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Staff and students from across RMIT have been contributing their thoughts to #ShapeRMIT in a series of events.
BONUS V 3 ON LEGACY ONLY
SKIN CURRENTLY IN WEEKEND SALE .
SHOWN ON EON (LITE) HEAD .
OBVIOUSLY WILL WORK ON THE FULL VERSION AS WELL oO
marketplace.secondlife.com/p/SHAPEshifters-KEVIN-V1V2-SHA...
It's the Shape Maker texture created in the Filter Forge plugin. It can be seamless tiled and rendered in any resolution without loosing details.
You can see the presets and download this texture for free on the Filter Forge site here — www.filterforge.com/filters/11648.html (created by vwg)
To use this texture download Filter Forge 30-day trial version for free here — www.filterforge.com/download/
This is a center variation to the one I made several years back. Here actually what the center should've been to begin with (just kidding). Both are good. (I also unsunk 4 corners from the center to give even more shape.. not shown in photo). Diagrams coming soon hopefully. Updated design by me 12/2018.
•Shapes midriff, hips, thighs and rear for a seamless look
•Lifts your rear
•Removable straps attach to any bra
•Legband-free design eliminates bulging at the thighs
•Cotton double gusset for comfort and ease when nature calls
•80% Nylon, 18% Spandex/Elastane, 2% Cotton
Tummy Control Shapers
Miss Moly Latex Body Shaper Girdle Waist Trainer Steel Boned Modeling Belt Tummy Control Shapers Slimming Shapewear Cincher
Description
Specification
Color:Black/Beige
Material:100%Latex
Underwear Size:S/M/L/XL/2L/3XL/4XL/5XL/6XL
Ocassion:Everday/Gym/Train/Sport/Yoga
Feature:Sweat sport corset workout sport ,activity
Bones:7 Sprial Steel Bones
Warehouse Location:China,United States
Our Advantage:
1. High quality Clothing
2. Faster and Safer shipping methods.
3. Fast Parpare in 48 hours
4. Sending from China and United States warehouse.
5. Professional team serve you.
Size Chart
Tag Size
Waist Size
Front Length
Back Length
-
inch
cm
inch
cm
inch
cm
S
27"~29"
69~74
12"
30.5
10 5/8"
27.0
M
29"~31"
74~79
12"
30.5
10 5/8"
27.0
L
31"~33"
79~84
12"
30.5
10 5/8"
27.0
XL
33"~35"
84~89
12"
30.5
10 5/8"
27.0
2XL
35"~37"
89~94
12"
30.5
10 5/8"
27.0
3XL
37"~39"
94~99
12 3/8"
31.5
11"
28.0
4XL
39"~41"
99~104
12 3/8"
31.5
11"
28.0
5XL
41"~43"
104~109
12 3/8"
31.5
11"
28.0
6XL
43"~45"
109~114
12 3/8"
31.5
11"
28.0
Size
United States Size
United Kingdom Size
Germany Size
France Szie
Spain Size
Italy Size
S
2.0
6~8
32~34
34~36
34~36
38~40
M
6.0
10.0
36.0
36~38
36~38
40~42
L
8.0
12.0
38.0
40.0
40.0
44.0
XL
12.0
14.0
40~42
42.0
42.0
46.0
2XL
16.0
16~18
44.0
46.0
46.0
50.0
3XL
18~20 (14W~16W)
20.0
48.0
50.0
50.0
54.0
4XL
18W~20W
22.
Hạ Long Bay (Vietnamese: Vịnh Hạ Long, About this sound listen, literally: "descending dragon bay") is a UNESCO World Heritage Site, and a popular travel destination, in Quảng Ninh Province, Vietnam. Administratively, the bay belongs to Hạ Long City, Cẩm Phả town, and the part of Vân Đồn District. The bay features thousands of limestone karsts and isles in various sizes and shapes. Hạ Long Bay is a center of a larger zone which includes Bái Tử Long bay to the northeast, and Cát Bà islands to the southwest. These larger zones share similar geological, geographical, geomorphological, climate, and cultural characters.
Hạ Long Bay has an area of around 1,553 km2, including 1,960–2,000 islets, most of which are limestone. The core of the bay has an area of 334 km2 with a high density of 775 islets. The limestone in this bay has gone through 500 million years of formation in different conditions and environments. The evolution of the karst in this bay has taken 20 million years under the impact of the tropical wet climate. The geo-diversity of the environment in the area has created biodiversity, including a tropical evergreen biosystem, oceanic and sea shore biosystem. Hạ Long Bay is home to 14 endemic floral species and 60 endemic faunal species.
Historical research surveys have shown the presence of prehistorical human beings in this area tens of thousands years ago. The successive ancient cultures are the Soi Nhụ culture around 18,000–7000 BC, the Cái Bèo culture 7000–5000 BC and the Hạ Long culture 5,000–3,500 years ago. Hạ Long Bay also marked important events in the history of Vietnam with many artifacts found in Bài Thơ Mount, Đầu Gỗ Cave, Bãi Cháy.
