Great set of articles Lynn. My first Beehive was in 1964 or 65. I also wonder about the eruptive cycles on a basin wide basis. Look at the thermal output in 1996-1998, in particular 1997...what a summer that was. The same seems to be true in the early 1950's after a rather sluggish late 1940's. The 1960's also were quite active, much of that had to do with the 1959 earthquake that "shook" things up. The '70's as I recall seemed to be less active but by the early 1980's there again seemed to be an increase in overall activity. Look at today, without Giant, Giantess, Splendid, F&M (which seem to be slipping back into their cyclical dormancy we seem to be in a period of lower activity.) What causes these apparent cycles? Could this huge magma pool beneath our feet be "breathing"? With each inhale the magma rises, and with exhale it sinks? Just my silly mind wandering where it probably has no business going; my observations are only what I have noticed over the years. The actual facts in the written records would probably dispell my notions. John Warnock From: lstephens2006 at hotmail.com To: geysers at lists.wallawalla.edu Date: Thu, 25 Apr 2013 20:14:27 -0600 Subject: [Geysers] Geysers taken for granted THIS INFORMATION IS FOR THE PERSONAL USE OF THE READERS OF THIS LISTSERV AND IS NOT TO BE REPRODUCED FOR ANY OTHER PURPOSE, INCLUDING PUBLICATION IN THE SPUT: Someone posted on the old faithful webcam chat page: "Lynn's recent listserv discussion on Giantess intervals has lead me into thinking of geysers in terms of decades and centuries. Most of the big geysers have extended dormancies. And I started wondering what geysers we might be taking for granted today." Short answer: The only "major" geysers that don't seem to have periods of dormancy are Great Fountain, Old Faithful, and Riverside. Even some of the medium size geysers have had years of dormancy. I'm not going to try to give a complete answer but here are some items from Marler's Inventory about some of the dormancies. Beehive: In addition to summers in the past 25 years with days and even weeks between eruptions, here's some information about selected years from Marler--although he admitted there may have been additional eruptions he had not learned about, in 1954 he only found 8 eruption; 1961 9; 1962 5; 1963 3 and 1965 5. Castle: Here's what Marler said: Unlike Riverside's and Old Faithful's, Castle's function since discovery has been marked with periods of dormancy and variations in its patterns of play. If during its early known history there were any approach in regularity it was not recognized by observers before the 1940's. Available records indicate that during the past score of years Castle has not only erupted with greater frequency, but the pattern of its activity makes the eruptions predictable with reasonable accuracy. Daisy: Per Marler: During Daisy's known history its performance has ranged from great regularity, through great irregularity, to dormancy. I believe Marler's actions one year attempting to rejuvenate Daisy were viewed with displeasure by the Park Service. Fan & Mortar: Marler--"The scanty record of Fan and Mortar since the 1890s reveals long periods of dormancy." Fountain (and Morning) --(Maureen--don't cringe when you read this): Marler-- During part of 1899, and until late in the season Fountain was dormant due to its eruptive energy having shifted to a nearby spring. [the nearby spring was probably Morning.] During part of 1900's second decade Fountain was seldom observed erupting. Following the 1920s I know of no authentic record of an eruption of Fountain until the 1947 season. From the late 1930s until 1947 I am personally aware that none occurred. The cause of dwindling activity and then complete cessation is unknown. From 1947 to 1954 Fountain's eruptions continued to come as a sequence to eruptions of Morning and Clepsydra. None were known to be independent. See Rocco Paperiello's article in Transaction IV for more extensive history of Fountain (and Morning). Giant--See various Transactions articles and charts in The Sput for Giant's history. Giantess--See prior listserv post and there will be an article in the June issue of the Sput (unless I push the article off to a later issue. Genean has had an article on Beehive's Seasonality that I keep pushing off for various reasons.) Grand--Yes, it has had seasons of long intervals. Marler: From 1927 on through the 1930's and most of the 1940's there was a general increase in the length of Grand's intervals, with seasonal fluctuations. Between 1930 and 1947 the seasonal average ranged between about 20 and 44 hours; the extreme intervals being 12 and 120 hours. I think I've also read something about Marler's intervention with Vent/Turban/Grand. Lion: For example, Marler wrote: "Following the 1951 season the frequency with which Lion went into an active phase began to decrease. Seldom more than two active phases occurred during a week. By 1955 active phases were occurring not oftener than once a week. Sometimes eruptions [within the active phase] were over 3 hours apart. During the 1958 season eruptions were seldom observed, but they were frequent the previous winter." Even Sawmill has had years of dormancy or near dormancy. Marler: During 1963 it was in a state of near dormancy. But few eruptions were observed during that year. Surprisingly 1964 through 1966 witnessed a return to near pre-1963 activity. However, from mid-June 1967 for the remainder of the season Sawmill was dormant. At the beginning of the 1968 season conditions about the crater were indicative that the dormancy of 1967 had persisted through the following winter. Some rejuvenation occurred in late July 1968. However, it was mid-season in 1969 before any activity was observed. The frequency of the eruptions seemed to increase as the season progressed. I'm not even going to go into Big Cub, Excelsior, Lioness, Sapphire, Steamboat, Union, etc. Lynn Stephens _______________________________________________ Geysers mailing list Geysers at lists.wallawalla.edu -------------- next part -------------- An HTML attachment was scrubbed... URL: </geyser-list/attachments/20130429/5dd265fe/attachment.html>