Ellsworth American COUNTY Dunham’S Hotel

Total Page:16

File Type:pdf, Size:1020Kb

Ellsworth American COUNTY Dunham’S Hotel Sbfcntfennmt*. Rsed, of Kllsworth, and Mrs. Annie 'Itjfnrtiacmmis. _ v- LOCAL AFFAIRS. Powers, of Bangor. Mrs. Higgins had friends in Ellsworth who NEW AI1VKUTIM M ENT* THIS WEEK. many regret C. 0. RURRILL & deeply to hear of her death. She visited SON, state assessor**’ notice. here about two *■* I‘s ('omtnissiiiu of fi-h and fisheries—Sealed years ago. ^ 1 proposals. The Mutual Life Insurance Co., of New Hancork lmll— M urrDon ( omeily « «>. m j of m qenekal INSURANCE Robert It H" in. < *<ut *\ culture *»ale- York, *, |Kent, of this city, j AGENTS, I’anook Is a speciafagent, has paid through Mr. Hi him Bank Bldg., ELLSWORTH, ME. Tyler, Fogg A « •»—Municipal bonds. Kent the policy of |15,0CK) on the life of ^ Rockland, My the late W. it. Blaisdell, of Franklin. ARSOL«JT.F*v 'piJRE Rockland Cumin* rc’.al < *•!!* ;<■. WE REPRESENT THE This is one of the largest policies of life \ A '•:iimri)1 '* > in«u1 me v; paid in this vicinity. Makes the food more de'icious and v 'v '. sew Most Kciiiihle Home ami Foreign Coni pan it's. Curtis Novelty < <>— Agent wanted George W. Davis, of Boston, formerly J'■■//> a ih/r V'i/h ! ■■■■■■■BHanannaHDunaniaaBHBaMHManiir^nMnnnnHr «ommJ9 L Safi )J. of this a brother of 10. Davis, t'nvijmt Far othrr focal news see pages •/, .7 and S. city, Henry lias purchased the Tontine house at Miss Mari* *i of Auburndaln, In sums to Hu it on real c.si ate and Morgan, Unitarian noinc. improved Brunswick. The Tontine is a popular re- of the engine had passed over the boy’s Conference at MON KY TO LOAN J is the guest of Miss Mabel —--- collateral.- ... MafiH., .joy. it off at ankle and The annual session be Han- sort for travelling men, and as Mr. Davis leg, cutting the badly eighth Miss Be tie Bnd are vis- the bones above the ankle. cock conferenee of l .an Had Joy Harry Joy has hjmself been on the road for many mangling county iting their Mrs. F. W. Stanton, in The was below the Christian churches ill he held sister, years, both host and hostelry are likely to leg amputated juBt pother Boston. * be popular. knee. with the Lamoine church on MV; day and THERE’S NO ARTICLE E. K. and wife drove to Ells- The State tish and commissioners Wednesday, Aug. 1 and 2. Hopkins James S. Reynolds, an honest and in- game On ho a worth from Brooklin a house Tuesday evening at 6.30 the opening at small Saturday, returning dustrious citizen of Elllsworth, died held hearing at' the American on the sermon of the conference will h Jven by Sunday. Tuesday, aged fifty-eight years. The de- last Wednesday evening petition of Ellsworth to close the Rev. A. L. Hudson, of Buffalo, in the FURNITURE .... M iss Sadie W. Burrill has returned from ceased was a native of Kllsworth, a son of sportsmen OF church at East Lamoine. Th° exerciser a visit f three weeks with friends in the 1h'< Nathaniel C. Reynolds, and all streams flowing Into Branch pond. The on at 1 * of was to a to Wednesday will begin o’clock, Montreal. his life had been spent here. He was a object the petitioii put stop the of small salmon which run and will be held at Shore L el, Kov. C. F. of Jamaica Mast* vetc;n of the civil war. An aged mother catching Dole, Plain, Lamoine Point. up the streams from the pond. The will preach at the Unitarian church survives him. small salmon bite voraciously, and un- Rev. Charle F. 1 ok, c? Jr- P; n, BELGIAN COUCHES. Sunday morning. R. B. Holmes, proprietor of the West conscionable fishermen have taken hun- will speak on “Religion f Men and The schooner “Samuel Lewis” came off End furniture store, announces that lie dreds of salmon from Hix to eight inches Boys”. Other speakers are .. C. C. the marine railway last week, and the is about to retire from the business. long from the streams. There were two Everett, D. D., Rev. H. A. Eli Rev. S. C. * went on. Some years ago Mr. Holmes gave up the “Victory” remonstrants at the hearing before the Bench, and Rev. T. C. Perkin Tin are made of well-seasoned and fruit and confectionery business because y substantially wood, highly finished, Mr. and Mrs. Charles Knox, of Chester, commissioners. asked that certain Lamoine will be reached boat leav- the indoor work too They by A few we are proved confining, are upholstered in Velour of handsome patterns. days ago bought Mass., visiting Mrs. Knox’s parents, brooks up which the salmon did not run, ing Bar Harbor daily at 5.15 p. m.. and on I and his