500 years ago, Nguyễn Trãi praised the beauty of Hạ Long Bay in his verse Lộ nhập Vân Đồn, in which he called it "rock wonder in the sky".[8] In 1962, the Ministry of Culture, Sports and Tourism of North Vietnam listed Hạ Long Bay in the National Relics and Landscapes publication. In 1994, the core zone of Hạ Long Bay was listed by UNESCO as a World Heritage Site according to criterion vii, and listed for a second time according to criterion viii.
ETYMOLOGY
The name Hạ Long is derived from the Sino-Vietnamese 下龍, meaning "descending dragon".
Before 19th century, the name Halong Bay had not been recorded in the old books of our country. It has been called An Bang, Luc Thuy, Van Don... Late 19th century, the name Halong Bay has appeared on the Maritime map of France. "Haiphong News" published in French, has reported: " Dragon appears on Halong Bay". The story can be summarized as follows: In 1898, lieutenant Lagoredin captain of Avalangso met a couple of giant sea snake on Halong Bay three times. Not only the lieutenant but also many other sailors saw those species. The European thought that those animals looked like Asian dragon. Maybe the appearance of strange animals led to the name of Quang Ninh sea area today: Halong Bay
According to local legend, when Vietnam had just started to develop into a country, they had to fight against invaders. To assist the Vietnamese in defending their country, the gods sent a family of dragons as protectors. This family of dragons began spitting out jewels and jade. These jewels turned into the islands and islets dotting the bay, linking together to form a great wall against the invaders. Under magics, numerous rock mountains abruptly appeared on the sea, ahead of invaders' ships; the forward ships struck the rocks and each other. After winning the battle, the dragons were interested in peaceful sightseeing of the Earth, and then decided to live in this bay. The place where the mother dragon descended was named Hạ Long, the place where the dragon's children attended upon their mother was called Bái Tử Long island (Bái: attend upon, Tử: children, Long: dragon), and the place where the dragon's children wriggled their tails violently was called Bạch Long Vỹ island (Bạch: white-color of the foam made when Dragon's children wriggled, Long: dragon, Vỹ: tail), present day Trà Cổ peninsula, Móng Cái.
OVERVIEW
The bay consists of a dense cluster of some 1,600 limestone monolithic islands each topped with thick jungle vegetation, rising spectacularly from the ocean. Several of the islands are hollow, with enormous caves. Hang Đầu Gỗ (Wooden stakes cave) is the largest grotto in the Hạ Long area. French tourists visited in the late 19th century, and named the cave Grotte des Merveilles. Its three large chambers contain large numerous stalactites and stalagmites (as well as 19th century French graffiti). There are two bigger islands, Tuần Châu and Cát Bà, that have permanent inhabitants, as well as tourist facilities including hotels and beaches. There are a number of beautiful beaches on the smaller islands.
A community of around 1,600 people live on Hạ Long Bay in four fishing villages: Cửa Vạn, Ba Hang, Cống Tàu and Vông Viêng in Hùng Thắng commune, Hạ Long city. They live on floating houses and are sustained through fishing and marine aquaculture (cultivating marine biota), plying the shallow waters for 200 species of fish and 450 different kinds of mollusks. Many of the islands have acquired their names as a result of interpretation of their unusual shapes. Such names include Voi Islet (elephant), Ga Choi Islet (fighting cock), Khi Islet (monkey), and Mai Nha Islet (roof). 989 of the islands have been given names. Birds and animals including bantams, antelopes, monkeys, and lizard also live on some of the islands.
Almost all these islands are as individual towers in a classic fenglin landscape with heights from 50m to 100m, and height/width ratios of up to about six.
Another specific feature of Halong Bay is the abundance of lakes inside the limestone islands. For example, Dau Be island has six enclosed lakes. All these island lakes occupy drowned dolines within fengcong karst.
LOCATION
Hạ Long Bay is located in northeastern Vietnam, from E106°56' to E107°37' and from N20°43' to N21°09'. The bay stretches from Yên Hưng district, past Hạ Long city, Cẩm Phả town to Vân Đồn District, bordered on the south and southeast by the Gulf of Tonkin, on the north by China, and on the west and southwest by Cát Bà Island. The bay has a 120 km long coastline and is approximately 1,553 km² in size with about 2,000 islets. The area designated by UNESCO as the World Natural Heritage Site incorporates 434 km² with 775 islets, of which the core zone is delimited by 69 points: Đầu Gỗ island on the west, Ba Hầm lake on the south and Cống Tây island on the east. The protected area is from the Cái Dăm petrol store to Quang Hanh commune, Cẩm Phả town and the surrounding zone.
CLIMATE
The climate of the bay is tropical, wet, sea islands, with two seasons: hot and moist summer, and dry and cold winter. The average temperature is from 15 °C- 25 °C, and annual rainfall is between 2 meters and 2.2 meters. Hạ Long Bay has the typical diurnal tide system (tide amplitude ranges from 3.5-4m). The salinity is from 31 to 34.5MT in the dry season and lower in the rainy season.
