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Daily Iowan (Iowa City, Iowa), 1953-10-22
The Weather Serving the State Partb c10., aDd eeoIH ·versity of Iowa toda,. CleariDc ....... Art slderlbb eooIer FrWar. Campus and JII,h ~aJ. T.; 1_. 52; Hla'h WednH41a7. II; low. he SUI art i.:wa City 67. attend the 1868 - A,P Leased Wile, Wirephot.o - Five Cent. Iowa City, Iowa, Thursday, Oct. 22, 1953 - Vol. 97, No. 276 the found- , Eat. College Art • ~---------------------------------------------- Department orlSin. Mln ./ '0 the rti.t trom .ohio the conter- ~ shown by ueen ·Will· Open Homecoming ence df 1he AcsthetJcs ege in. No- • Homecoming Mums Aqui Show To Feature Five Iowa sportscasters and Qne ------------ Varied Acts sports writer will judge the utes past any given point In the beauty, or~inallty and humor ot parade route. The 40 tloats wiU Three days ot 1953 Homecom , ' the I10nt entries In the fifth an- then move to the area just east In, frolic will let the ful\-steam- nual SUI Homecoming parade Frl- of Iowa stadium to remain throu,ll abead si,nal tonight when one ot day night at 7. Saturday's game as a post-parade Taking time out from their re- dISplay parade chairman Loren five campus lovelies is named porting responsibilities to score Hlcker ~on lays. Dolphin Queen for SUY'! 31st an- each of 40 floats ror beaut), will . nUIII poolsld~ sholl'. be Gene Claussen, KXIC Iowa Musical marching grou~s In the City and Gene Shumate KSO De parade will total 13, With nine Pre!\Cntatlon of the qucen-ror- Moines. • high school bands, Shriner bands a-weekend will come at 8 p.m. -
Martian Crater Morphology
ANALYSIS OF THE DEPTH-DIAMETER RELATIONSHIP OF MARTIAN CRATERS A Capstone Experience Thesis Presented by Jared Howenstine Completion Date: May 2006 Approved By: Professor M. Darby Dyar, Astronomy Professor Christopher Condit, Geology Professor Judith Young, Astronomy Abstract Title: Analysis of the Depth-Diameter Relationship of Martian Craters Author: Jared Howenstine, Astronomy Approved By: Judith Young, Astronomy Approved By: M. Darby Dyar, Astronomy Approved By: Christopher Condit, Geology CE Type: Departmental Honors Project Using a gridded version of maritan topography with the computer program Gridview, this project studied the depth-diameter relationship of martian impact craters. The work encompasses 361 profiles of impacts with diameters larger than 15 kilometers and is a continuation of work that was started at the Lunar and Planetary Institute in Houston, Texas under the guidance of Dr. Walter S. Keifer. Using the most ‘pristine,’ or deepest craters in the data a depth-diameter relationship was determined: d = 0.610D 0.327 , where d is the depth of the crater and D is the diameter of the crater, both in kilometers. This relationship can then be used to estimate the theoretical depth of any impact radius, and therefore can be used to estimate the pristine shape of the crater. With a depth-diameter ratio for a particular crater, the measured depth can then be compared to this theoretical value and an estimate of the amount of material within the crater, or fill, can then be calculated. The data includes 140 named impact craters, 3 basins, and 218 other impacts. The named data encompasses all named impact structures of greater than 100 kilometers in diameter. -
APR 2 0 2005 Sigjfeture Oncertifying Official Date
NFS Form 10-900 / AO^/rS^ OMB No. 1024-0018 (Rev. 10-90) United States Department of the Interior National Park Service NATIONAL REGISTER OF HISTORIC PLA REGISTRATION FORM ^ ^ ^ This form is for use in nominating or requesting determinations for individual properties and districts. See instructions in How to Complete the National Register of Historic Places Registration Form (National Register Bulletin 16A). Complete each item by marking "x" in the appropriate box or by entering the information requested. If any item does not apply to the property being documented, enter "N/A" for "not applicable." For functions, architectural classification, materials, and areas of significance, enter only categories and subcategories from the instructions. Place additional entries and narrative items on continuation sheets (NFS Form 10-900a). Use a typewriter, word processor, or computer, to complete all items. 