present change is to be made for Calvin P. and wife. were b at '• a us to offer these Joy but from which only trout caught Wednesday by special .ng Bar tin1 entire stock *>f Boston dealer, and this enables high- the same reason. Mr-J. J. i\ Simon!on ;s much mocc com- be left open. The commissioners voted Harbor about 9.20 a. m. P * will re- at the nominal of of grade couches price Rev. N. H. Whittlesey, D. D., New < fortable thi~* week, and her friends are to close Winkutnpaw, Gotta, and Rocky j turn to Bar Harbor after th>- ercih*s. II,. the committee n, Conn., secretary of Rond and to that effect A dinner will be st : at t ue more hopeful of her recovery. brooks, notices picnic of the national council of ministerial re- will be at once. I hotel noon free to who at- C. \V. Bobbins, editor of the Oldtown posted Wednesday lief for the Congregational churches, tend the conference. A cord.-b invita- $5.50. Enterprise, was in town last week and | in the I spoke Sunday morning Congrega- “J IIK tion is extended to all to attend. made The American a call. BLUFFS.” pleasant tionnl church. He made an earnest ap- one to a customer. At Hancock Furniture Store. ^ Only County's Largest Miss Margaret H. the Hayes, competent peal for contributions for the ministerial Ellsworth Men Negotiating for Pur- jjinancial. and faithful in The Ameri- book-keeper relief fund, making it appear as a duty chase of Hotel at Mt. Desert Ferry. can is her annual vaca- ••••••» i« • ••• •: office, enjoying rather than a charity. E. H. Oeely. of Ellsworth, representing tion. The MethodiHt and Bantist r Ellsworth and Bar •) -C • A. W. CUSHMAN & SON, Sunday numher of Harbor CL d-i ^4-~7 Harvey W. Bowie*, of Bangor, formerly schools are arranging for their unnunl ex- is for the pur- gentlemen, negotiating ; Jciiciy^ of Ellsworth, was married yesterday. cursion lo Newbury Neck by schooner chase of the hotel, “The Bluffs,” at Mt. (• ») Cor. Main and Franklin Stn., Ellsworth. C) is the most import ;feature '• 1 lie bruit* v. us m iss iselle A. Merrill, or and The will be made next Desert It was an- tug. trip Ferry. prematurely <• ol an invcslmeut. *) Bangor. Tuesday, Aug. 1, if a suitable vessel can be nounced last week that the sale had been Miss Lizzie M. Osgood it ft Tuesday for obtained. It is probable that a number of closed. i Borh I* MunicipalX 9) Cottage City, Vineyard llaven, where she Cninn river yachts will go down the bay Mr. Greely said yesterday that the CLOTHING had been a are safer than alm< t any form MIDSUMMER will be the remainder of the slight en.j toyed negotiations delayed by of investment, a: ''.l fair » the < .it of the school ex- hitch in the title. He 0, now demand No better stock in Ellsworth summer. .joyok Sunday thought, however, in in greatest <• interest returns. •) cursionists. that it w ould not a serious obstacle, to select from. Mr. and Mrs. Charles E. Lynch, of prove and that the hotel would soou change West Somerville, Mass., are vi iting rela- At an adjourned parish meeting of the hands. LIGHT-WEIGHT SUITS. tives and friends in this c.iy, thoir for- C'u;.i;:egHtionai society held last Saturday Y fOGG & GO. the matter of a was It is the purpose of the prospective pro- ?;T LE.s, mer home. parsonage | evening, to continue The Bluffs as a first LIGHT-WEIGHT UNDERWEAR. further discussed. After long delibera- prietors « » Col. Joseph W. Porter, of Bangor, was IVi. class summer hotel. Extensive BANGOR, tion it was voted to build, and to place improve- • in Ellsworth Monday. Col. Porter is • • 0 • • • i • 3 • 9 • • * « ?. 5 *y LIGHT-WEIGHT HOSIERY. the matter in the hands of a ments will be made. The hotel com- familiar to Bangor Commercial readers as absolutely committee of three. A committee of live mands one of the finest views to be f und And everything else that will tend to add ease and com- Wayfarer”. \\u chosen to select this committee of along the coast of Maine. fort to the hot spell. Miss Alice Haslem, whose serious illness a BARROWS & three. At this writing the latter com- The hotel was erected in 1885 by stock BLAKE, BROWN, was is now _ reported last week, critically It mittee has not been chosen. company, and cost about £11,000. has, BANGOR, ME. ill. Her little en- physician gives very with the two adjacent cottages belonging ■e Morrison comedy company is couragement. to the property, about sixty-five guest- OWEN BYRN, booked to appear in Hancock hall for the Senator ant| Mrs. McMillan, of Michi- rooms, and there are dining entire week 31.