HISTORY
SOI NHU CULTURE (16,000–5000 BC)
Located in Hạ Long and Bái Tử Long are archaeological sites such as Mê Cung and Thiên Long. There are remains from mounds of mountain shellfish (Cyclophorus), spring shellfish (Melania), some fresh water mollusc and some rudimentary labour tools. The main way of life of Soi Nhụ's inhabitants included catching fish and shellfish, collecting fruits and digging for bulbs and roots. Their living environment was a coastal area unlike other Vietnamese cultures, for example, like those found in Hòa Bình and Bắc Sơn.
CAI BEO CULTURE (5000–3000 BC)
Located in Hạ Long and Cát Bà island, its inhabitants developed to the level of sea exploitation. Cái Bèo culture is a link between Soi Nhụ culture and Hạ Long culture.
FEUDAL PERIOD
History shows that Hạ Long Bay was the setting for local naval battles against Vietnam's coastal neighbors. On three occasions, in the labyrinth of channels in Bạch Đằng River near the islands, the Vietnamese army stopped the Chinese from landing. In 1288, General Trần Hưng Đạo stopped Mongol ships from sailing up the nearby Bạch Đằng River by placing steel-tipped wooden stakes at high tide, sinking the Mongol Kublai Khan's fleet.
During the Vietnam War, many of the channels between the islands were heavily mined by the United States navy, some of which pose a threat to shipping to this day.
GEOLOGY AND GEOMORPHOLOGY
In 2000, the UNESCO’s World Heritage Committee has inscribed the Hạ Long Bay in the World Heritage List according to its outstanding examples representing major stages of the Earth’s history and its original limestone karstic geomorphologic features. The Hạ Long Bay and its adjacent areas consist of a part of the Sino-Vietnamese composite terrane having its development history from pre-Cambrian up to present day. During Phanerozoic, terrigenous, volcanogenic and cherty-carbonate sediments containing in abundance graptolites, brachiopods, fishes, corals, foraminiferas, radiolarias, bivalves and flora, separated one from another by 10 stratigraphic gaps, but the boundary between Devonian and Carboniferous has been considered as continuous. The limestone karstic geomorphology of the bay was developed since Miocene, especially the cone-shaped hills (fengcong), or isolated high limestone karst towers (fenglin) with many remnants of old phreatic caves, old karstic foot caves, marine notch caves form magnificent limestone karst landforms as unique on the world. The Quaternary geology was developed through 5 cycles with the intercalation of marine and continental environments. The present Hạ Long Bay, in fact, appeared after the Middle Holocene maximum transgression, leaving ultimate zone of lateral undercutting in the limestone cliffs bearing many shells of oysters, having the 14C age as 2280 to >40,000 y. BP. Geological resources are abundant: anthracite, lignite, oil shale, petroleum, phosphate, limestone and cement additives, kaolin, silica sand, dolomite, quartzite of exogenous origin, and antimony, mercury of hydrothermal origin. Besides, there still are surface water, groundwater and thermal mineral water on the shore of the Hạ Long - Bái Tử Long Bays and other environmental resources.
In terms of marine geology, this area is recorded as an especially coastal sedimentary environment. In the alkaline seawater environment, the chemical denudation process of calcium carbonate proceeds rapidly, creating wide, strangely shaped marine notches.
The bottom surface sediments are various from clay mud to sand, however, silty mud and clay mud are dominated in distribution. Especially, the carbonate materials originated from organisms make up from 60-65% sedimentary content. The surface sediments of coral reefs are mainly sand and pebbles of which the carbonate materials occupy for more than 90%. The intertidal zone sediments are various from clay mud to sand and gravel depending to distinguished sedimentary environments such as mangrove marshes, tidal flats, beaches etc. At the small, but wonderfully beautiful beaches, the sand sediments may be dominated quartz or carbonate materials.
The sediment layers of intertidal zone, the upper sea bed with a plain surface conserving ancient rivers, systems of caves and it's sediments, traces of ancient marine action forming distinctive notches, beaches and marine terraces, mangrove swamps are important evidence of geological events and processes taking place during Quaternary.
HISTORY OF TECTONICS
Hạ Long Bay has experienced at least 500 million years in various geological states of orogeny, marine transgression and marine regression. During the Ordovician and Silurian periods (500-410 million years ago), Hạ Long Bay was deep sea. During the Carboniferous and Permian periods (340-250 million years ago), Hạ Long Bay was at shallow sea level.
The dominated uplift movement of neotectonic and recent tectonic influenced deeply on topography of this area, and the present landscape of sea-islands was formed around 7 or 8 thousand years ago by the sea invasion during Holocene transgression begun at about 17-18 thousand years ago. Particularly from the Holocene time, from about 11,000 years ago Cat Ba - Hạ Long area has much archaeological evidence connecting variations in sea levels with the development of ancient cultures such as the Soi Nhu and Ha Long cultures.