1. Name of Property historic name: Holualoa 4 Archaeological District (State Site No. 50-10-37-23.661) other names/site number: Kamoa Point/Keolonahihi Complex (10-37-2059): Keakealaniwahine Residential Complex (no #): and Kaluaokalani______________ 2. Location street & number Ali'i Drive not for publication city or town Kailua-Kona vicinity ______ state Hawaii code HI county Hawaii zip code 96745 3. State/Federal Agency Certification As the designated authority under the National Historic Preservation Act of 1986, as amended, I hereby certify that this x nomination __ request for determination of eligibility meets the documentation standards for registering properties in the National Register of Historic Places and meets the procedural and professional requirements set forth in 36 CFR Part 60. In my opinion, the property x meets __ does not mi National Register Criteria. -
Planetary Constants and Models
JPL D-12947 PF-IOO-PMC-01 Mars Pathfinder ProJect PLANETARY CONSTANTS AND MODELS Mars at Launch Earth at La_ Dec 2, 1996 SunI, Earth at Mars at Aniva July 4, 1997 December 1995 JilL Jet Propulsion Laboratory California Institute of Technology Pasadena, California JPL D-I2947 PF-IOO-PMC-OI Mars Pathfinder Project PLANETARY CONSTANTS AND MODELS Prepared by: ' Robin Vaughan December 1995 JPL Jet Propulsion Laboratory California Institute of Technology Pasadena, California JPL D-12947 PFolOO-PMCoO1 Revision History Date Changes Status 10/95 Issued preliminary version for review by project person-el Draft 12/95 First official release; incorporated comments from prelimi- Final nary review. JPL D- !294 7 PFo 100-PMCo 01 Contents List of Figures V 4 List of Tables vii List of Acronyms and Abbreviations ix INTRODUCTION 1 1.1 Purpose ............ .......................... 1 1.2 Scope .................... ................... 1 2 COORDINATE SYSTEMS 3 2.1 Definitions 2.1.1 Frame • " • • • ° * ° • " ° • * • ° ° " ° ° * ° • • • ° " " " ' • • • • • • 3 2.1.2 Center • " " • ° " " " ' ° ° ° • * " • • " • " • • " • " " " ° • ° • • • . • 6 2.1.3 Type .................................... 7 2.2 Celestial Systems . ; ............................. 7 2.2.1 The Inertial Reference Frames ..................... 8 2.2.2 Sun-Centered Systems .......................... 9 2.2.3 Earth-Centered Systems ......................... 9 2.2.4 Mars-Centered Systems ......................... 11 2.2.5 Spacecraft-CenteredSystems ...................... 16 2.2.6 MiscellaneousSystems -
Topographic History of the Maui Nui Complex, Hawai'i, and Its Implications for Biogeography1
Topographic History ofthe Maui Nui Complex, Hawai'i, and Its Implications for Biogeography 1 Jonathan Paul Price 2,4 and Deborah Elliott-Fisk3 Abstract: The Maui Nui complex of the Hawaiian Islands consists of the islands of Maui, Moloka'i, Lana'i, and Kaho'olawe, which were connected as a single landmass in the past. Aspects of volcanic landform construction, island subsi dence, and erosion were modeled to reconstruct the physical history of this complex. This model estimates the timing, duration, and topographic attributes of different island configurations by accounting for volcano growth and subsi dence, changes in sea level, and geomorphological processes. The model indi cates that Maui Nui was a single landmass that reached its maximum areal extent around 1.2 Ma, when it was larger than the current island of Hawai'i. As subsi dence ensued, the island divided during high sea stands of interglacial periods starting around 0.6 Ma; however during lower sea stands of glacial periods, islands reunited. The net effect is that the Maui Nui complex was a single large landmass for more than 75% of its history and included a high proportion of lowland area compared with the contemporary landscape. Because the Hawaiian Archipelago is an isolated system where most of the biota is a result of in situ evolution, landscape history is an important detertninant of biogeographic pat terns. Maui Nui's historical landscape contrasts sharply with the current land scape but is equally relevant to biogeographical analyses. THE HAWAIIAN ISLANDS present an ideal logic histories that can be reconstructed more setting in which to weigh the relative influ easily and accurately than in most regions. -