Recommended publications
  • 61 Pleistocene Lake Mojave Stratigraphy And
    HISTORY, PROCBSS, AND TRADITION: it SYMPOSIUM FOR MAKOTO KOnA 61 PLEISTOCENE LAKE MOJAVE STRATIGRAPHY AND ASSOCIATED CULTURAL MATERIAL CLAUDE N. WARREN AND JOAN S. SCHNEIDER The problems of geoarchaeology addressed in this paper were probably most clearly stated very early in the research, almost 40 years ago (Warren and DeCosta 1964). To adequately date the artifact assemblages from the 24 "surface sites" on the high beach lines of Pluvial Lake Mojave, two tasks must be successfully completed: (1) construct the geomorphic history of Lake Mojave from the strafigraphy, topographic re/afionships, radiocarbon dates, and any other useful data, and (2) demonstrate the stratigraphic relationship between prehistoric artifacts and lacustrine deposits of Lake Mojave. These two tasks are addressed in this paper, demonstrating the sequence of beach-ridge INTRODUCTION formation at Lake Mojave (Antevs 1937; Ore and Warren 1971; Wells et al. 1989). Additional data The Mojave River periodically flowed into from other locations within the range of elevations Death Valley during the late Pleistocene and early of the high beach ridges are integrated with Holocene. On its way to Death Valley, it filled observations made at the EI Capitan Beach the basins of today's Silver and Soda playas to Complex. overflow levels, forming Pleistocene (and early Holocene) Lake Mojave (Map 1). The final Within the uppermost portion of the Lake overflow stage of Pleistocene Lake Mojave was Mojave Basin are three high beach ridges referred probably about 9,000 years ago. With the to as BRI, BRII, and BRIll. These are the most increasing aridity of the early Holocene, the flow extensive shoreline features formed by the early of the Mojave River decreased, and by 7,500 years high stands of Lake Mojave.
    [Show full text]
  • MAPPING and CHARACTERIZING a RELICT LACUSTRINE DELTA in CENTRAL LOWER MICHIGAN by Christopher B. Connallon a THESIS Submitted T
    MAPPING AND CHARACTERIZING A RELICT LACUSTRINE DELTA IN CENTRAL LOWER MICHIGAN By Christopher B. Connallon A THESIS Submitted to Michigan State University in partial fulfillment of the requirements for the degree of Geography – Master of Science 2015 ABSTRACT MAPPING AND CHARACTERIZING A RELICT LACUSTRINE DELTA IN CENTRAL LOWER MICHIGAN By Christopher B. Connallon This research focuses on, mapping and characterizing the Chippewa River delta - a sandy, relict delta of Glacial Lake Saginaw in central Lower Michigan. The delta was first identified in a GIS, using digital soil data, as the sandy soils of the delta stand in contrast to the loamier soils of the lake plain. I determined the textural properties of the delta sediment from 142 parent material samples at ≈1.5 m depth. The data were analyzed in a GIS to identify textural trends across the delta. Data from 3276 water well logs across the delta, and from 185 sites within two-storied soils on the delta margin, were used to estimate the thickness of delta sands and to refine the delta's boundary. The delta heads near Mount Pleasant, expanding east, onto the Lake Saginaw plain. It is ≈18 km wide and ≈38 km long and comprised almost entirely of sandy sediment. As expected, delta sands generally thin away from the head, where sediments are ≈4-7m thick. In the eastern, lower portion of the delta, sediments are considerably thinner (≈<1-2m). The texturally coarsest parts of the delta are generally coincident with former shorezones. The thick, upper delta portion is generally coincident with the relict shorelines of Lakes Saginaw and Arkona (≈17.1k to ≈ 16k years BP), whereas most of the thin, distal, lower delta is generally associated with Lake Warren (≈15k years BP).
