Hawaiian quilts (see procedures

Goemetry and Quilts Lesson Quilt Blocks: Geometry with a Cultural Warmth Subjects :Geometry, Social Sciences, Clothing and Textiles, Art Patty Winkler Michael E. DeBakey High School for Health Professions Houston, TX email address: pwinkler@houstonisd.org All rights reserved. Any use of these materials is prohibited without the expressed written permission of the author. Overview This lesson can be taught at any grade level but is recommended for middle or high school. It is meant to be a fun lesson to generate interest in geometrical patterns and the world around us. Objectives Develop an appreciation of geometry as a means of describing the physical world Recognize and appreciate the geometric patterns found in quilts Describe the symmetry and other geometric aspects of quilt block patterns Create scale drawing of life objects. Discuss the history and cultural influence of some of the quilt blocks found Find and view information from the WWW Materials Needed squares of paper or cloth for Hawaiian quilts (see procedures for details)quad rule graph papercolored pencils, markers or crayonsresource materials listed below Procedures Quilting is a wonderful pastime which has lost its luster and interest in todays generations. Quilting has many wonderful traditions which can be explored in may different ways. I have outlined some ideas below and included just a few of the cultural resources I have found. Try to find a guest speaker to discuss quilting and some of the new and old patterns. Hawaiian quilting: Hawaiian quilting differs from that which evolved in other parts of the world. Its unique method of design leaves a striking impression on anyone who has the opportunity to view a finished product. The actual emergence of this style of quilting is pure speculation, as to date, no information has been found to substantiate any one theory. A set of instructions and steps for making a quilt are included with the lesson. Take some time to read the Introduction to gain a better understanding of the emergence of this type of quilting. After the history has been discussed, have the students create a design of their own by following the steps for folding and creating the design. If square are not available in the suggested 16 and 20 size, use 6 and 8.5 squares. Once they have created a design in one color from a 6 square have them choose another color to paste it on. Once they have created their quilt block have them fake the echo stitching by lightly demonstrating the technique in pencil throughout their block. Once all blocks are completed by the students, put them together on a bulletin board or tape their backs together to create your own Hawaiian quilt. Have students discuss how they got the design they had and if they were using anything from their life or nature to create the design. Early American/European patchwork quilting This type of quilting involves cutting pieces of cloth in specific shapes and sizes to create a desired pattern. There are hundreds of patchwork patterns and variations with new ones being developed regularly. I have included the initial page from an Internet site on Amish quilts. The Amish are famous for their quilting techniques. The midwestern Amish do more intricate patchwork designs where the Pennsylvania Amish have very simple patchwork with very intricate and detailed quilting lines. The quilts with the detailed stitching are desired worldwide and can be very expensive. Students should do some research on patchwork quilting. There are a number of sites on the Internet as well as a numerous magazines and books available on the market. Once they have seen some of the patterns which are already in existence, show them the two that are included here. One is called Kaleidoscope and the other is called Fractal. They can see a very direct relationship to mathematics through these quilts. They are both brand new designs. African American quilting The influence of the African textile techniques and practices are evident in the quilts with this distinct style. African style quilting shows two major influences. First is the African preference for strip textiles and strips of cloth developed on hand looms. Second are the religious symbols of their cultures. These both appear in many of the quilts of African-American quilting. Some of the most famous quilt designs include: Lazy Gal; Spider Leg; Twin Sisters; Spider Web; and Wild Goose Chase. Whether consisting of a single piece or many small scraps of cloth, strips are a dominant design element as well as a chief construction technique in both West African textiles and Afro-American quilts. I have included a copy of the article African Symbolism in Afro-American Quilts from African Arts magazine. The reference is included in the reference list at the end of this group of lessons. Once the students have had a chance to explore patchwork quilting, have them use graph paper to design (in scale) and color their own patchwork quilt. Quad rule graph paper works best here. Have them share these designs either in small groups or by placing them on a bulletin board or empty wall. Evaluation The creation of the designs discussed above. Resource Materials Quilting in America Paint a Quilt Lesson Quilt Gallery Quilts - One of my favorite things Immigration Quilt Project Hawaiian Quilting materials Aloha Quilts Helen Friend-Hawaiian Quilter Amish Quilting Materials Homepage for American Quilts Amish Art African-American quilting article General quilting information Yahoo search - Quilting Teacher Comments Growing up in a small, rural, farming community gave me a deep appreciation for the art and craft of quilting. I am not very skillful, unlike my sister and my aunts; however, I do see and understand the geometry involved in designing an appealing quilt. There are hundreds (maybe thousands) of quilt block designs all around the world. Each of them was created by someone who wanted to tell a story, make a point, or stir an emotion. This is an art that is dying and needs to be rekindled in the younger generations.

