracery of the windows is in the style known as Reticulated Gothic, having a pattern of a single repeated shape, in this case a trefoil, giving a "reticulate" or net-like appearance.

 

The retrochoir extends across the east end of the choir and into the east transepts. At its centre the vault is supported by a remarkable structure of angled piers. Two of these are placed as to complete the octagonal shape of the Lady Chapel, a solution described by Francis Bond as "an intuition of Genius". The piers have attached shafts of marble, and, with the vaults that they support, create a vista of great complexity from every angle. The windows of the retrochoir are in the Reticulated style like those of the Lady Chapel, but are fully Flowing Decorated in that the tracery mouldings form ogival curves.

 

The chapter house was begun in the late 13th century and built in two stages, completed about 1310. It is a two-storeyed structure with the main chamber raised on an undercroft. It is entered from a staircase which divides and turns, one branch leading through the upper storey of Chain Gate to Vicars' Close. The Decorated interior is described by Alec Clifton-Taylor as "architecturally the most beautiful in England". It is octagonal, with its ribbed vault supported on a central column. The column is surrounded by shafts of Purbeck Marble, rising to a single continuous rippling foliate capital of stylised oak leaves and acorns, quite different in character from the Early English stiff-leaf foliage. Above the moulding spring 32 ribs of strong profile, giving an effect generally likened to "a great palm tree". The windows are large with Geometric Decorated tracery that is beginning to show an elongation of form, and ogees in the lesser lights that are characteristic of Flowing Decorated tracery. The tracery lights still contain ancient glass. Beneath the windows are 51 stalls, the canopies of which are enlivened by carvings including many heads carved in a light-hearted manner.

 

Wells Cathedral contains one of the most substantial collections of medieval stained glass in England, despite damage by Parliamentary troops in 1642 and 1643. The oldest surviving glass dates from the late 13th century and is in two windows on the west side of the chapter-house staircase. Two windows in the south choir aisle are from 1310 to 1320.

 

The Lady Chapel has five windows, of which four date from 1325 to 1330 and include images of a local saint, Dunstan. The east window was restored to a semblance of its original appearance by Thomas Willement in 1845. The other windows have complete canopies, but the pictorial sections are fragmented.

 

The east window of the choir is a broad, seven-light window dating from 1340 to 1345. It depicts the Tree of Jesse (the genealogy of Christ) and demonstrates the use of silver staining, a new technique that allowed the artist to paint details on the glass in yellow, as well as black. The combination of yellow and green glass and the application of the bright yellow stain gives the window its popular name, the "Golden Window". It is flanked by two windows each side in the clerestory, with large figures of saints, also dated to 1340–45. In 2010 a major conservation programme was undertaken on the Jesse Tree window.

 

The panels in the chapel of St Katherine are attributed to Arnold of Nijmegen and date from about 1520. They were acquired from the destroyed church of Saint-Jean, Rouen, with the last panel having been purchased in 1953.

 

The large triple lancet to the nave west end was glazed at the expense of Dean Creighton at a cost of £140 in 1664. It was repaired in 1813, and the central light was largely replaced to a design by Archibald Keightley Nicholson between 1925 and 1931. The main north and south transept end windows by James Powell and Sons were erected in the early 20th century.

 

The greater part of the stone carving of Wells Cathedral comprises foliate capitals in the stiff-leaf style. They are found ornamenting the piers of the nave, choir and transepts. Stiff-leaf foliage is highly abstract. Though possibly influenced by carvings of acanthus leaves or vine leaves, it cannot be easily identified with any particular plant. Here the carving of the foliage is varied and vigorous, the springing leaves and deep undercuts casting shadows that contrast with the surface of the piers. In the transepts and towards the crossing in the nave the capitals have many small figurative carvings among the leaves. These include a man with toothache and a series of four scenes depicting the "Wages of Sin" in a narrative of fruit stealers who creep into an orchard and are then beaten by the farmer. Another well-known carving is in the north transept aisle: a foliate corbel, on which climbs a lizard, sometimes identified as a salamander, a symbol of eternal life.