KARST GEOMORPHOLOGY VALUE
Due to a simultaneous combination of ideal factors such as thick, pale, grey, and strong limestone layers, which are formed by fine-grained materials; hot and moist climate and slow tectonic process as a whole; Hạ Long Bay has had a complete karst evolution for 20 million years. There are many types of karst topography in the bay, such as karst field.
Hạ Long Bay is a mature karst landscape developed during a warm, wet, tropical climate. The sequence of stages in the evolution of a karst landscape over a period of 20 million years requires a combination of several distinct elements including a massive thickness of limestone, a hot wet climate and slow overall tectonic up lift. The process of karst formation is divided into five stage is the formation of the distinctive do line karst. This is followed by the development of fengcong karst can be seen in the groups of hills on Bo Hon and Dau Be Inland. These cones with sloping side average 100m in height with the tallest exceeding 200m. Fenglin karst is characterised by steep separate towers. The hundreds of rocky islands with form the beautiful and famous landscape of the Bay are the individual towers of a classic Fenglin landscape where the intervening plains have been submerged by the sea. Most towers reach a height of between 50 and 100m with a height to width ratio of about 6. The karst dolines were flooded by the sea becoming the abundance of lakes that lie within the limestone islands. For example, Dau Be island at the mouth of the Bay has six enclosed lakes including those of the Ba Ham lakes lying within its fencong karst. The Bay contains examples of the landscape elements of fengcong, fenglin and karst plain. These are not separate evolutionary stages but the result of natural non – uniform processes in the denudation of a large mass of limestone. Marine erosion created the notches which in some places have been enlarged into caves. The marine notch is a feature of limestone coastline but, in Ha Long Bay, it has created the mature landscape.
Within Ha Long Bay, the main accessible caves are the older passages that survive from the time when the karst was evolving though its various stages of fengcong and fenglin. Three main types of caves can be recognized in the limestone islands (Waltham, T. 1998):
Remnants of old phreatic caves
Old karstic foot caves
Marine notch caves
The first group of caves is old phreatic caves which include Sung Sot, Tam Cung, Lau Dai, Thien Cung, Dau Go, Hoang Long, Thien Long. Nowadays, these caves lie at various high levels. Sung Sot cave is on Bo Hon island. From its truncated entrance chambers on allege high on the cliff, a passage of more that 10m high and wide descends to the south. Tam Cung is a large phreatic fissure cave that developed in the bedding planes of the limestone dividing the fissure cave into three chambers. Lau Dai is a cave with a complex of passages extending over 300m opening on the south side of Con Ngua island. Thien Cung and Dau Go are remnants of the same old cave system. They both survive in the northern part of Dau Go island at between 20 and 50m above sea level. Thien Cung has one large chamber more that 100m long, blocked at its ends and almost subdivided into smaller chambers by massive wall of stalactites and stalagmites. Dau Go is a single large tunnel descending along a major set of fractures to a massive choke.
The second group of caves is the old karstic foot caves which include Trinh Lu, Bo Nau, Tien Ong and Trong caves. Foot caves are a ubiquitous feature of karst landscapes which have reached a stage of widespread lateral undercutting at base level. They may extend back into maze caves of stream caves draining from larger cave systems within the limestone. They are distinguished by the main elements of their passages being close to the horizontal and are commonly related to denuded or accumulated terraces at the old base levels. Trinh Nu, which is one of the larger foot caves in Ha Long Bay with its ceiling at about 12m above sea level and about 80m in length, was developed in multiple stages. Bo Nau, a horizontal cave containing old stalactite deposits, cuts across the 25o dip of the bedding plane.
The third group is the marine notch caves that are a special feature of the karst of Ha Long Bay. The dissolution process of sea water acting on the limestone and erosion by wave action crates notches at the base of the cliffs. In advantageous conditions, dissolution of the limestone allows the cliff notches to be steadily deepened and extended into caves. Many of these at sea level extend right though the limestone hills into drowned dolines which are now tidal lakes.
A distinguishing feature of marine notch caves is an absolutely smooth and horizontal ceiling cut through the limestone. Some marine notch caves had been not formed at present sea level, but old sea levels related to sea level changes in Holocene transgression, event to Pleistocene sea levels. Some of them passed preserved the development of old karstic foot cave in mainland environment or preserved the remnants of older phreatic caves. One of the most unusual features of Ha Long Bay is the Bo Ham lake group of hidden lakes and their connecting tunnel – notch caves in Dau Be island. From the island’s perimeter cliff a cave, 10m wide at water level and curving so that it is almost completely dark, extends about 150m to Lake 1. Luon cave is on Bo Hon island and extends 50m though to an enclosed tidal lake. It has a massive stalactite hanging 2m down and truncated at the modern tidal level. It has passed though many stages in its formation.
