The above map shows some of my completed island mapping projects. Each icon contains the name of the primary island associated with the project and a link to the post. Once all of my projects are posted, the map will be covered with icons. To productively use the map, zoom into a region of interest. Then select an icon.

Each of my maps is constructed of numerous layers of information. All of the layers are vector files. I will make these files available upon request. You are free to use them with certain restrictions - 1) Don't sell them. You can use them on research projects, post them to your website or things of that nature. If you aren't sure about the use of my maps, drop me a line and we can discuss your idea. 2) Give me credit when you use my vectors or images of my maps. Credit them to Peter Minton @ EVS-Islands

If I have the island vector file(s) and based upon your need, I will make them available. Images of my maps are yours to download and use, with the above restrictions applicable. Enjoy!

Thursday, May 04, 2006

Marotiri FP

Marotiri - Image

Marotiri - Landsat Image S-06-25_2000

Marotiri - Map

Marotiri - Marplot Map

Marotiri (aka Bass Rocks aka Ilots de Bass) is SE of Rapa. These four pinacle shaped rocks and seldom visited. However, there was a visit July 22, 1934 by a couple of scientists. They spent a few hours scouring these island. They gathered information on the flora and fauna found on this small points of land.

MOROTIRI (BASS ROCKS) AUSTRAL ISLANDS by F.R. Fosberg Smithsonian Institution

Morotiri or Bass Rocks is a small cluster of 4 rugged volcanic rocks and a number of stacks that form the southeast extremity of the Austral Island Group, in French Polynesia. They are located about 46 miles east by south of Rapa, at about 28S, 143 30W. As nothing of a general nature seems to have beenpublished on their natural history, it may be worthwhile to publish notes made on a short visit on July 22, 1934, when Harold St. John, Elwood C. Zimmerman and I landed on the largest of the rocks and collected what could be found and reached in a couple of hours of scrambling and climbing over guano-covered ledges and cliffs.

The highest of the rocks is about 100 m high and not much more than that wide, several times as long. The rocks were practically without a real covering of vegetation. A sparse growth made up of Cypems, Ridens, Diavia and Portulaca was present on the non-perpendicular slopes and ledges, luxuriant in favorable spots. In the crevices in the rocks Aspleniunz, Neplzrolepis, and Clzeilanthes formed tufts. Solanurn nigmm was present hereand there. Lyciurn was seen on the lowest slopes, and a prostrate Eupizovbia formed mats on one slope on one end of the island. A sterile rosette of Soncizus was seen.

Some of the rocks were sparsely covered with lichens. A sterile moss was occasional around seeps. These seeps were evidently highly charged with lime or some other substance that crystallized out around the cracks.

Under the plants and stones was a remarkably large fauna of insects, spiders, centipedes, and isopods. Of the last, 3 species occurred under stones and a species of Ligia ran around over rocks, collecting in numi>ersunder overhangingrocks.At least 1 species of centipede, 4 or 5 of spiders, 1 or 2 of ticks, 2 of mites, 1 of Lepisma, 1 of Machilis, 2 of Collenibola, 1 cricket, 1 or 2 of ants, 1 lygeid, 4 species of Rhynchogonus, and 1 other weevil all lived under stones and plants. Two or 3 kindsofflies and 2 of moths were seen flying. A louse fly (Ovevsia sp.?) was abundant on shearwaters.

Birds were more than abundant, but nearly all belonged to a species of gray tern and 2 or 3 of shearwater. A couple of white-tailed tropic birds were seen. The shearwaters were nesting and eggs and young were abundant on small ledges and between tufts of sedges. Burrowing would be difficult here.

The rock is composed of more or less bedded basalt, forming a high core in the center, and the two ends are capped with tilted beds of what is probably tuff (described as "apparently sedimentary rock" in my notes at the time).

No coral was seen. Encrusting calcareous algae colored the lower rocks. Non-calcareous algae were reasonably abundant but badly beaten to pieces by wave action. The waves, even at the "quiet" period of our visit, were several meters high, making landing hazardous, to say the least. Acorn barnacles and chitons were seen on the lower rocks.

Fish of many kinds were abundant in the area and many were caught while the ship cruised around the area near the rock while we worked.

(ARB-162:9-10).


This project took about 3-hours to complete. The reason it took so long was I spent an hour gathering information off of the internet about these islands. The article from ARB is an aged jewel. It is not often that people visit these very small places and study them with a scientist's eye.

Enjoy!

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Wednesday, May 03, 2006

Maps and RSGBIOTA

Let's discuss radio amateurs again. As stated a few posts ago, these hardy souls travel to islands throughout the world. Upon arrival they establish a transmitting and receiving station. Then they transmit and receive. The signals might be voice or even morse code. IOTA (Islands on the Air) awards are piled up for every two-way contact that is made and validated (QSL card). There are folks out there that have 1,000's of these contacts. IOTA has between 18,000 to 20,000 members. Now for the mapping part. They venture to some pretty lonely spots, places with poor maps for advanced planning. Some entrepreneurial soul out there should supply the teams visiting these distant islands with maps and images. And they ought to do it for free! Hey, that's what I'm doing. Way to go, me!