 

Carvings in the Decorated Gothic style may be found in the eastern end of the buildings, where there are many carved bosses. In the chapter house, the carvings of the 51 stalls include numerous small heads of great variety, many of them smiling or laughing. A well-known figure is the corbel of the dragon-slaying monk in the chapter house stair. The large continuous capital that encircles the central pillar of the chapter house is markedly different in style to the stiff-leaf of the Early English period. In contrast to the bold projections and undercutting of the earlier work, it has a rippling form and is clearly identifiable as grapevine.

 

The 15th-century cloisters have many small bosses ornamenting the vault. Two in the west cloister, near the gift shop and café, have been called sheela na gigs, i. e. female figures displaying their genitals and variously judged to depict the sin of lust or stem from ancient fertility cults.

 

Wells Cathedral has one of the finest sets of misericords in Britain. Its clergy has a long tradition of singing or reciting from the Book of Psalms each day, along with the customary daily reading of the Holy Office. In medieval times the clergy assembled in the church eight times daily for the canonical hours. As the greater part of the services was recited while standing, many monastic or collegiate churches fitted stalls whose seats tipped up to provide a ledge for the monk or cleric to lean against. These were "misericords" because their installation was an act of mercy. Misericords typically have a carved figurative bracket beneath the ledge framed by two floral motifs known, in heraldic manner, as "supporters".

 

The misericords date from 1330 to 1340. They may have been carved under the direction of Master Carpenter John Strode, although his name is not recorded before 1341. He was assisted by Bartholomew Quarter, who is documented from 1343. They originally numbered 90, of which 65 have survived. Sixty-one are installed in the choir, three are displayed in the cathedral, and one is held by the Victoria and Albert Museum. New stalls were ordered when the eastern end of the choir was extended in the early 14th century. The canons complained that they had borne the cost of the rebuilding and ordered the prebendary clerics to pay for their own stalls. When the newly refurbished choir opened in 1339 many misericords were left unfinished, including one-fifth of the surviving 65. Many of the clerics had not paid, having been called to contribute a total sum of £200. The misericords survived better than the other sections of the stalls, which during the Protestant Reformation had their canopies chopped off and galleries inserted above them. One misericord, showing a boy pulling a thorn from his foot, dates from the 17th century. In 1848 came a complete rearrangement of the choir furniture, and 61 of the misericords were reused in the restructured stalls.

 

The subject matter of the carvings of the central brackets as misericords varies, but many themes recur in different churches. Typically the themes are less unified or directly related to the Bible and Christian theology than small sculptures seen elsewhere within churches, such as bosses. This applies at Wells, where none of the misericord carvings is directly based on a Bible story. The subjects, chosen either by the woodcarver, or perhaps by the one paying for the stall, have no overriding theme. The sole unifying elements are the roundels on each side of the pictorial subject, which all show elaborately carved foliage, in most cases formal and stylised in the later Decorated manner, but with several examples of naturalistic foliage, including roses and bindweed. Many of the subjects carry traditional interpretations. The image of the "Pelican in her Piety" (believed to feed her young on her own blood) is a recognised symbol for Christ's love for the Church. A cat playing with a mouse may represent the Devil snaring a human soul. Other subjects illustrate popular fables or sayings such as "When the fox preaches, look to your geese". Many depict animals, some of which may symbolise a human vice or virtue, or an aspect of faith.