The karst landscape of Ha Long Bay is of international significance and of fundamental importance to the science of geomorphology. The fenglin tower karst, which is the type present in much of Ha Long Bay, is the most extreme form of limestone landscape development. If these karst landscapes are broadly compared in terms of their height, steepness and number of their limestone towers, Ha Long Bay is probably second in the entire world only to Yangshou, in China. However, Ha Long Bay ha also been invaded by the sea so that the geomorphology of its limestone is lands are, at least in part, the consequence of marine erosion. The marine invasion distinguishes Ha Long Bay and makes it unique in the world. There are other areas of submerged karst towers which were invaded by the sea, but none is as extensive as Ha Long Bay.
TIMELINE OF GEOLOGIC EVOLUTION
Some of the most remarkable geological events in Hạ Long Bay's history have occurred in the last 1,000 years, include the advance of the sea, the raising of the bay area, strong erosion that has formed coral, and, pure blue and heavily salted water. This process of erosion by seawater has deeply engraved the stone, contributing to its fantastic beauty. Present-day Hạ Long Bay is the result of this long process of geological evolution that has been influenced by so many factors.
Due to all these factors, tourists visiting Hạ Long Bay are not only treated to one of the natural wonders of the world, but also to a precious geological museum that has been naturally preserved in the open air for the last 300 million years.
ECOLOGY
Halong Bay is host to two ecosystems: a tropical, moist, evergreen rainforest ecosystem; and a marine and coastal ecosystem. The bay is home to seven endemic species: Livistona halongensis, Impatiens halongensis, Chirita halongensis, Chirita hiepii, Chirita modesta, Paraboea halongensis and Alpinia calcicola.
The many islands that dot the bay are home to a great many other species, including (but likely not limited to): 477 magnoliales, 12 pteris, 20 salt marsh flora; and 4 amphibia, 10 reptilia, 40 aves, and 4 mammalia.
Common aquatic species found in the bay include: cuttlefish (mực); oyster (hào); cyclinae (ngán); prawns (penaeidea (tôm he), panulirus (tôm hùm), parapenaeopsis (tôm sắt), etc.); sipunculoideas (sá sùng); nerita (ốc đĩa); charonia tritonis (ốc tù và); and cà sáy.
ENVIRONMENTAL DAAGE
With an increasing tourist trade, mangroves and seagrass beds have been cleared and jetties and wharves have been built for tourist boats.
Game fishing, often near coral reefs, is threatening many endangered species of fish.
Local government and businesses are aware of problems and many measures have been taken to minimize tourism affect to the bay environment for sustainable economic growth like introducing eco friendly tours and introducing tight waste control on resorts.
AWARDS AND DESIGNATIONS
In 1962, the Vietnam Ministry of Culture, Sport and Tourism designated Hạ Long Bay a 'Renowned National Landscape Monument'.
Hạ Long Bay was first listed as a UNESCO World Heritage Site in 1994, in recognition of its outstanding, universal aesthetic value. In 2000 the World Heritage Committee additionally recognised Hạ Long Bay for its outstanding geological and geomorphological value, and its World Heritage Listing was updated.
In October 2011, World Monuments Fund included the bay on the 2012 World Monuments Watch, citing tourism pressures and associated development as threats to the site that must be addressed. The goal of Watch-listing is to promote strategies of responsible heritage-driven development for a sustainable future.
In 2012, New 7 Wonders Foundation officially named Halong Bay as one of New Seven Natural Wonders of the world.
Hạ Long Bay is also a member of the Club of the Most Beautiful Bays of the World.
IN LITERATURE
In writings about Hạ Long Bay, the following Vietnamese writers said:
Nguyễn Trãi: "This wonder is ground raising up into the middle of the high sky".
Xuân Diệu: "Here is the unfinished works of the Beings...Here is the stones which the Giant played and threw away".
Nguyên Ngọc: "...to form this first- rate wonder, nature only uses: Stone and Water...There are just only two materials themselves chosen from as much as materials, in order to write, to draw, to sculpture, to create everything...It is quite possible that here is the image of the future world".
Ho Chi Minh: "It is the wonder that one cannot impart to others".
Phạm Văn Đồng: "Is it one scenery or many sceneries? Is it the scenery in the world or somewhere?".
Nguyễn Tuân: "Only mountains accept to be old, but Hạ Long sea and wave are young for ever".
Huy Cận: "Night breathes, stars wave Hạ Long's water".
Chế Lan Viên:
"Hạ Long, Bái Tử Long- Dragons were hidden, only stones still remain
On the moonlight nights, stones meditate as men do..."
Lord Trịnh Cương overflowed with emotion: "Mountains are glistened by water shadow, water spills all over the sky".
ANCIENT TALES
Hạ Long bay's inhabitants have developed numerous tales explaining names given to various isles and caves in the bay.
Đầu Gỗ cave (literally: "the end of wooden bars" cave): these wooden bars in this cave are the remnants of sharped wooden columns built under the water level by the order of Trần Hưng Đạo commander in order to sink Mongolian invaders' ships in the 13th century.
