This is a strange one, and appears to have started once we upgraded to 8.4 from 8.3 - and set up pull request decoration (those were both done about the same time). It is only happening to one project. I noticed on Monday that one project had a high level of security hotspots. I looked at them, and was pretty sure they were ones I had marked off previously. They all had old creation dates. I went through and marked them all safe again. Yesterday morning, same thing. This morning, they are back again. None of them have anything in the Activity section showing they had ever been marked safe.
It looks like this started happening on 8/11, per logging we have that queries the API and captures the number of open bugs, hotspots, etc. per project. We updated to 8.4 on August 4, and started adding pull request decoration on 8/10.
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If you are observing this on the same branch, can you provide the commands you used when you performed that caused the Hotspots to reopen? Also, the scans you performed in CI when they did not reappear?
I suspect that your scans may have inconsistencies between what is checked out on the file system and what branch/PR parameters are being applied. I suggest you review these and make sure everything is consistent.
Note: the things I keep having the mark off, these were things I marked off months ago. They had been off the report for a long time. They started re-appearing after we added PR scans triggered by Azure DevOps.
Also, looking at the database, I believe it really is recreating them. I grabbed the kee for a hotspot I know I previously marked off, then queried the issues table. I then queried for issues with the same component_uuid, project_uuid, issue_type and rule_uuid. There are 12 of them so far. The only difference between the open and closed ones (besides the obvious ones like kee, created_at, issue_close_date, etc.) are:
Some more information. There is now a 13th instance of this hotspot. The previous one flipped from reviewed/safe to closed/fixed (and line set to null) last night during a scan triggered by a PR merge. Specifically:
The information you are providing is insufficient to determine what is the issue. As mentioned earlier, if you post the scan command line, git commands and logs used in your builds, we can investigate further.
For the scan where they get recreated (target branch) would be most helpful, but both are preferable. Please make sure DEBUG (/d:sonar.verbose=true) is set in your begin step. I am also interested in the git commands that are run around these so that I can recreate your scenario if needed.
Conservation International was a pioneer in defining and promoting the concept of hotspots. In 1989, just one year after scientist Norman Myers wrote the paper that introduced the hotspots concept, Conservation International adopted the idea of protecting these incredible places as the guiding principle of our investments. For nearly two decades thereafter, hotspots were the blueprint for our work.
Today, our mission has expanded beyond the protection of hotspots. We recognize that it is not enough to protect species and places; for humanity to survive and thrive, the protection of nature must be a fundamental part of every human society.
Hotspot Kits are checked out for 30 days and will renew up to three times after the original due date if there are no other customers waiting. Please monitor due dates to avoid being charged the full replacement cost of the Hotspot Kit.
Please take care of your Hotspot Kit. Fees will apply if the Wi-Fi hotspot or any accessory is lost or damaged. Library card privileges will be suspended until the Hotspot Kit is returned or charges on the account are paid.
You can check the availability of hotspots at your local branch by searching "mobile hotspot" in the library catalog or by calling any branch. If hotspots are not available, you may place a Hotspot Kit on hold. Only one hold is allowed per library account. Once you are notified that your Hotspot Kit is available, you will have seven business days to pick it up at your selected library location.
The vast majority of earthquakes and volcanic eruptions occur near plateboundaries, but there are some exceptions. For example, the Hawaiian Islands,which are entirely of volcanic origin, have formed in the middle of thePacific Ocean more than 3,200 km from the nearest plate boundary. How dothe Hawaiian Islands and other volcanoes that form in the interior of platesfit into the plate-tectonics picture?
Space Shuttle photograph of the Hawaiian Islands, the southernmostpart of the long volcanic trail of the "Hawaiian hotspot" (seetext). Kauai is in the lower right corner (edge) and the Big Island of Hawaiiin the upper left corner. Note the curvature of the Earth (top edge). (Photographcourtesy of NASA.)