 

Twenty-seven of the carvings depict animals: rabbits, dogs, a puppy biting a cat, a ewe feeding a lamb, monkeys, lions, bats, and the Early Christian motif of two doves drinking from a ewer. Eighteen have mythological subjects, including mermaids, dragons and wyverns. Five are clearly narrative, such as the Fox and the Geese, and the story of Alexander the Great being raised to Heaven by griffins. There are three heads: a bishop in a mitre, an angel, and a woman wearing a veil over hair arranged in coils over each ear. Eleven carvings show human figures, among which are several of remarkable design, conceived by the artist specifically for their purpose of supporting a shelf. One figure lies beneath the seat, supporting the shelf with a cheek, a hand and a foot. Another sits in a contorted manner supporting the weight on his elbow, while a further figure squats with his knees wide apart and a strained look on his face.

 

Some of the cathedral's fittings and monuments are hundreds of years old. The brass lectern in the Lady Chapel dates from 1661 and has a moulded stand and foliate crest. In the north transept chapel is a 17th-century oak screen with columns, formerly used in cow stalls, with artisan Ionic capitals and cornice, set forward over the chest tomb of John Godelee. There is a bound oak chest from the 14th century, which was used to store the chapter seal and key documents. The bishop's throne dates from 1340, and has a panelled, canted front and stone doorway, and a deep nodding cusped ogee canopy above it, with three-stepped statue niches and pinnacles. The throne was restored by Anthony Salvin around 1850. Opposite the throne is a 19th-century octagonal pulpit on a coved base with panelled sides, and steps up from the north aisle. The round font in the south transept is from the former Saxon cathedral and has an arcade of round-headed arches, on a round plinth. The font cover was made in 1635 and is decorated with the heads of putti. The Chapel of St Martin is a memorial to every Somerset man who fell in World War I.

 

The monuments and tombs include Gisa, bishop; † 1088; William of Bitton, bishop; † 1274; William of March, bishop; † 1302; John Droxford; † 1329; John Godelee; † 1333; John Middleton, died †1350; Ralph of Shrewsbury, died †; John Harewell, bishop; † 1386; William Bykonyll; † c. 1448; John Bernard; † 1459; Thomas Beckington; † died 1464; John Gunthorpe; † 1498; John Still; † 1607; Robert Creighton; † 1672; Richard Kidder, bishop; † 1703; George Hooper, bishop; † 1727 and Arthur Harvey, bishop; † 1894.

 

In the north transept is Wells Cathedral clock, an astronomical clock from about 1325 believed to be by Peter Lightfoot, a monk of Glastonbury. Its mechanism, dated between 1386 and 1392, was replaced in the 19th century and the original moved to the Science Museum in London, where it still operates. It is the second oldest surviving clock in England after the Salisbury Cathedral clock.

 

The clock has its original medieval face. Apart from the time on a 24-hour dial, it shows the motion of the Sun and Moon, the phases of the Moon, and the time since the last new Moon. The astronomical dial presents a geocentric or pre-Copernican view, with the Sun and Moon revolving round a central fixed Earth, like that of the clock at Ottery St Mary. The quarters are chimed by a quarter jack: a small automaton known as Jack Blandifers, who hits two bells with hammers and two with his heels. At the striking of the clock, jousting knights appear above the clock face.

 

On the outer wall of the transept, opposite Vicars' Hall, is a second clock face of the same clock, placed there just over seventy years after the interior clock and driven by the same mechanism. The second clock face has two quarter jacks (which strike on the quarter-hour) in the form of knights in armour.

 

In 2010 the official clock-winder retired and was replaced by an electric mechanism.

 

The first record of an organ at this church dates from 1310. A smaller organ, probably for the Lady Chapel, was installed in 1415. In 1620 an organ built by Thomas Dallam was installed at a cost of £398 1s 5d.

 

The 1620 organ was destroyed by parliamentary soldiers in 1643. An organ built in 1662 was enlarged in 1786 and again in 1855. In 1909–1910 an organ was built by Harrison & Harrison of Durham, with the best parts of the old organ retained. It has been serviced by the same company ever since.

 

Since November 1996 the cathedral has also had a portable chamber organ, by the Scottish makers, Lammermuir. It is used regularly to accompany performances of Tudor and baroque music.