    [Show full text]
  • Table of Contents. Letter of Transmittal. Officers 1910
    TWELFTH REPORT OFFICERS 1910-1911. OF President, F. G. NOVY, Ann Arbor. THE MICHIGAN ACADEMY OF SCIENCE Secretary-Treasurer, GEO. D. SHAFER, East Lansing. Librarian, A. G. RUTHVEN, Ann Arbor. CONTAINING AN ACCOUNT OF THE ANNUAL MEETING VICE-PRESIDENTS. HELD AT Agriculture, CHARLES E. MARSHALL, East Lansing. Geography and Geology, W. H. SHERZER, Ypsilanti. ANN ARBOR, MARCH 31, APRIL 1 AND 2, 1910. Zoology, A. S. PEARSE, Ann Arbor. Botany, C. H. KAUFFMAN, Ann Arbor. PREPARED UNDER THE DIRECTION OF THE Sanitary and Medical Science, GUY KIEFER, Detroit. COUNCIL Economics, H. S. SMALLEY, Ann Arbor. BY PAST-PRESIDENTS. GEO. D. SHAFER DR. W. J. BEAL, East Lansing. Professor W. H. SHERZER, Ypsilanti. BRYANT WALKER, ESQ. Detroit. BY AUTHORITY Professor V. M. SPALDING, Tucson, Arizona. LANSING, MICHIGAN DR. HENRY B. BAKER, Holland. WYNKOOP HALLENBECK CRAWFORD CO., STATE PRINTERS Professor JACOB REIGHARD, Ann Arbor. 1910 Professor CHARLES E. BARR, Albion. Professor V. C. VAUGHAN, Ann Arbor. Professor F. C. NEWCOMBE, Ann Arbor. TABLE OF CONTENTS. DR. A. C. LANE, Tuft's College, Mass. Professor W. B. BARROWS, East Lansing. DR. J. B. POLLOCK, Ann Arbor. Letter of Transmittal .......................................................... 1 Professor M. H. W. JEFFERSON, Ypsilanti. DR. CHARLES E. MARSHALL, East Lansing. Officers for 1910-1911. ..................................................... 1 Professor FRANK LEVERETT, Ann Arbor. Life of William Smith Sayer. .............................................. 1 COUNCIL. Life of Charles Fay Wheeler.............................................. 2 The Council is composed of the above named officers Papers published in this report: and all Resident Past-Presidents. President's Address—Outline of the History of the Great Lakes, Frank Leverett.......................................... 3 On the Glacial Origin of the Huronian Rocks of WILLIAM SMITH SAYER.
    [Show full text]
  • Quagga Mussels Threaten Western U.S. Waters, Researcher Reports 1 July 2008
    Quagga mussels threaten western U.S. waters, researcher reports 1 July 2008 and are out-competing zebra mussels, O'Neill told the House committee. Last year, quaggas were discovered for the first time in the West in Nevada's Lake Mead and have since been found down the Colorado River in Lake Mojave, Lake Havasu and in various locations in California. "[The spread west] is not a surprise," said O'Neill. "It's something that's been expected to happen." Both quagga and zebra mussels originated in Eurasia in the Caspian, Ural and Baltic seas and spread to the United States in ballast water from Both quagga, pictured, and zebra mussels originated in freighters. Eurasia in the Caspian, Ural and Baltic seas and spread to the United States in ballast water from freighters. Zebra mussels filter food as small as 15 microns Credit: Natalie Muth, Utah Division of Wildlife Resources (the size of a mold spore); quagga mussels can feed on even smaller bacteria and out-compete their relatives. In both species, mature females produce up to one million eggs at a time that turn Pipe-clogging invasive mussels caused up to $1.5 into free-swimming larvae called veligers. Two to billion in damage across 23 states between 1989 five weeks after hatching, veligers become too and 2007. Now, fingernail-sized quagga mussels, a heavy to float and search for hard surfaces to close relative of zebra mussels, have spread to the attach themselves. Water-intake pipes and similar West and threaten to do even more damage. structures offer ideal habitat for their colonization because the continuous flow of water provides The threat was outlined by Chuck O'Neill, a senior steady food and oxygen and carries away waste; extension associate with Cornell and New York the structures protect the veligers against Sea Grant, in testimony before the U.S.