Local Lunar Gravity Field Analysis Over the South Poleaitken Basin from SELENE Farside Tracking Data
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 117, E02005, doi:10.1029/2011JE003831, 2012 Local lunar gravity field analysis over the South Pole-Aitken basin from SELENE farside tracking data Sander Goossens,1,2,3 Yoshiaki Ishihara,1 Koji Matsumoto,1 and Sho Sasaki1 Received 16 March 2011; revised 22 November 2011; accepted 13 December 2011; published 14 February 2012. [1] We present a method with which we determined the local lunar gravity field model over the South Pole-Aitken (SPA) basin on the farside of the Moon by estimating adjustments to a global lunar gravity field model using SELENE tracking data. Our adjustments are expressed in localized functions concentrated over the SPA region in a spherical cap with a radius of 45° centered at (191.1°E, 53.2°S), and the resolution is equivalent to a 150th degree and order spherical harmonics expansion. The new solution over SPA was used in several applications of geophysical analysis. It shows an increased correlation with high-resolution lunar topography in the frequency band l =40–70, and admittance values are slightly different and more leveled when compared to other, global gravity field models using the same data. The adjustments expressed in free-air anomalies and differences in Bouguer anomalies between the local solution and the a priori global solution correlate with topographic surface features. The Moho structure beneath the SPA basin is slightly modified in our solution, most notably at the southern rim of the Apollo basin and around the Zeeman crater. Citation: Goossens, S., Y. Ishihara, K. Matsumoto, and S. Sasaki (2012), Local lunar gravity field analysis over the South Pole-Aitken basin from SELENE farside tracking data, J. -
U-Series Isotopic Constraints on Mantle Upwelling on the Periphery of the Hawaiian Plume Isotope Geochemistry of Haleakala Crater Basanites Erin H
U-series isotopic constraints on mantle upwelling on the periphery of the Hawaiian plume Isotope geochemistry of Haleakala crater basanites Erin H. Phillips and Kenneth W.W. Sims, University of Wyoming, and Vincent J.M. Salters, Florida State University 1. Introduction 2. Major and Trace Element Geochemistry and Long-lived Radiogenic Isotopes 100 400 ● The Hawaiian islands are part of the age progressive series of 16 Comparison to Haleakala Crater (this study) 90 global alkaline volcanoes that form the Hawaiian-Emperor seamount chain. At 14 Haleakala SW Rift Zone (Sims et al., 1999) 300 suites Haleakala, on the island of Maui, basanitic lavas of the Hana Haleakala post-shield 80 12 Haleakala shield 200 Volcanics represent end-member rejuvenated stage alkaline 70 Kilauea magmatism (Clauge, 1987). Although shield-stage tholeiitic 100 10 Mauna Loa 60 volcanism predominates in the Hawaiian islands, alkaline lavas O 2 Mauna Kea 0 erupted on the trailing edge of the Hawaiian plume present an 8 Hualalai trachytes 50 O+Na important component to understanding mantle melting and solid 2 Loihi K 40 6 Nyiragongo mantle upwelling. Averages for 30 Leucite Hills lamproites Hawaiian Lavas 4 Ross Island, Antarctica basanites 20 ● We present geochemical data for 13 samples from Haleakala Samoa crater. 14C ages for seven samples range from 870 ± 40 to 4070 ± 50 2 See supplement for full reference list 10 years (Sherrod and McGeehin, 1999). Preliminary data for 5 0 1995) Mantle (McDonough and Sun, Sample/Primitive 0 samples from the Haleakala southwest rift zone (Sims et al., 1999) 35 40 45 50 55 60 65 Rb Ba Th U Nb La Ce Sr Pb Nd Sm Hf Eu Dy Y Yb Lu SiO are consistent with iso-viscous (Watson and McKenzie, 1991) and 2 thermo-viscous (Hauri et al., 1994) fluid mechanical models of 10 plume upwelling in which upwelling rates are slower on the Hawaiian Lavas periphery of plume. -
A Prodromus of the Water Bear Fauna of Haleakala National Park