RSGBIOTA RSGBIOTA Area
The above map covers a RSGBIOTA Area that encompasses the Central Kiribati Islands. It is called OC-043 T31. Currently I have not found these delineated on any maps. I think they should be mapped and those map files made available to radio amateurs. Does this sound like a fun project for some ambitious soul? If you are interested, and you have the time, and you have the hardware (computer), and you have the software (I can fix you up with map files), then you could bring this project to life. Somebody out there would love to do this . . . right? OT: Special Topic

Iles Moucha DJ

Moucha Islands - Image Moucha Islands - Image (N-38-10_2000) Moucha Islands - Map Moucha Islands - Map
Moucha Islands consists of a group of small islands located approximately 11-km NNW of Djibouti City in the country of Djibouti. The island to the west is called Maskali. The larger island is called Moucha. The islands are sparsely covered with scrub vegetation. small groves of non-native trees and mangroves. The islands are frequented by tourists that, after making a 1/2 hour boat trip from Djibouti City, dive on the extensive reefs surrounding the islands. The map files created, cover the shoreline, reefs and some vegetation (trees and mangroves). The mapping took about 2-hours from start to finish. OC: Indian

Tuesday, May 02, 2006

If All The World Were Imaged at 1-Meter.

Nisos Mykonos - Image Detail ETM An Ill-Defined Feature (Landsat ETM+)
Nisos Mykonos - Image Detail Ikonos The Same Feature at 1-Meter (Ikonos)
It would be so easy to become discouraged in my quest to map the world's shorelines using Landsat ETM+ 2000 imagery when one views the above comparison. That fuzzy blob in the first image (Landsat ETM+) was initially mapped, by me, as an unknown feature just offshore. The straight lines and the faint connection to the shore suggested some sort of docking facility. The same feature at 1-meter resolution is easily discernable is a docking facility with numerous ships and boats scattered about. Okay, 1-meter resolution is great, but it isn't freely available like Landsat ETM+ is. For shoreline work the 1-meter resolution does such a great job at illuminating all features both above and below water that it creates mapping decision problems galore. It does such a great job that the decisions as to what to map become magnified to an awesome level. My simple decisions - "Where is the shoreline? Is that a rock or a pier? Is that feature underwater or above water?" - become much more complex. Working by myself, as I do, little mapping would be finished. I would still be pondering my first island and trying to determine the most precise line of information to digitize. Don't get me wrong. I love 1-meter resolution imagery. I think it is cool to see the exquisite details that this sort of imagery gives you. However, when you are making shoreline maps that are intended to improve upon 1:250,000 scale existing shorelines and you try doing that with 1-meter imagery - that mapping becomes too complex, expensive and time-consuming for a 1-man operation. Others might be able to use 1-meter imagery to make maps , with unlimited resources and money, but that isn't me. My mapping is done in my den on my Sony Vaio viewing a 17-inch flat screen. I use a wireless mouse to trace digitized lines from on-screen imagery. I listen to classical music as I map. Sometimes I map and watch a baseball game (Go Padres!). All of the Landsat ETM+ 2000 imagery of all of the world's shorelines is either on my hard drive or on DVD's in a storage case resting beside my workstation (desk). I can greatly improve on the 1:250,000 shorelines that are currently available. In fact the United States shoreline is mapped at 1:70,000 and my maps are able to either match or improve upon these shorelines as well. Yes, 1-meter resolution imagery is great for many viewing and mapping needs. But not for my project. Landsat ETM+ at 14.5-meter resolution (depending on which continent you are viewing) is just fine for me. Hopefully, for you as well. Enjoy my maps! OT: Images

Nisos Dilos GR

Nisos Dilos - Image Nisos Dilos - Image (N-35-35_2000)
Nisos Dilos - Map Nisos Dilos - Map
The island of Nisos Dilos (aka Delos Island) is the navel of Ancient Greece. I believe it is reputed to be the birthplace of Apollo. The entire island is a archeological preserve. One can make day trips to the island and explore the temples and ruins. I have to go to school now and will add research information when I get a break during the day. The kids will not wait, but this post will. Have a nice day! SE: Mediterranean