    [Show full text]
  • Great Lakes Region, USA
    Spatial variation in till texture and clay mineralogy across the Saginaw Lobe terrain, Great Lakes region, USA Department of Geography, Environment and Spatial Sciences, Randall J. Schaetzl, Chris Baish, Jarrod Knauff, Thomas Bilintoh, East Lansing, Michigan, USA Dan Wanyama, Kevin McKeehan, and Michelle Church Abstract STUDY AREA SAMPLE DISTRIBUTION Great Lakes region We present a spatial/mapping approach to the study of the glacial history of the Saginaw lobe of the Laurentide Ice Sheet. The Saginaw Lobe flowed into southern Michigan, USA, forming modern-day Saginaw Bay and leaving behind a series of small moraines in down- ice locations. Upon its retreat – and likely also during its advance – a large proglacial lake (Glacial Lake Saginaw) formed in the northeastern margins of the “Saginaw terrain”. The Saginaw lobe advanced to the southwest, out of this lake basin and onto thinly mantled, sandstone and shale bedrock. Although the Late Pleistocene deglacial chronology of this lobe has been generally assumed for decades, few numerical ages exist that could help constrain a better defined timeline. Indeed, as luminescence ages slowly emerge for terrain of the Saginaw Lobe and nearby areas, it seems clear that the lobe retreated from the region considerably earlier than is generally assumed, adding to the potential for large areas of ponded water in proglacial settings, all of which are as yet unmapped. In this project, we sampled tills on uplands across the terrain of the Saginaw Lobe, avoiding outwash plains. In all, we obtained 334 samples of calcareous till, by bucket auger. Sample locations were sited generally uniformly across >20,000 km2.
    [Show full text]
  • 2008 Trough to Trough
    Trough to trough The Colorado River and the Salton Sea Robert E. Reynolds, editor The Salton Sea, 1906 Trough to trough—the field trip guide Robert E. Reynolds, George T. Jefferson, and David K. Lynch Proceedings of the 2008 Desert Symposium Robert E. Reynolds, compiler California State University, Desert Studies Consortium and LSA Associates, Inc. April 2008 Front cover: Cibola Wash. R.E. Reynolds photograph. Back cover: the Bouse Guys on the hunt for ancient lakes. From left: Keith Howard, USGS emeritus; Robert Reynolds, LSA Associates; Phil Pearthree, Arizona Geological Survey; and Daniel Malmon, USGS. Photo courtesy Keith Howard. 2 2008 Desert Symposium Table of Contents Trough to trough: the 2009 Desert Symposium Field Trip ....................................................................................5 Robert E. Reynolds The vegetation of the Mojave and Colorado deserts .....................................................................................................................31 Leah Gardner Southern California vanadate occurrences and vanadium minerals .....................................................................................39 Paul M. Adams The Iron Hat (Ironclad) ore deposits, Marble Mountains, San Bernardino County, California ..................................44 Bruce W. Bridenbecker Possible Bouse Formation in the Bristol Lake basin, California ................................................................................................48 Robert E. Reynolds, David M. Miller, and Jordon Bright Review
    [Show full text]
  • North Ridge Scenic Byway Geology
    GUIDE TO THE NORTH RIDGE SCENIC BYWAY GEOLOGY LANDFORMS The North Ridge Scenic Byway corridor lies in the Erie Lake Plain landform of the Central Lowlands Physiographic Province of the United States (Fenneman 1938; Brockman 2002). The Lake Plain consists of wide expanses of level or nearly level land interrupted only by sandy ridges that are remnants of glacial-lake beaches and by river valleys carved into Paleozoic bedrock. With the exception of the sandy ridges, much of the Lake Plain in Avon and Sheffeld was a dense swamp forest prior to settlement. The North Ridge Scenic Byway follows the northernmost ancient beach ridge as it traverses Sheffeld and Avon at an elevation ranging from 675 to 690 feet above sea level, some 105 to 120 feet above modern Lake Erie. Topography of Sheffeld and Avon Townships as surveyed in 1901, showing North Ridge near the center of the map (courtesy of U.S. Geological Survey, Oberlin, Ohio Quadrangle 1903). 2 GEOLOGY FORMATION OF NORTH RIDGE Approximately 18,000 years ago, the last The chronology of lake stages in the Lake continental glacier blanketed northern Ohio as Erie basin relates a fascinating story of glacial it pushed down from the north to its maximum action, movements of the earth’s crust and southern thrust. The ice sheet reached as far erosion by waves to form the body of water south as Cincinnati, Ohio, then it began to we see today. The story begins nearly 15,000 melt back. As the glacier paused in its retreat, years ago as the last glacier [known as the piles of rock and clay debris [known as end Wisconsinan ice sheet] temporarily halted to moraines] were built up at the ice margins.