A PRODROMUS OF THE WATER BEAR FAUNA OF HALEAKALA NATIONAL PARK Samuel M. Gon III Department of Entomology University of Hawai'i Honolulu, Hawai'i 96822 Robert A. Kimsey and Robert O. Schuster Department of Entomology University of California Davis, California 95616 Mark A. Willis Department of Entomology University of California Riverside, California 92507 ABSTRACT: The terrestrial meiofauna of the Hawaiian islands is almost completely unknown to science. Water bears (Tardigrada) represent a phylum that seems preadapted for long distance dispersal to the Hawaiian islands, and here we present, for the first time, 31 species in 10 genera and four families. The diversity of species in an area smaller than 50 square miles means that the Haleakala site is the most tardigrade rich location yet found on the planet. These species occupy a highly specialized niche in the Central Crater District of Haleakala National Park that involves alpine and subalpine cryptogams subject to extremes of temperature and desiccation. Several of the Hawaiian species are capable of anhydrobiosis, which is probably the mechanism that allows their occupation of alpine habitats. We present arguments that suggest that the richest habitats for Hawaiian water bears will be in subalpine and alpine settings of Maui and Hawai'i. 15 INTRODUCTION The biota of the Hawaiian islands attracts biologists because of its diversity. We have all came to expect new and exciting things here; new species being among the more engaging discoveries. We report here a first glimpse of a fascinating phylum that has until now passed generally unnoticed in Hawaiian biology. The phylum is Tardigrada, comprised of small (50 to 1200 micron) creatures usually called water bears because of their appearance and deliberate "pawing" form of locomotion. -
Hawaiʻi Board on Geographic Names Correction of Diacritical Marks in Hawaiian Names Project - Hawaiʻi Island
Hawaiʻi Board on Geographic Names Correction of Diacritical Marks in Hawaiian Names Project - Hawaiʻi Island Status Key: 1 = Not Hawaiian; 2 = Not Reviewed; 3 = More Research Needed; 4 = HBGN Corrected; 5 = Already Correct in GNIS; 6 = Name Change Status Feat ID Feature Name Feature Class Corrected Name Source Notes USGS Quad Name 1 365008 1940 Cone Summit Mauna Loa 1 365009 1949 Cone Summit Mauna Loa 3 358404 Aa Falls Falls PNH: not listed Kukuihaele 5 358406 ʻAʻahuwela Summit ‘A‘ahuwela PNH Puaakala 3 358412 Aale Stream Stream PNH: not listed Piihonua 4 358413 Aamakao Civil ‘A‘amakāō PNH HBGN: associative Hawi 4 358414 Aamakao Gulch Valley ‘A‘amakāō Gulch PNH Hawi 5 358415 ʻĀʻāmanu Civil ‘Ā‘āmanu PNH Kukaiau 5 358416 ʻĀʻāmanu Gulch Valley ‘Ā‘āmanu Gulch PNH HBGN: associative Kukaiau PNH: Ahalanui, not listed, Laepao‘o; Oneloa, 3 358430 Ahalanui Laepaoo Oneloa Civil Maui Kapoho 4 358433 Ahinahena Summit ‘Āhinahina PNH Puuanahulu 5 1905282 ʻĀhinahina Point Cape ‘Āhinahina Point PNH Honaunau 3 365044 Ahiu Valley PNH: not listed; HBGN: ‘Āhiu in HD Kau Desert 3 358434 Ahoa Stream Stream PNH: not listed Papaaloa 3 365063 Ahole Heiau Locale PNH: Āhole, Maui Pahala 3 1905283 Ahole Heiau Locale PNH: Āhole, Maui Milolii PNH: not listed; HBGN: Āholehōlua if it is the 3 1905284 ʻĀhole Holua Locale slide, Āholeholua if not the slide Milolii 3 358436 Āhole Stream Stream PNH: Āhole, Maui Papaaloa 4 358438 Ahu Noa Summit Ahumoa PNH Hawi 4 358442 Ahualoa Civil Āhualoa PNH Honokaa 4 358443 Ahualoa Gulch Valley Āhualoa Gulch PNH HBGN: associative Honokaa -
Kapa'a, Waipouli, Olohena, Wailua and Hanamā'ulu Island of Kaua'i
CULTURAL IMPACT ASSESSMENT FOR THE KAPA‘A RELIEF ROUTE; KAPA‘A, WAIPOULI, OLOHENA, WAILUA AND HANAMĀ‘ULU ISLAND OF KAUA‘I by K. W. Bushnell, B.A. David Shideler, M.A. and Hallett H. Hammatt, PhD. Prepared for Kimura International by Cultural Surveys Hawai‘i, Inc. May 2004 Acknowledgements ACKNOWLEDGMENTS Cultural Surveys Hawai‘i wishes to acknowledge, first and foremost, the kūpuna who willingly took the time to be interviewed and graciously shared their mana‘o: Raymond Aiu, Valentine Ako, George Hiyane, Kehaulani Kekua, Beverly Muraoka, Alice Paik, and Walter (Freckles) Smith Jr. Special thanks also go to several individuals who shared information for the completion of this report including Randy Wichman, Isaac Kaiu, Kemamo Hookano, Aletha Kaohi, LaFrance Kapaka-Arboleda, Sabra Kauka, Linda Moriarty, George Mukai, Jo Prigge, Healani Trembath, Martha Yent, Jiro Yukimura, Joanne Yukimura, and Taka Sokei. Interviews were conducted by Tina Bushnell. Background research was carried out by Tina Bushnell, Dr. Vicki Creed and David Shideler. Acknowledgements also go to Mary Requilman of the Kaua‘i Historical Society and the Bishop Museum Archives staff who were helpful in navigating their respective collections for maps and photographs. Table of Contents TABLE OF CONTENTS I. INTRODUCTION............................................................................................................. 1 A. Scope of Work............................................................................................................ 1 B. Methods...................................................................................................................... -