 

The first recorded organist of Wells was Walter Bagele (or Vageler) in 1416. The post of organist or assistant organist has been held by more than 60 people since. Peter Stanley Lyons was Master of Choristers at Wells Cathedral, and Director of Music at Wells Cathedral School in 1954–1960. The choral conductor James William Webb-Jones, father of Lyons's wife Bridget (whom he married in the cathedral), was Headmaster of Wells Cathedral School in 1955–1960. Malcolm Archer was the appointed Organist and Master of the Choristers from 1996 to 2004. Matthew Owens was the appointed organist from 2005 to 2019.

 

There has been a choir of boy choristers at Wells since 909. Currently there are 18 boy choristers and a similar number of girl choristers, aged from eight to fourteen. The Vicars Choral was formed in the 12th century and the sung liturgy provided by a traditional cathedral choir of men and boys until the formation of an additional choir of girls in 1994. The boys and girls sing alternately with the Vicars Choral and are educated at Wells Cathedral School.

 

The Vicars Choral currently number twelve men, of whom three are choral scholars. Since 1348 the College of Vicars had its own accommodation in a quadrangle converted in the early 15th century to form Vicar's Close. The Vicars Choral generally perform with the choristers, except on Wednesdays, when they sing alone, allowing them to present a different repertoire, in particular plainsong.

 

In December 2010 Wells Cathedral Choir was rated by Gramophone magazine as "the highest ranking choir with children in the world". It continues to provide music for the liturgy at Sunday and weekday services. The choir has made many recordings and toured frequently, including performances in Beijing and Hong Kong in 2012. Its repertoire ranges from the choral music of the Renaissance to recently commissioned works.

 

The Wells Cathedral Chamber Choir is a mixed adult choir of 25 members, formed in 1986 to sing at the midnight service on Christmas Eve, and invited to sing at several other special services. It now sings for about 30 services a year, when the Cathedral Choir is in recess or on tour, and spends one week a year singing as the "choir in residence" at another cathedral. Although primarily liturgical, the choir's repertoire includes other forms of music, as well as performances at engagements such as weddings and funerals.

 

The cathedral is home to Wells Cathedral Oratorio Society (WCOS), founded in 1896. With around 160 voices, the society gives three concerts a year under the direction of Matthew Owens, Organist and Master of the Choristers at the cathedral. Concerts are normally in early November, December (an annual performance of Handel's Messiah) and late March. It performs with a number of specialist orchestras including: Music for Awhile, Chameleon Arts and La Folia.

 

The bells at Wells Cathedral are the heaviest ring of ten bells in the world, the tenor bell (the 10th and largest), known as Harewell, weighing 56.25 long hundredweight (2,858 kg). They are hung for full-circle ringing in the English style of change ringing. These bells are now hung in the south-west tower, although some were originally hung in the central tower.

 

The library above the eastern cloister was built between 1430 and 1508. Its collection is in three parts: early documents housed in the Muniment Room; the collection predating 1800 housed in the Chained Library; and the post-1800 collection housed in the Reading Room. The chapter's earlier collection was destroyed during the Reformation, so that the present library consists chiefly of early printed books, rather than medieval manuscripts. The earlier books in the Chained Library number 2,800 volumes and give an indication of the variety of interests of the members of the cathedral chapter from the Reformation until 1800. The focus of the collection is predominantly theology, but there are volumes on science, medicine, exploration, and languages. Books of particular interest include Pliny's Natural History printed in 1472, an Atlas of the World by Abraham Ortelius, printed in 1606, and a set of the works by Aristotle that once belonged to Erasmus. The library is open to the public at appointed times in the summer and presents a small exhibition of documents and books.

 

Three early registers of the Dean and Chapter edited by W. H. B. Bird for the Historical Manuscripts Commissioners – Liber Albus I (White Book; R I), Liber Albus II (R III) and Liber Ruber (Red Book; R II, section i) – were published in 1907. They contain with some repetition, a cartulary of possessions of the cathedral, with grants of land back to the 8th century, well before hereditary surnames developed in England, and acts of the Dean and Chapter and surveys of their estates, mostly in Somerset.