In 1963, J. Tuzo Wilson, the Canadian geophysicist who discovered transformfaults, came up with an ingenious idea that became known as the "hotspot"theory. Wilson noted that in certain locations around the world, such asHawaii, volcanism has been active for very long periods of time. This couldonly happen, he reasoned, if relatively small, long-lasting, and exceptionallyhot regions -- called hotspots -- existed below the plates that wouldprovide localized sources of high heat energy (thermal plumes) tosustain volcanism. Specifically, Wilson hypothesized that the distinctivelinear shape of the Hawaiian Island-Emperor Seamounts chain resulted fromthe Pacific Plate moving over a deep, stationary hotspot in the mantle,located beneath the present-day position of the Island of Hawaii. Heat fromthis hotspot produced a persistent source of magma by partly melting theoverriding Pacific Plate. The magma, which is lighter than the surroundingsolid rock, then rises through the mantle and crust to erupt onto the seafloor,forming an active seamount. Over time, countless eruptions cause the seamountto grow until it finally emerges above sea level to form an island volcano.Wilson suggested that continuing plate movement eventually carries the islandbeyond the hotspot, cutting it off from the magma source, and volcanismceases. As one island volcano becomes extinct, another develops over thehotspot, and the cycle is repeated. This process of volcano growth and death,over many millions of years, has left a long trail of volcanic islands andseamounts across the Pacific Ocean floor.
According to Wilson's hotspot theory, the volcanoes of the Hawaiian chainshould get progressively older and become more eroded the farther they travelbeyond the hotspot. The oldest volcanic rocks on Kauai, the northwesternmostinhabited Hawaiian island, are about 5.5 million years old and are deeplyeroded. By comparison, on the "Big Island" of Hawaii -- southeasternmostin the chain and presumably still positioned over the hotspot -- the oldestexposed rocks are less than 0.7 million years old and new volcanic rockis continually being formed.
Above: Artist's conception of the movement of the PacificPlate over the fixed Hawaiian "Hot Spot," illustrating the formationof the Hawaiian Ridge-Emperor Seamount Chain. (Modified from a drawing providedby Maurice Krafft, Centre de Volcanologie, France). Below: J. TuzoWilson's original diagram (slightly modified), published in 1963, to showhis proposed origin of the Hawaiian Islands. (Reproduced with permissionof the Canadian Journal of Physics.)
The possibility that the Hawaiian Islands become younger to the southeastwas suspected by the ancient Hawaiians, long before any scientific studieswere done. During their voyages, sea-faring Hawaiians noticed the differencesin erosion, soil formation, and vegetation and recognized that the islandsto the northwest (Niihau and Kauai) were older than those to the southeast(Maui and Hawaii). This idea was handed down from generation to generationin the legends of Pele, the fiery Goddess of Volcanoes. Pele originallylived on Kauai. When her older sister Namakaokahai, the Goddess of the Sea,attacked her, Pele fled to the Island of Oahu. When she was forced by Namakaokahaito flee again, Pele moved southeast to Maui and finally to Hawaii, whereshe now lives in the Halemaumau Crater at the summit of Kilauea Volcano.The mythical flight of Pele from Kauai to Hawaii, which alludes to the eternalstruggle between the growth of volcanic islands from eruptions and theirlater erosion by ocean waves, is consistent with geologic evidence obtainedcenturies later that clearly shows the islands becoming younger from northwestto southeast.
Although Hawaii is perhaps the best known hotspot, others are thought toexist beneath the oceans and continents. More than a hundred hotspots beneaththe Earth's crust have been active during the past 10 million years. Mostof these are located under plate interiors (for example, the African Plate),but some occur near diverging plate boundaries. Some are concentrated nearthe mid-oceanic ridge system, such as beneath Iceland, the Azores, and theGalapagos Islands.
A few hotspots are thought to exist below the North American Plate. Perhapsthe best known is the hotspot presumed to exist under the continental crustin the region of Yellowstone National Park in northwestern Wyoming. Hereare several calderas (large craters formed by the ground collapseaccompanying explosive volcanism) that were produced by three gigantic eruptionsduring the past two million years, the most recent of which occurred about600,000 years ago. Ash deposits from these powerful eruptions have beenmapped as far away as Iowa, Missouri, Texas, and even northern Mexico. Thethermal energy of the presumed Yellowstone hotspot fuels more than 10,000hot pools and springs, geysers (like Old Faithful), and bubbling mudpots(pools of boiling mud). A large body of magma, capped by a hydrothermalsystem (a zone of pressurized steam and hot water), still exists beneaththe caldera. Recent surveys demonstrate that parts of the Yellowstone regionrise and fall by as much as 1 cm each year, indicating the area is stillgeologically restless. However, these measurable ground movements, whichmost likely reflect hydrothermal pressure changes, do not necessarily signalrenewed volcanic activity in the area. 152ee80cbc
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