Regional Tsunami Evacuations for the State of Hawaii: a Feasibility Study Based on Historical Runup Data
REGIONAL TSUNAMI EVACUATIONS FOR THE STATE OF HAWAII: A FEASIBILITY STUDY BASED ON HISTORICAL RUNUP DATA Daniel A. Walker Tsunami Memorial Institute 59-530 Pupukea Road Haleiwa, Hawaii 96712 ABSTRACT Historical runup data for the Hawaiian Islands indicate that evacuations of only limited coastal areas, rather than statewide evacuations, may be appropriate for some small tsunamis originating along the Kamchatka, Aleutian, and Alaskan portion of the circum-Pacific arc. With such limited evacuations most statewide activities can continue with little or no disruptions, saving millions in lost revenues and overtime costs, and maintaining or enhancing credibility in state and federal agencies. However, such evacuations are contingent upon accurate real-time modeling of the maximum expected runup values. Also, data indicate that such evacuations may not be appropriate for small Chilean tsunamis. Furthermore, data from other regions are thus far too limited for an evaluation of the appropriateness of partial evacuations for small tsunamis from those regions. Science_of_Tsunami_Hazards,_Vol_22,_No._1,_page_3_(2004) Introduction Historical data indicate that tsunami runups are generally greatest along the northern coastlines of the Hawaiian Islands for earthquake originating in that portion of the circum-Pacific arc from Kamchatka through the Aleutians Islands to Alaska. A critical question is whether a statewide warning should be issued if tide gauge, magnitude, and modeling data predict a maximum runup of only 1 meter for some portions of those northern shores. [A one meter tsunami is generally considered by the scientific community and civil defense agencies to be a potentially life threatening phenomenon requiring a warning, if possible, of its arrival and location.] The answer to the question depends on the accuracy of the prediction and how much smaller the runups might be on those other coastlines. -
Association of Unit Owners Contact List
Association of Unit Owners Contact List Project Name/Number AOUO Designated Officer for Direct Contact/Mailing Address Management Company/Telephone Number 1001 WILDER GAIL PRESIDENT 1001 Wilder, #403 CITY PROPERTIES INC Reg.# 5 LEVY HONOLULU HI 96822 8085241455 1010 WILDER RICHARD TREASURER 1010 WILDER AVE 1602 SELF MANAGED Reg.# 377 KENNEDY HONOLULU HI 96822 8085241961 1011 PROSPECT RICHARD PRESIDENT 1188 BISHOP ST STE 2503 CERTIFIED MGMT INC, DBA ASSOCIA HAW Reg.# 1130 CONRADT HONOLULU HI 96813 8088360911 1015 WILDER LINDA PRESIDENT 1015 WILDER AVE #905 HAWAIIANA MGMT CO LTD Reg.# 1960 FUJITANI HONOLULU HI 96822 8085939100 1037 KAHUAMOKU VITA PRESIDENT 94-1037 KAHUAMOKU ST 3 OISHI'S PROP MGMT CORP Reg.# 1551 VILI WAIPAHU HI 96797 8089499499 1040 KINAU JERRY PRESIDENT 55 S JUDD ST 607 HAWAIIAN PROPERTIES, LTD Reg.# 527 ZAK HONOLULU HI 96817 8085399777 1041 KAHUAMOKU Alan President 94-1041 Kahuamoku Street, #404 CEN PAC PROPERTIES INC Reg.# 1623 Ige Waipahu HI 96797 8085932902 1054 KALO PLACE JUANA PRESIDENT 1415 S KING STREET, #504 HAWAIIANA MGMT CO LTD Reg.# 5450 DAHL HONOLULU HI 96814 8085939100 1073 KINAU ANSON PRESIDENT 1073 KINAU ST #1003 HAWAIIANA MANAGEMENT COMPANY, LTD Reg.# 616 QUACH HONOLULU HI 96814 8085939100 1111 WILDER BRENDAN PRESIDENT 1111 WILDER AVE #7A HAWAIIAN PROPERTIES, LTD Reg.# 228 BURNS HONOLULU HI 96822 8085399777 1112 KINAU LINDA Y SOLE OWNER 1112 KINAU ST PH Reg.# 1295 NAKAGAWA HONOLULU HI 96814 1133 WAIMANU KELFRED PRESIDENT 975 Kapiolani Blvd Ste 200 CITY PROPERTIES INC Reg.# 3335 CHANG Honolulu HI 96814 8085241455