Kim Quy cave (literally: "Golden Turtle" cave): it is told that the Golden Turtle swam toward the Eastern Sea (international name: South China Sea) after returning the holy sword which had assisted King Lê Thái Tổ in the combat against Ming invaders from China. Next, with the approval of the Sea King, Golden Turtle continued to fight against monsters in this marine area. The turtle became exhausted and died in a cave. Consequently, the cave was named after the Golden Turtle.
Con Cóc isle (literally: Frog isle): is a frog- like isle. According to ancient tales, in a year of severe drought, a frog directed all animals to the Heaven and protested against the God. They demonstrated in favour of making rain. As a result, the God must accept the frog as his uncle. Since then, whenever frogs grind their teeth, the God has to pour water down the ground.
WIKIPEDIA
22nd Annual Christian Harmony Sing held at the John C. Campbell Folk School in Brasstown, NC on Saturday, July 12, 2014.
Key to Lawrence Livermore National Laboratory shape-memory-polymer (SMP) foam technology is its compressibility. A 10-millimeter-diameter spherical SMP foam plug is shown in its primary (original) shape. [More information]
While lingering at the Point of the Arches, one gets to see so many different lines and odd shapes within this tortured landscape. Waves and very powerful winter storms erode away this once fully connected land mass to reform these pillars of interest. The fact that trees grow on these remote and desolate sea stacks is both curious and amazing.
Facilitated by: Raissa Kanku (Community Specialist, Africa, Global Shapers Community), Sophia Otoo (Selections, Community, and Impact Specialist, Schwab Foundation for Social Entrepreneurship) With: Chido Munyati (Head of Regional Agenda, Africa), Wanjuhi Njoroge (Global Shapers Foundation Board), Rene Parker (CEO, RLabs) speaking in the Intergenerational Approaches to Local Realities in Sub-Saharan Africa at the Global Shapers Annual Summit 2023 in Geneva, Switzerland, 16 June 2023. World Economic Forum Headquarters, Mont Blanc A and B. Copyright: World Economic Forum/Marc Bader
To view more my images of the Aquilegia, please click "here"!
Aquilegia (common names: granny's bonnet or columbine) is a genus of about 60-70 species of perennial plants that are found in meadows, woodlands, and at higher altitudes throughout the Northern Hemisphere, known for the spurred petals of their flowers. The genus name Aquilegia is derived from the Latin word for eagle (aquila), because the shape of the flower petals, which are said to resemble an eagle's claw. The common name "columbine" comes from the Latin for "dove", due to the resemblance of the inverted flower to five doves clustered together. The fruit is a follicle. the five points that stick out further than the petals are the calyx (chalis). Columbines are closely related to plants in the genera Actaea (baneberries) and Aconitum (wolfsbanes/monkshoods), which like Aquilegia produce cardiogenic toxins. They are used as food plants by some Lepidoptera (butterfly and moth) caterpillars. These are mainly of noctuid moths – noted for feeding on many poisonous plants without harm – such as Cabbage Moth (Mamestra brassicae), Dot Moth (Melanchra persicariae) and Mouse Moth (Amphipyra tragopoginis). The Engrailed (Ectropis crepuscularia), a geometer moth, also uses columbine as a larval foodplant. Plants in the Aquilegia genus are a major food source for Bombus hortorum, a species of bumblebee. Specifically, they have been found to forage on species of Aquilegia vulgaris in Belgium and Aquilegia chrysantha in North America and Belgium. The bees do not show any preference in color of the flowers. Columbine is a hardy perennial, which propagates by seed. It will grow to a height of 15 to 20 inches. It will grow in full sun; however, it prefers growing in partial shade and well drained soil, and is able to tolerate average soils and dry soil conditions. Columbine is rated at hardiness zone 3 in the USA so does not require mulching or protection in the winter. Large numbers of hybrids are available for the garden, since the European A. vulgaris was hybridized with other European and North American varieties. Aquilegia species are very interfertile, and will self-sow. Some varieties are short-lived so are better treated as biennials.
From Wikipedia, the free encyclopedia
This image: For more than a century, astronomers have categorized galaxies near and far, both by comparing their shapes by eye and precisely measuring their properties with data known as spectra. For example, Edwin Hubble created the Hubble Tuning Fork in 1926 to begin to sort the shapes and sizes of nearby galaxies, showing that many are spirals and ellipticals.
As telescopes’ instruments have become increasingly more sensitive, it is easier to more accurately classify their shapes. New data from the James Webb Space Telescope have added nuances to astronomers’ classifications. Since Webb observes in infrared light, many more extremely distant galaxies appear in its images. Plus, the images are finely detailed, allowing researchers to identify if there are additional areas of star formation – or confirm they aren’t present.