    [Show full text]
  • The Clinton Independent,A^M HANDSOME Dtepiar of Pattern
    BOTCHER k PETNCITS OPENING of Fall and Winter Millinery Will Occur FRIDAY AND 8ATCRDAT. SEPTEMBER 27 and 28. T'HK iiu»l and new—I nor*In ^m HANDSOME dtepiar of Pattern (n Era1 1—i Fall aad Winter M Htl per feet g en -will a* *x- A Sthlted at <Mtr o—um Frt4«> •n mat now be mmintoeri and ftatepirar. Srpt *1 aad ». A —e- vitatlun to love— of art aad HOUCHIB * I»BTSCU Laeaiy- The Clinton Independent, UOUCHKB * PI VOL XXIX.—NO. #0 ST. JOHNS, MICH.. FRIDAY MORNING, SEPTEMBER 27. 18»5. WHOLE NO.—1510. New Advertisement*. — Mrs. Henry Mulder is confined to -Ninety-six tickets were sold at this —Official board meeting at M. E. This Wm* Only. Vtelt Oar *t»r* her home by sickuees. station for the excursion to Detroit laat church tomorrow evening. During the week of the Fair we will We extend to you a cordial invitation MercautHe Oo.— Dry Gnoda. Uromrtm aad Sunday. offer some special bargains to aash buy­ to visit (Mir store during the week of the Boots aad Shorn. —Geo. K. Horry, St. Johns, has been —Eugenie Fern in the latest society granted an increase of pension. —Judge Daboll will deliver an address dramas, at Seriven's Opera House all ers. Here are the inducements : fair—next week. Jokn HIckt-biT Oooda, Cloaks. Carpets. One gent ’s open faee gold filled watch Our trimmers are making ready a fine Wilson A Son—Clot i>ln«. —It i» reported that Earnest, son of at the Gratiot county fair, to-day .
    [Show full text]
  • Geology of Michigan and the Great Lakes
    35133_Geo_Michigan_Cover.qxd 11/13/07 10:26 AM Page 1 “The Geology of Michigan and the Great Lakes” is written to augment any introductory earth science, environmental geology, geologic, or geographic course offering, and is designed to introduce students in Michigan and the Great Lakes to important regional geologic concepts and events. Although Michigan’s geologic past spans the Precambrian through the Holocene, much of the rock record, Pennsylvanian through Pliocene, is miss- ing. Glacial events during the Pleistocene removed these rocks. However, these same glacial events left behind a rich legacy of surficial deposits, various landscape features, lakes, and rivers. Michigan is one of the most scenic states in the nation, providing numerous recre- ational opportunities to inhabitants and visitors alike. Geology of the region has also played an important, and often controlling, role in the pattern of settlement and ongoing economic development of the state. Vital resources such as iron ore, copper, gypsum, salt, oil, and gas have greatly contributed to Michigan’s growth and industrial might. Ample supplies of high-quality water support a vibrant population and strong industrial base throughout the Great Lakes region. These water supplies are now becoming increasingly important in light of modern economic growth and population demands. This text introduces the student to the geology of Michigan and the Great Lakes region. It begins with the Precambrian basement terrains as they relate to plate tectonic events. It describes Paleozoic clastic and carbonate rocks, restricted basin salts, and Niagaran pinnacle reefs. Quaternary glacial events and the development of today’s modern landscapes are also discussed.
    [Show full text]
  • Is There Any Evidence of Mega-Lake Manly in the Eastern Mojave Desert During Oxygen Isotope Stage 5E/6?