Hawaiian food, prizes Fireworks

Inside Binghamton University PO Box 6000 Binghamton, NY 13902-6000 Contacts SUBMIT to insideBU : News Ads 777-2174 DATELINE -A daily news listserv: Submit news, subscriptions DAILY EVENTS 777-3535 SPORTS 777-6666 WEATHER UPDATES 777-7669 (SNOW) Published weekly during the academic year by the Office of Communications and Marketing. >> COMMENTS October 03, 2003 Volume 25, No. 6 >> BACK ISSUES Headlines >> Homecoming 2003 Join the Hawaiian luau during Homecoming 2003 Homecoming schedule Berg showcases his lullaby to Broadway Exemplary student to be named during Homecoming Alumni artwork exhibition displayed during weekend Roam the trails with campus community and alumni Comedian Tommy Davidson to make Homecoming appearance Baxters Village Luau offers Hawaiian food, prizes Fireworks to conclude Homecoming celebration Baxters Village Luau offers Hawaiian food, prizes The Peace Quad takes on a Hawaiian flavor from noon to 4 p.m. Saturday, October 11, for Baxters Village Luau. Catch a display of the Brain Train floats on the Peace Quad drive after the parade. Festivities kick off at 1 p.m. with a hula dancing performance. The 2003 Exemplary Student Award will be announced at approximately 1:10 p.m. The luau will also feature a dunk tank, spaghetti wrestling and a limbo contest. A steel drum band will provide a performance. Students and alumni can sign up for prize drawings, which will take place throughout the afternoon. Various student and campus groups will table in the Luau tent village. A menu reflective of Homecomings hula theme will be available. Treats include aloha chicken breast sandwich, veggie burgers, Italian sausage with peppers and onions, hamburgers, hotdogs, fresh fruit and tropical bars. Students eat free, alumni and visitors pay $3 at the Alumni Welcome Center. Giveaways include smoothies pina colada and orange squeeze and popcorn.

Hawaii Hotels Hawaii Resorts

Hawaii Hotels. Hawaii Resorts Accommodation and Apartments Discounts My Account UnitedStates Hawaii Hotels Seattle Hotels San Francisco Hotels San Diego Hotels Los Angeles Hotels SanJose Hotels Phoenix Hotels Portland Hotels Anaheim Hotels Miami Hotels Chicago Hotels Coronado Island Hotels RelatedLinks Hawaii Hotels Hawaii Resorts Accommodation and Apartments Discounts for online Reservation Welcome to HolidayCity reservation service! We provide a wide selection of properties - budget, business, tourist, luxury, bed and breakfasts and apartments accommodation. HolidayCity Hawaii hotels offer comfort, quality and great value for the money, ideal for leisure and business travellers. To start selecting, click on the hotel links below, categorised by prices and locations. The hotels in the Most Popular Box represent frequently booked accommodation by our guests. Search for Hawaii Hotels Country : City : Check-in Date : 01 02 03 04 05 06 07 08 09 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Check-out Date : 01 02 03 04 05 06 07 08 09 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec No. of Rooms : 1 2 3 4 5 6 7 8 9 10 No. of Adults : 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 No. of Children : 0 1 2 3 4 5 Hawaii Hotels by Price Below US$ 120 HolidayCity Most Popular Park Shore Waikiki Hotel Hawaii US$134 Hotel Four Seasons Resorts Maui US$345 US$ 120 to US$ 220 Above US$ 220 View All Hawaii Resorts by Location Honolulu Maui Waikiki Beach Kona Other Areas Select Hotels in Hawaii by Location by clicking on the map below Hawaii Hotels Los Angeles