A team led by Viraj Pandya, a NASA Hubble Fellow at Columbia University in New York, recently analyzed hundreds of distant galaxies in Webb’s Cosmic Evolution Early Release Science (CEERS) Survey. CEERS intentionally covers much of the same area as the Hubble Space Telescope’s Extended Groth Strip, which was one of the five fields used to create the Cosmic Assembly Near-infrared Deep Extragalactic Legacy Survey (CANDELS). This allowed them to double-check Webb’s results where the telescopes’ observations overlap.
“Our analysis of Webb’s galaxies was very consistent with galaxies in the Hubble Space Telescope catalog,” Pandya confirmed. “Two sets of data allowed us to fully vet our models as we ran our analysis, and better understand and categorize galaxies that only Webb detected.” The team began their analysis by sorting the galaxies into broad classes based on similar characteristics. (They did not classify each galaxy’s individual appearance since that would require detailed information from data known as spectra.)
They found an array of odd shapes when the universe was 600 million to 6 billion years old. The galaxy shapes that dominate look flat and elongated, like pool noodles or surfboards. These two galaxy types make up approximately 50 to 80% of all the distant galaxies they studied – a surprise, since these shapes are rare closer to home.
Other galaxies Webb detected appear round but also flattened, like frisbees. The least populated category is made up of galaxies that are shaped like spheres or volleyballs.
Webb’s data also resolved a riddle that was introduced by the Hubble Space Telescope’s observations decades ago. Why do so many distant galaxies appear like long lines? Was there more to the galaxies that didn’t appear in its images? Webb answered this in short order: Hubble hasn’t missed anything.
“Webb confirmed what Hubble has long shown us, but in greater detail in infrared light,” Pandya said. “Their combined observations show that in the early universe, many more galaxies appear flat and elongated. This has profound implications, since we usually assume that galaxies like our own Milky Way started out as disks, but that may not be the case.”
Why do galaxies have such different shapes early in the history of the universe? This question remains unanswered for now, but research is underway to better understand how galaxies evolved over all of cosmic time.
Read more: www.nasa.gov/missions/webb/webb-shows-many-early-galaxies...
Credits: NASA, ESA, CSA, STScI, Steve Finkelstein (UT Austin), Micaela Bagley (UT Austin), Rebecca Larson (UT Austin)
Image description: In the far-left column are two galaxies that have been magnified. The top left galaxy appears circular and light pink with a slightly whiter central region, taking up less than one-sixth of the box. The bottom galaxy is elongated, stretching almost from top left to bottom right. It has a white line at the center that has a pink outline that transitions into bluish edges at far left and right. Thin lines from each magnified galaxy point to their appearances in the broader field. The top galaxy appears as a tiny dot at the upper center, and the bottom galaxy toward the left. Thousands of galaxies appear across most of this view, which is set against the black background of space. There are many overlapping objects at various distances. They include large, blue foreground stars, with Webb’s signature eight-pointed diffraction spikes, and white and pink spiral and elliptical galaxies. Numerous tiny red dots appear throughout the scene. This is a portion of a vast survey known as CEERS.
Agricultural activities have long been recognised as being a shaper of the rural landscape and environment which exist in Ireland today. Historically, farmers have engaged in protection of the land out of necessity to maintain their production capacity through generations. Our knowledge and appreciation of soils is continually growing however. The role of soils and the key functions they provide is increasingly being recognised and there is a new impetus from all soil users for enchanced protection of a key natural resource.
Critical to the successful management of our soil resource is knowledge on the location of our soils, and their associated properties. The Irish Soil Information System project has gathered together existing information and data from previous soil survey work in Ireland and augmented it with a new field campaign, leading to the production of a new national soil map at a scale of 1:250,000, as well as a collection of tools to access and interact with the data.
An extensive range of soil types (or series) have been identified in Ireland, each of them different in properties, with different environmental and agronomic responses. For each, the properties have been recorded in a database that can now be used to satisfy the information required both for soils management and effective policy implementation. Importantly the database can also be used to provide the public with the means to enquire and learn about the precious soil resources of Ireland. The following website provides a series of tools and descriptive information seeking to help all users engage with the soils information resource now available to us. (Provided by the Irish Soil Information System.)
For more information about the Soils of Ireland, visit;
gis.teagasc.ie/soils/index.php
and the sponsors...
A block plane and sandpaper remove the final bit of material on the outside (you will probably need to re-scribe the shape as the lines will have worn off.
Roll #2 was a cheap canister of Fujifilm 200 I picked up from my local Walmart. On something of a whim, I cross-processed it as black and white film. The result was interesting and definitely gave the scanner some convulsions (and the negatives are too dense to print), but there are some interesting effects here. The reduced contrast creates a bit of a surrealistic atmosphere to many of these frames, which I find interesting indeed.
3rd in a series of 4 enamel necklaces. these enamels were done with a combination of techniques. they have fine silver shapes in them and then i built up layers of colors by wet packing and then kiln firing. i kept sanding the colors back and adding more layers and patterns of color until i was happy with the forms and the surface was level with the silver. i was trying to achieve a very painterly effect. the silver work was done in my idea of an abstract/constructivist style. i deliberately melted wires and used them, made things a bit "raw".