 

Adjacent to the cathedral is a large lawned area, Cathedral Green, with three ancient gateways: Brown's Gatehouse, Penniless Porch and Chain Gate. On the green is the 12th-century Old Deanery, largely rebuilt in the late 15th century by Dean Gunthorpe and remodelled by Dean Bathurst in the late 17th century. No longer the dean's residence, it is used as diocesan offices.

 

To the south of the cathedral is the moated Bishop's Palace, begun about 1210 by Jocelin of Wells but dating mostly from the 1230s. In the 15th century Thomas Beckington added a north wing, now the bishop's residence. It was restored and extended by Benjamin Ferrey between 1846 and 1854.

 

To the north of the cathedral and connected to it by the Chain Gate is Vicars' Close, a street planned in the 14th century and claimed to be the oldest purely residential street in Europe, with all but one of its original buildings intact. Buildings in the close include the Vicars Hall and gateway at the south end, and the Vicars Chapel and Library at the north end.

 

The Liberty of St Andrew was the historic liberty and parish that encompassed the cathedral and surrounding lands closely associated with it.

 

The English painter J. M. W. Turner visited Wells in 1795, making sketches of the precinct and a water colour of the west front, now in the Tate gallery. Other artists whose paintings of the cathedral are in national collections are Albert Goodwin, John Syer and Ken Howard.

 

The cathedral served to inspire Ken Follett's 1989 novel The Pillars of the Earth and with a modified central tower, featured as the fictional Kingsbridge Cathedral at the end of the 2010 television adaptation of that novel. The interior of the cathedral was used for a 2007 Doctor Who episode, "The Lazarus Experiment", while the exterior shots were filmed at Southwark Cathedral.

 

An account of the damage to the cathedral during the Monmouth Rebellion is included in Arthur Conan Doyle's 1889 historical novel Micah Clarke.

 

The cathedral provided scenes for the 2019–2020 television series The Spanish Princess.

Doran of T1 at League of Legends Worlds 2025 Semifinal Features on October 27, 2025 in Shanghai, China. (Photo by David Lee/Riot Games)

Warner Bros Studio Tour London: The Making of Harry Potter

Warner Bros Studio, Aerodrome Way, Leavesden, Watford, Herts, WD25 7LS

 

A great day out for every fan of the boy wizard.

 

The Making of Harry Potter studio tour, covering 150,000 square foot, on two soundstages opened on the 31st March 2012, with stars galore at the red carpet launch at the Leavesden Studios where all eight movies were produced.

 

The home for many film productions, including several James Bond features, before a relatively new production company arrived there to make a film about a young boy who on his 11th birthday discovers he is a wizard.

 

Over the next ten years, the cast and crew of over 4,000 in total used more and more of the studios as the popularity of the books and films grew. The three young stars lived, grew up, went to school and turned into adults there on those stages.

 

Your tour begins in the foyer, with a flying Ford Anglia hanging from the ceiling and the walls adorned with huge photos of the cast, along with a few props.

 

Passing by the set of the cupboard under the stairs, you enter a room with a number of vertical TV screens showing Potter movie posters from around the world, followed by a short video sequence showing the rise of Harry’s popularity, the production teams discovery of the stories and the enormous worldwide success of the books and films.

 

Moving into the cinema, a short film introduced by Daniel Radcliffe, Emma Watson and Rupert Grint, talking about their experiences growing up on a film set for ten years, with clips from all eight films. The film ends with them standing in front of the main doors to the Great Hall and they walk in through the doors and invite you to follow them.

 

The screen at this point slowly rises to reveal the actual main doors to the Great Hall, surrounded with stone statues and carvings. What a wizard way to start the tour.