Monday, May 01, 2006

Oeno Atoll PC

Oeno Atoll - Image Oeno Atoll - Image (S-09-20_2000) Oeno Atoll - Map Oeno Atoll - Map
Oeno Atoll (23˚56'S., 130˚44'W.) is a low and dangerous atoll; the shallow lagoon is completely surrounded by the coral reef. Near the center of the atoll there is a large island covered with trees; Sandy Island lies in the center of the N part of the reef. The N ends of both islets were being eroded, and the S end of Sandy Island and the E extremity of the center islet were extending. Two towers, each 24m high and about 1 mile apart, stand on the reef.
I haven't used Sailing Directions for island information in a long time. This atoll does have an excellent source of information. It is the Pitcairn Islands Study Center located at Pacific Union College. This 7th Day Adventist college is located in Angwin CA. The Pitcairn islanders practice this religion. If you are interested in the Pitcairn Islands this really is a wonderful site. Enjoy! OC: Pacific

Henderson Island PC

Henderson Island - Image Henderson Island - Image (S-09-20_2000)
Henderson Island - Map Henderson Island - Map
Henderson Island is an uninhabited uplifted coral island in the south Pacific Ocean, annexed to the Pitcairn Islands colony in 1902. It has an area of twelve square miles (31 km²) and is 120 miles (193 km) northeast of Pitcairn at 24°22′ S 128°16′ W. It has been designated a World Heritage Site by the United Nations in 1988 because of its bird life and untouched phosphate reserves. The island itself is too small and steep for agriculture and has no fresh water.

Although Henderson is virtually uninhabitable, archaeological evidence suggests that it was inhabited by a small Polynesian permanent colony between the twelfth and fifteenth centuries (CE) until this group disappeared. The reasons for its disappearance are unknown, but are probably related to the similar disappearance of the Polynesians on Pitcairn Island, on whom the Hendersonians would have depended for many of the basics of life (the Pitcairn Polynesians may in turn have disappeared because of the decline of nearby Mangareva; thus, Henderson was at the end of a chain of small, dependent colonies).

Today, Henderson is rarely visited except by Pitcairners looking for wood. However, in 1957, a man lived the life of a castaway on the island for approximately two months, accompanied by a pet chimpanzee, apparently as a publicity stunt. He was eventually rescued by locals from Pitcairn. [1]

OC: Pacific

Greasemonkey, Script and Tags

This doesn't have much to do with maps, but it is nice to know. I use tags on my uploaded images in Flickr and in Technorati. However, I had not used them in my blog site. That is up until now. This site, A Consuming Experience, has a wonderful article on adding tags to your Blogger posts. Since I use Firefox 1.5 the download of a program called Greasemonkey and the addition of a script created this neat little box at the bottom of my posts that lets me add all of the tags I need once I have completed an entry. Read the article and install the "Append Tags" box and you can begin tagging your blog posts. OT: Special Topic

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Sunday, April 30, 2006

Peng-hu Tao (Southern Group) TW

Peng-hu Tao - Image Peng-hu Tao (Southern Group) - Image (N-50-20_2000)
Peng-hu Tao - Map Peng-hu Tao (Southern Group) - Map
Why this particular group of islands, you might ask. The shorelines were relatively simple in structure allowing me to digitize the islands within about 2-hours. When I compared them to my original files (3-years old) they matched perfectly. So, my fear that I had not digitized these islands 3-years ago was unfounded. I had done the map work and it had been done well. Now, about these islands, everything you might want to know about this Southern Group and the other islands within the entire group (64-islands at high tide, over 100-islands at low tide) is found at Penghu Islands web site. As I researched these islands I did come across a number of sites. They all talk about pristine waters and low islands that are a mecca for tourists. OC: Pacific

Taiwan TW

Taiwan - Image Taiwan - Image (N-51-20_2000; N-51-25_2000; N-50-20_2000)
I digitized the Taiwanese shoreline over 3-years ago. To digitize 2,300 km's of shoreline was a big task. I had great base imagery. The Landsat images were 98%+ cloud free and the shoreline was easily discernable. There was a large mudflat along the center western coast that was tough to digitize. The rest of the island was straight forward.
Taiwan - Map> Taiwan - Map
The map is a simple shoreline depiction. I briefly considered adding details, but realized that I would still be working on the map. I kept reminding myself that I wanted to create a quality shoreline map. And it is that.
Tai-pei City - Image Tai-pei City - Image (N-51-25_2000)
A long time ago (1973) my wife and daughter followed me to Taiwan. It was the greatest. I was fluent in Mandarin Chinese and thoroughly enjoyed the time spent on the island. We lived in a neighborhood north of the main city called Yang Ming Shan. It was an idyllic period. I recommend Tai-pei to any of you travellers. It is a city full of adventure. There is much to do and see and you are safe anytime night or day. Great Place!
Tai-pei City Area Shoreline - Map Tai-pei City Area Shoreline - Map
Shoreline maps aren't great when it comes to showing a vibrant city. They are not intended to do that. Shoreline maps show detailed representations of shorelines, and that it. Now you could add your own unique layers of information., Then the shoreline map has some punch to it. OC: Pacific

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