NEW shape
・❥ Only for leLutka evo x Ceylon 3.1 bento head, others may look different.
・❥ Shape to Lara, Legacy, Freya, Gen x classic, curvy & Kupra, Reborn mesh body.
・❥ Style card & eyebrow sharp included.
・❥ Eyeliner & blushes >BONUS< !
・❥ Shop at Marketplace
・❥・CREDITS:
Jamila Dress from NiU
New Shape by Lou's Little Secrets
All my shapes are copy/mod to fit your needs using mesh body parts!!
Marketplace only store: marketplace.secondlife.com/stores/156364
After making this I was told that it is quite similar looking to the dee-lite pop video groove is in the heart. Based on stock by Taversia: taversia.deviantart.com/art/Lady-In-Red-18-192523732
Product Name: Shape Water Game
Product No: GW030
Size: 7mL
Pack: 1.2m× 0.6m× 0.6m
Weight: 25kg
Material: 0.9mm PVC
Cert: CE,EN14960,EN71
Contact Site:http://www.pangoinflatable.com/
Not just fit and finish, Pango make a second blower tube and hide it if not use. We make the two tubes on different of the bouncer so that could fit the power location. Looking down the road you will find you need a second inflation tube. We want to make sure clients could use the bouncer convenient.
Stronger Baffles
Baffles that are secured by a 840 denier material that provides the MAXIMUM strength of the internal baffling of every inflatables. This material upgrade is unmatched by anyone else in the industry. This material is key to the overall durability of the products we sell.
D Ring Expose
Take a close look at the construction of the "d" rings in the products we sell. A tether system is only as strong as its weakest link. Tether points on the inflatable are extremely durable. The "d" ring tethering System have been laboratory-tested and certified by Professional Engineers for use on all giant slides and all other types of inflatables.
Vinyl（PVCTarpaulin） Expose
At Pango Inflatable, the only products we sell are constructed from the finest coated vinyl. Unlike other vinyl producers, the Coated Vinyl are Lead-Free in addition to meeting the EN71 test by SGS. Lead-Free vinyl are a standard that has been that way since day one. Exposure to lead is dangerous to children. The products Pango Inflatable sell are safe from the effects of lead. As for durability, the materials are a weft inserted substrate, which makes any possible rips virtually impossible.
No Wax Surfaces
We provide removable sliding surfaces for every slides we made, While other only provide the normal vinyl, Inflatable vinyl is not naturally slippery, therefore, waxing has become a normal preparation for getting a slide ready for use. The removable sliding surface found the on the products we sell is a high polished urethane coating, which in turn reduces the need to wax.
Zipper with Flaps
Unlike others, Pango Inflatable sells products that are easy to use. For example, the deflation zipper utilizes a Velcro flap that covers the zipper, thus, less air is lost and zippers are not exposed to abrasion or mischief.
Blower Tube Strap
While most manufacturers tie their blower inflation tubes to the blower system, however, the products Pango Inflatable sells, utilizes a universal sleeve with a cinching Velcro strap. One- handed operation keeps the tube securely attached to the blower system.
Liquid Laminator
DWe do the Digital Printing in our factory, unlike most factory here in China, they do the printing outside and could not control the delivery time and the quality. igitally printed graphics are one thing, keeping those beautiful images durable as well scratch and fade resistant is quite another. Every digital image used within an inflatable sold by Pango Inflatable is clear-coated with a special liquid laminate that is vulcanized to the vinyl surface.
Finger-Safe Netting
Most bouncer manufacturers use 1" or 2" netting. A child bouncing can easily catch their fingers in that size of netting, thus serious injuries can happen. Only the Pango Inflatable could provide netting that even a small child's finger cannot penetrate. Yet, the netting is still transparent enough to allow for easy viewing.
Removable Covers
Virtually every area that your customers step, slide or climb upon is on a replaceable & easily removable vinyl cover. From climbing stairs, to entrance tunnel sleeves to sliding surfaces, Pango Inflatable only sells products that are designed for high-volume traffic.
Safety Door on Bouncers
Worried about children possibly falling out of a bouncer? Don't be. We got 3 points of reinforcement on the entrance of the bouncer which make the entrance very strong. Also we add the step outside the entrance following the AU and USA standards of jumping castle.
On-Staff Engineering and Designing
We do reinforce stitching at the fixion of D-ring. Four stitching line will share the tension of the bouncer. This made the D-ring last much longer and stronger. Other factory use other design of the fixion, but will not good for the tension sharing. Could find the differnce in the attached photos.
Cushion Designs
We do cushion between the wall and the base. When the kids bounce on the bouncer this parts bear most of the pressure, so this new design will make this parts much more strong and safety, while other factory only stitch to the base.
Now available at the Marketplace:
marketplace.secondlife.com/p/MACCUS-Enzel-Shape-Style-Car...
[Released a day later, as I made a few changes to it.]