Hawaiian Islands are volcanic

The Formation of the Hawaiian Islands The Formation of the Hawaiian Islands [ HCV Home ][Formation of the Islands][ Active Hawaiian Volcanoes ][ General Info ]    The Hawaiian Islands are volcanic in origin. Each island ismade up of at least one primary volcano, although many islandsare composites of more than one. The Big Island, for instance,is constructed of 5 major volcanoes: Kilauea, Mauna Loa, Mauna Kea,Hualalai and Kohala. Mauna Loa is the largest active volcano onEarth. Kilauea is presently one of the most productive volcanoeson Earth (in terms of how much lava it erupts each year). The primary volcanoes on eachof the islands are known as a shield volcanoes, which are gently sloping mountains produced from a large number of generally very fluid lava flows.    Hawaiian volcanoes primarily erupt a type of rock known as basalt. When molten, basalt produces liquids of relatively high fluidity, compared to volcanoesthat erupt more silica rich magma types such as andesite, dacite or rhyolite. The fluidity of molten basalt favors the formation of lava flows,which is why the Hawaiian volcanoes generally have gentle sloping sides. Bycontrast, lavas with higher silica content are more viscous and commonly produce either thicker, shorter lava flows, thick blocky deposits and/orthick beds of ash that fall from the sky following explosive eruptions.These other types of volcanoes (common outside of Hawaii) are typically steepersided.    The Hawaiian volcanoes were produced by the Hawaiian hot spot, which is presently under the Big Island of Hawaii.The image below shows the islands of the Hawaiian chainand the intervening shallows, banks and reefs along a line from southeastto northwest. Note that the islands of Lanai and Kahoolawe are not shownbecause they would "overlap" with Molokai and Maui, respectively( see the map of the Islands on the Hawaiian Volcanoes page )In general, when you move along the island chain from southeast (Hawaii) to northwest, (Kure), the volcanoes become older and older.     The aging of the islands with distance from the current hot spotis demonstrated in the diagram below, where distance along thechain is approximated as distance away from Kilauea volcano (theyoungest above-sea-level Hawaiian volcano). In fact, even beyond Kurethe Hawaiian chain continues as a series of now-submergedformer islands known collectively as the Emperorseamounts. The two primary volcanoes that make up Oahu (where Honolulu is) have not erupted for well over a million years!    The age trend of the volcanoes is thought to be due tothe way in which the islands are built on the moving sea floor of the NorthPacific Ocean: the Pacific Ocean is mostly floored by a single tectonic plate(known as the "Pacific Plate")that is moving over the layer in the Earth known as the Asthenosphere.This movement takes it to the northwest compared to the layers below itat a rate of 5 to 10 cm/yr (the rate depends on where you are on it). As theplate moves over a fixed spot deeper in the Earth where magma (moltenlava) forms, a new volcano can punch through this plate and createan island. The Hawaiian Islands are believed to be formed from onesuch 'hot spot'. As the plate moves away, the volcano stops eruptingand a new one is formed in its place. With time, the volcanoes keepdrifting westward and getting older relative to the one active volcanothat is over the hot spot. As they age, the crust upon which they sitcools and subsides. This, combined with erosion of the islands onceactive volcanism stops, leads to a shrinking of the islands with ageand their eventual submergence below the ocean surface.    