 

Walking through into the Great Hall we are told that we were now walking on the actual stone floor used in the films and seeing the actual tables where the actors ate their feasts. Dummies down each side of the hall wear the actual costumes used in the films. At the far end of the hall is the teachers’ table area, with more amazing costumes worn by Professors Dumbledore, Snape, McGonagall, Moody, Trelawney and Flitwick, as well as Hagrid and Filch too.

 

Leaving the Great Hall you enter the first of two vast sound stages. This includes sets for the Gryffindor Common Room and Dormitory, Dumbledore’s Office, Potions Classroom, Hagrid’s Hut, Burrow’s Kitchen and parts of the Ministry of Magic, also Umbridge’s gaudy pink, feline office. Each filled to the brim with props and costumes.

 

Props can be seen everywhere, with a massive cage in the centre, chock-a-block with goblets, chandeliers, wands and armour. A huge glass case contains the wands of 24 of the major characters – less than 1 percent of the total number of wands made for the films. The ornate doors to a Gringott’s vault and to the Chamber of Secrets are seen after passing a wall dedicated to the paintings produced to decorate the walls of Hogwarts.

 

Below the giant swinging pendulum of the Hogwarts castle clock there are several huge touch screens containing an interactive Marauders Map.

 

There are sections of the soundstage dedicated to various movie-making crafts. The hair and makeup section, costumes section, animal department, graphic design and production.

The final section in this first soundstage is dedicated to the Special Effects department with three huge video screens showing all the tricks and techniques, including greenscreen footage and CGI. Props attached to their motion rigs, include the Gringott’s Vault Cart and Mad-Eye Moody’s Recumbent Broomstick.

 

In separate room you can have a go on a broomstick or drive the Ford Anglia yourself, using the greenscreen technology.

 

The Backlot about half way round the tour is an open air section between the two soundstages where refreshments are available, including Butterbeer the popular wizarding beverage.

 

Also featured on the backlot are the Knight Bus, another Ford Anglia, Hagrid’s motorbike/sidecar, the Riddle family tombstone, a section of the rickety wooden Hogwarts Bridge, Potter’s burnt out cottage from Godric’s Hollow and Number 4 Privet Drive.

 

Entering the second soundstage you pass some of the giant chess pieces from the first movie. A number of video screens here progressively show what it was like to work in the creature shop, cleverly leading you from one screen to the next, past models of Fawkes, a snapping Monster Book of Monsters and a giant animatronic head of Hagrid. The next room has the life size (i.e., ENORMOUS!) model of Aragog the spider and one of three animatronic Buckbeak models.

 

Walking around the corner (WOW) you are transported into another world entirely. The dark lighting and cobbled street can only mean one thing – you have entered Diagon Alley. The shops using the original sets have been rebuilt– Flourish & Blotts, Eeylops Owl Emporium, Potage’s Cauldron Shop and of course Ollivander’s Wand Shop, each and every one them is crammed full of detail. At the other end of the street is Weasleys’ Wizard Wheezes, with the bright orange shopfront standing out from the crowd of blackness and featuring a moving model of one of the red-haired twins doffing his hat.

 

At the end of Diagon Alley you move onto the Art and Design department with walls covered with architectural drawings and detailed plans, accurate down to the millimetre, for many of the props and sets already seen. A draftsman’s table serves as a projection screen for another video about the work of the art department.

 

Moving on, up the ascending path are walls full of concept paintings and artwork, also intricate cardboard models of Hogsmead and the Hogwarts.

 

You are only looking at a model of the model though, as entering the next room, there, spread over at least 15 square metres is the most amazing, complex and elaborate model built to a 1:24 scale. It has a bigger footprint than the average house.

 

The last part of the tour is a fitting tribute to the crew and cast of the most popular film franchise of all time. A much tidier recreation of the interior of Ollivander’s Wand shop, with over 4,000 wand boxes lining its shelves – one for every single person who worked on the films.

 

Exit through the Gift Shop.

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