    Quaternary Research 57, 177–179 (2002) doi:10.1006/qres.2001.2299, available online at http://www.idealibrary.com on REPLY Is There Any Evidence of Mega-Lake Manly in the Eastern Mojave Desert during Oxygen Isotope Stage 5e/6? I am pleased to have the opportunity to defend and clarify the implication that Ku’s dates are more reliable than those of my hypothesis regarding the extent of the Blackwelder stand of Hooke and Lively (see Hooke and Dorn, 1992) is debatable, Lake Manly during marine oxygen isotope stage 6 (OS6). Let given that both use the -counting technique and thus may suffer me start by addressing a couple of general points. from problems with U migration. First, with reference to the pejorative prefix “mega” in Enzel Salt Spring Hills shoreline. Enzel et al. maintain that this et al.’s comment, let me put the size of the lake under discussion shoreline is cut into colluvium and, at its southeastern end, into in perspective. If water were to fill Death Valley to the 90-m alluvial fan deposits. I agree with the former. On the other hand, level today, the surface area would be 1600 km2 (Meek, 1997), air photos, a map in Anderson and Wells (1997), and my own whereas the area Hale proposed, based on overflow at Ash Hill observations do not support the interpretation that it is cut into an pass, would have been 8000 km2 (Hale, 1985). The surface alluvial fan at its southeastern end. Even if further study shows area of the OS6 lake proposed in my paper is 2800 km2, less that it is, however, Enzel et al.’s statements about the age of than half the size of Hale’s lake and less than twice the size a the fan unit are misleading (1) because they are based on dates 90-m lake would have were it to occupy the valley today.
    [Show full text]
  • Evaluation of Quagga Mussel Veliger Thermal Tolerance
    EVALUATION OF QUAGGA MUSSEL VELIGER THERMAL TOLERANCE FINAL REPORT – JANUARY 2011 RESEARCH SESSION July 2011 Prepared for: Colorado Division of Wildlife Aquatic Wildlife Research Group Aquatic Section Fort Collins Research Center Invasive Species Program 317 W. Prospect St. 6060 Broadway Fort Collins, CO 80526 Denver, Colorado 80216 Prepared by: Christopher D. Craft and Christopher A. Myrick, Ph.D. Department of Fish, Wildlife, and Conservation Biology Colorado State University Fort Collins, Colorado 80523-1474 (970) 491-5657 CDOW Task Order # CSU1003 CSU Number 53-0555 Table of Contents Table of Contents ............................................................................................................................. 2 Introduction ..................................................................................................................................... 3 Materials and Methods .................................................................................................................... 6 Veliger Collection ........................................................................................................................ 6 Veliger Holding System .............................................................................................................. 6 Veliger Thermal Tolerance Testing ............................................................................................. 7 Statistical Analyses .....................................................................................................................
    [Show full text]
  • The Pueblo in the Mojave Sink: an Archaeological Myth
    California State University, San Bernardino CSUSB ScholarWorks Theses Digitization Project John M. Pfau Library 2002 The pueblo in the Mojave Sink: An archaeological myth Barbara Ann Loren-Webb Follow this and additional works at: https://scholarworks.lib.csusb.edu/etd-project Part of the Archaeological Anthropology Commons Recommended Citation Loren-Webb, Barbara Ann, "The pueblo in the Mojave Sink: An archaeological myth" (2002). Theses Digitization Project. 2107. https://scholarworks.lib.csusb.edu/etd-project/2107 This Thesis is brought to you for free and open access by the John M. Pfau Library at CSUSB ScholarWorks. It has been accepted for inclusion in Theses Digitization Project by an authorized administrator of CSUSB ScholarWorks. For more information, please contact [email protected]. THE PUEBLO IN THE MOJAVE SINK: AN ARCHAEOLOGICAL MYTH A Thesis Presented to the Faculty of California State University, San Bernardino In Partial Fulfillment of the Requirements for the Degree Masters of Arts in Interdisciplinary Studies by Barbara Ann Loren-Webb March 2003 THE PUEBLO IN THE MOJAVE SINK: AN ARCHAEOLOGICAL MYTH A Thesis Presented to the Faculty of California State University, San Bernardino by Barbara Ann Loren-Webb March 2003 Approved by: Russell Barber, Chair, Anthropology Date Pete Robertshesw, Anthropology ABSTRACT In 1929 Malcolm Rogers published a paper in which he stated that there was evidence of an Anasazi or Puebloan settlement or pueblo, in the Mojave Sink Region of the Mojave Desert. Since then, archaeologists have cited Rogers' publication and repeated his claim that such a pueblo was located in the Western Mojave Desert. The purpose of this thesis started out as a review of the existing evidence and to locate this pueblo.
    [Show full text]