Importantly, the time over which various active volcanoes on the islandsremain active is long (hunders of thousands of years) so that significantoverlap in ages occur on neighboring islands. For instance although Haleakala volcano on Mauiis a great distance away from the presently erupting Kilauea, Haleakalalast erupted only about 200 years ago. Currently there are 3 Hawai'ian volcanoes that we can easily classify as active: Kilauea, actively erupting since 1983 Mauna Loa, which last erupted in 1984 and is building for a new eruption inthe next few years Loihi, which erupted in 1996   All three of these active Hawaiian volcanoes sharethe Hawaiian hot spot, but retain unique volcanic histories and compositions.You can view a schematic representationof the geometry of this situation HERE The most likely Dormant volcanoes are: Hualalai, which last erupted in 1801 Haleakala, which last erupted in about 1790 Mauna Kea, which last erupted about 4,000 years ago.    Here is some additional general age information from USGS Professional Paper 1350 , Chapter 1 by Clague and Dalrymple, pages 5-54 (1987). Data from that source has been augmented by data and information in Garcia et al. Lithos , vol 20, pages 323-336 (1987) and Clague (1996) in The Origin and Evolution of Pacific Island biotas, New Guniea to Eastern Polynesia, patterns and processes (Keast and Miller, editors), pages 35-50. Ages of some of the Hawaiian Islands and outer seamounts Volcano Number (see note at table bottom) Volcano Name Distance from Kilauea along trend of chain (km) Best K-Ar age (Ma) Data Source (tabulated below) 1 Kilauea 0 0-0.4 -- 3 Mauna Kea 54 0.375 + 0.05 1 5 Kohala 100 0.43 + 0.02 2 6 Haleakala 182 0.75 + 0.04 3 7 Kahoolawe 185 > 1.03 + 0.18 3 8 West Maui 221 1.32 + 0.04 4 9 Lanai 226 1.28 + 0.04 5 10 East Molokai 256 1.76 + 0.04 3 11 West Molokai 280 1.90 + 0.06 3 12 Koolau 339 2.6 + 0.1 4,6 13 Waianae 374 3.7 + 0.1 6 14 Kauai 519 5.1 + 0.20 7 15 Niihau 565 4.89 + 0.11 8 15A Kaula 600 4.0 + 0.2 21 17 Nihoa 780 7.2 + 0.3 9 20 Unnamed 913 9.2 + 0.8 20 930 9.6 + 0.8 22 23 Necker 1,058 10.3 + 0.4 9 26 La Perouse Pinnacles 1,209 12.0 + 0.4 9 27 Brooks Bank 1,256 13.0 + 0.6 20 1,330 13.0 + 0.6 22 30 Gardner Pinnacles 1,435 12.3 + 1.0 20 1,460 12.3 + 1.0 22 36 Laysan 1,818 19.9 + 0.3 10 37 Northampton Bank 1,841 26.6 + 2.7 10 50 Pearl and Hermes Reef 2,281 20.6 + 2.7 11 52 Midway 2,432 27.7 + 0.6 12 57 Unnamed 2,600 28.0 + 0.4 11 63 Unnamed 2,825 27.4 + 0.5 11 65 Colohan 3,128 38.6 + 0.3 13 65A Abbott 3,280 38.7 + 0.9 13 67 Daikakuji 3,493 42.4 + 2.3 14 69 Yuryaku 3,520 43.4 + 1.6 11 72 Kimmei 3,668 39.9 + 1.2 14 74 Koko (southern) 3,758 48.1 + 0.8 14,15 81 Ojin 4,102 55.2 + 0.7 16 83 Jingu 4,175 55.4 + 0.9 17 86 Nintoku 4,452 56.2 + 0.6 16 90 Suiko (southern) 4,794 59.6 + 0.6 18,19 91 Suiko (central) 4,860 64.7 + 1.1 16 Data Sources: 1. Porter and others (1977) 12. Dalrymple and others (1977) 2. McDougall and Swanson (1972) 13. Duncan and Clague (1984) 3. Naughton and others (1980) 14. Dalrymple and Clague (1976) 4. Mcdougall (1964) 15. Clague and Dalrymple (1973) 5. Bonhommet and others (1977) 16. Dalrymple and others (1980a) 6. Doel and Dalrymple (1973) 17. Dalrymple and Garcia (1980) 7. McDougall (1979) 18. Saito and Ozima (1975) 8. G.B. Dalrymple (unpub. Data, 1982) 19. Saito and Ozima (1977) 9. Dalrymple and others (1974) 20. Garcia and others (1986b) 10. Dalrymple and others (1981) 21.Garcia and others (1986a) 11. Clague and others (1975) 22. Garcia and Others (1987) Other Notes: "Volcano Number" refers to the number in sequence along the HawaiianChain. Loihi, the youngest expression of the Hawaiian hot spot isnumber 0, Kilauea is number 1, etc.. Note that not all volcanoesare listed in the table (e.g., number 2 = Mauna Loa and number 4 =Hualalai); also note that further up the chain, the numbering schemebecomes more subjective. HCV Home Hawaiian Volcanoes Loihi Kilauea Mauna Loa Hualalai This page created and maintained by Ken Rubin ©, krubin@soest.hawaii.edu Other credits for this web site. Last page update on 4 Apr 2005

