Volcanic Springs

Geysers, Hot Springs,
Mud Pots, and Fumaroles

Norris Porcelain Basin - Features east of the central boardwalk to Pinwheel Geyser (II)

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At Sunday Geyser a branch of the boardwalk leads eastwards to the Porcelain Spings. It meets the ramp of the old trail after approximately one hundred yards. Features west of the ramp have been presented on the previous pages. So in the follwing features east of the ramp will be shown.

On the east side of the old ramp, at some distance to the boardwalk, the Primrose Springs form a cluster of inconspicuous hot springs. Primrose Spring (south), the largest among the cluster, is empty most oft the time. Eruptions of springs within the cluster are rare and reach only a few feet high.

The Primrose Springs:

Primrose Springs Yellowstone

Primrose Springs Yellowstone
East of the Primrose Springs and somewhat closer to the boardwalk a further typically clouded blue pool can be seen. It carries a funny but fitting name: Swiss Cheese Pool.

Swiss Cheese Pool:

Swiss Cheese Pool Yellowstone

Swiss Cheese Pool Yellowstone
A nameless, but attractive spring is embedded in the knolls a few feet northeast of Swiss Cheese Pool. Sometimes the spring shows weak eruptions.

Unnamed Spring northeast of Swiss Cheese Pool on July 13th, 2013:

Spring northeast of Swiss Cheese Pool Yellowstone

The adjacent Porcelain Springs occupy a flat area called Porcelain Terrace, bordered to the west, the south and the east by gently sloping hills. Structures within Porcelain Springs are changing very quickly because emitted hot water precipitates a lot of minerals in a short time. On the other hand the minerals together with thermophilic bacteria often generate fanciful deposites in gorgeous colors. Dying trees reveal the progress of hot ground on a comparison of stacked photos from 2013 (on top) and 2015 (beneath).

Porcelain Springs, western section in 2013 (roll mouse over picture to compare with 2015):

Porcelain Springs Yellowstone

Porcelain Springs Yellowstone
However, changes are not only becoming apparent in the quick growth of sinter, but also in terms of general activity. From the early 2000s up to 2011 the Porcelain Springs showed a low discharge rate, and the overall impression of the section was quite dull. This changed from the end of 2011 onwards, when hot, bluish water flooded extended areas again and brought back the extensive growth of colorful bacterial mats. There is a reason why the Porcelain Springs and all the way to the Primrose Springs are differing so much in terms of colorfulness from the reast of Porcelain Basin. They are an enclave of alkaline conditions within an acidic surrounding.

Porcelain Springs, eastern section:

Porcelain Springs Yellowstone

Porcelain Springs
Two informally named geysers are located within the Porcelain Springs, Lambchop Geyser and Incline Geyser. Lambchop Geyser is sometimes acting as a forceful steam vent, sometimes as geyser.

Lambchop Geyser in 2013, steam phase:

Lambchop Geyser Yellowstone

Lambchop Geyser

Lambchop Geyser in 2015, water phase:

Lambchop Geyser Yellowstone

Lambchop Geyser
At the time of its development in the early 1990s, Incline Geyser underwent some of the largest eruptions ever seen in Porcelain Basin. But then it fell dormant and used to be only a jagged crater, partially filled with water. New activity started at the end of 2011, when the water level rose and the previously weak spouting activity increased at different spots. The freshly precipitated sinter together with the pale blue water make a grateful object for photographers.

Incline Geyser in 2013:

Incline Geyser Yellowstone

Incline Geyser

Spouters around Incline Geyser in 2015:

Incline Geyser Yellowstone

Incline Geyser
Only few visitors take time to look out for the numerous geysers and perpetual spouters on the flat further beyond the Porcelain Springs. Even when these features usually do only exist for a short period of time, some of them are in terms of colors, frequency, or height of eruptions in no way inferior to other, far more prominent geysers. But the distance from the trail and steam do often impede the view. Follow the link "Unnamed geysers on the flat of Norris Porcelain Basin" or proceed to page 5 to find a selection of noteworthy features.
Far out on the sinter flat the small Iris Spring and Blue Geyser are rare examples of features with a continuance over many decades. Both are mostly active during a disturbance. Prior to 1933 Iris Spring carried the name Apple Green Geyser for some time.

Iris Spring on the left next to Blue Geyser on the right hand side:

Iris Spring and Blue Geyser Yellowstone

Iris Spring and Blue Geyser Yellowstone

Iris Spring erupting on August 16th, 2017:

Iris Spring Yellowstone

Iris Spring Yellowstone
The northeast end of Porcelain Basin is marked by a range of low hills. On the slopes and on top of the hills further geysers and hot springs are to be found. A large bluish clouded pool, featuring a cave with a collapsed roof at its far side, is most eye-catching among them. The marginally visible spring is much larger than it appears, approximately as extended as Scummy Pool. The appearance of a collapsed cave could lead to a confusion with Collapsed Cave Geyser, but that one lies actually on the slope beyond it and can not be spotted from the boardwalk (many thanks to Byron Taylor for the clarification). Eruptions of Collapsed Cave Geyser may be noticed as forceful steam emissions only.

Pool with collapsed cave:

Pool with collapsed cave

Collapsed Cave Geyser
With the help of binoculars it is possible to observe geyser activity even at the remote northeast corner of Porcelain Basin. At least three unnamed geysers are active in this region.

Geysers at northeast corner of Porcelain Basin:

Geysers at northeast corner of Porcelain Basin Yellowstone

Across the boardwalk from the Porcelain Springs trees largely obscure the view in a southward direction. Some hot springs are located among or behind the trees, for example NPBNN022.

Hot spring NPBNN022:

Hot spring NPBNN022 Yellowstone

A branch of the boardwalk leads through this southern area back to Norris Museum. The first feature to the left hand side is Congress Pool, an acidic geyser more noticeable because of its strongly changing water level than the height or frequency of eruptions. Its name refers to the 5th International Geological Congress held 1891 in Yellowstone. The most interesting secret of Congress Pool is not readily visible. Microbiologists detected a community of the hydrogen sulfide oxidizing archaeon Sulfolobus acidocaldarius in Congress Pool, which is parasitized by viruses nobody ever found before. Moreover, Congress Pool is one of a few acidic hot springs in Yellowstone where in the early 1970s Thomas D. Brock collected the samples which let him discover Sulfolobus itself.

Congress Pool at low water level:

Congress Pool Yellowstone

Congress Pool
Both beyond Congress Pool and on its south side, even on the slope, further hot springs are to be found. Some of them carry names such as Locomotive Spring, Vermillion Spring "Red Vent" and Vermillion Spring "White Vent". What they all have in common are water levels not visible from the boardwalk. An exception regarding visibility is the artificial Carnegy Drill Hole from 1929. It can be spotted as a steaming, sometimes also splashing pile of cemented rocks far beyond Congress Pool. Another unnamed, small pool next to the trail is shown on the next photo.

Unnamed pool southwest of Congress Pool:

Pool southwest of Congress Pool Yellowstone

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