Hawaii Volcano

Volcano Watch [ TEXT ONLY ] Volcano Watch Volcano Watch is a weekly newsletter written by the scientists at the US Geological Survey's Hawaiian Volcano Observatory. It is published in the Hawaii Tribune-Herald's Sunday newspaper and the West Hawai'i Today's Monday newspaper, and posted here the following Monday or Tuesday. While primarily addressed to the residents of the Big Island of Hawai`i, some articles may have a broader scope. Article topics may range from volcanic features on the Big Island, volcanic hazards, informational topics of Long Valley, Montserrat, or Alaska, to topics about the Hawaiian Volcano Observatory. Latest Issue: January 19, 2006: Revolution in thinking about Kilauea's explosions comes to HVO: Part 1 Previous Issue: January 12, 2005: 2005: Another relatively quiet year for Hawaiian earthquakes Kilauea Eruption Status From Volcano Watch, January 19, 2006: During the past week, the number of earthquakes located beneath Kilauea remains at levels typical of the current eruption. Inflation of the summit continues. Eruptive activity at Pu`u `O`o also continues. On clear nights, glow is visible from several vents within the crater and on the southwest side of the cone. Lava is still flowing through the PKK lava tube from its source on the flank of Pu`u `O`o to the ocean, with scattered surface flows breaking out of the tube. Surface flows on the pali are visible at night (weather permitting) from the end of Chain of Craters Road. As of January 19, lava is entering the ocean at East Lae`apuki, in Hawai`i Volcanoes National Park. The active lava bench continues to regrow following the major collapse of November 28. Access to the ocean entry and the surrounding area remains closed, due to significant hazards. If you visit the eruption site, check with the rangers for current updates, and remember to carry lots of water when venturing out onto the flow field. There were two earthquakes beneath Hawai`i Island reported felt within the past week. A magnitude-3.6 earthquake occurred at 11:04 p.m. on Saturday, January 14, and was located 7 km (5 miles) southeast of Hualalai summit at a depth of 28 km (17 miles). A magnitude-4.7 earthquake occurred at 4:05 p.m. on Wednesday, January 18, and was located 16 km (10 miles) offshore and east of Na`alehu at a depth of 40 km (25 miles). Mauna Loa is not erupting. During the past week, the count of earthquakes located beneath the volcano remains at low levels. Inflation continues, but at a slower rate since early October 2005. Visit our web site (hvo.wr.usgs.gov) for daily volcano updates and nearly real-time Hawai`i earthquake information. For maps, photographs, and more current information see Kilauea's eruption updatepage . Visit The Hawaii Center for Volcanology for captivating eruptive photos and a history of the eruption. The Volcano Watch Archive Search Text to Search For: Boolean: AND OR Case Insensitive Sensitive || 1994 || 1995 || 1996 || 1997 || 1998 || 1999 || 2000 || 2001 || 2002 || 2003 || 2004 || 2005 || Other articles || USGS, HVO would like to thank Gerard Fryer at SOEST for doing a great job posting, archiving, and maintaining our Volcano Watch articles on their website from December 30, 1994 through March 6, 1998. The URL of this page is http://hvo.wr.usgs.gov/volcanowatch/ Contact: hvowebmaster@usgs.gov Updated: January 23, 2006 (pnf)