In fact the only reason the flows stopped is because there wasn’t enough material sustain it.įor an eruption smaller than the Tambora this very impressive. The pyroclastic flows traveled 80 km from the volcano, over mountains and across valleys, while traveling at the speed of sound for a significant portion of the flows lifetime. In my opinion, this might be the only historical eruption that rivals the 1883 eruption of Krakatoa’s intensity.This eruption released over 30 km3 of tephra in just 5 minutes and produced the most impressive pyroclastic flows since the Akahoya eruption. The most violent of which, the Hatepe eruption, hasn’t gotten as much attention as it’s peers. The most violent eruptions of then past 2000 years have grabbed endless amounts of fascination among the geological community. We haven’t even come close to seeing the worst case scenario for eruptions, in fact we haven’t seen a truly bad case scenario for volcanoes! Think back to all of the most deadly eruptions of the past 100 years, all of those eruptions were 100s, 1,000s, 10,000s, or even 100,000s of times smaller than some of the larger eruptions in recent geological history. This is actually a fun point of contention (For me at least) and is part of a larger passive debate. I believe that title goes to volcanoes while my father believes it goes to earthquakes. The system automatically deletes the resource when its process terminates, however, calling the appropriate function saves memory and decreases the size of the process's working set.My father and I disagree on a lot of things from religion, politics, career, and more One of the things we disagree on is the title of worst geological disaster. When you are finished using the resource, you can release its associated memory by calling one of the functions in the following table. To get extended error information, call GetLastError. If the function fails, the return value is NULL. If the function succeeds, the return value is the handle to the newly created image. If the resource contains multiple images, the function uses the size of the first image. If this flag is not specified and cxDesired and cyDesired are set to zero, the function uses the actual resource size. Uses the width or height specified by the system metric values for cursors or icons, if the cxDesired or cyDesired values are set to zero. This flag is only valid if uType is IMAGE_BITMAP. Otherwise, the bitmap image is created as a device-dependent bitmap. If this is set and a new bitmap is created, the bitmap is created as a DIB section. If this flag is not specified, a new object is always created.
Returns the original hImage if it satisfies the criteria for the copy-that is, correct dimensions and color depth-in which case the LR_COPYDELETEORG flag is ignored. This will succeed only if hImage was loaded by LoadIcon or LoadCursor, or by LoadImage with the LR_SHARED flag. If this flag is set, CopyImage uses the size in the resource file closest to the desired size. Without this flag, CopyImage stretches the original image to the new size. This is useful for creating a different-sized copy when the resource file contains multiple sizes of the resource. Tries to reload an icon or cursor resource from the original resource file rather than simply copying the current image. Valueĭeletes the original image after creating the copy. This parameter can be one or more of the following values. If this is zero, then the returned image will have the same height as the original hImage. The desired height, in pixels, of the image. If this is zero, then the returned image will have the same width as the original hImage.
The desired width, in pixels, of the image. This parameter can be one of the following values. If necessary, the function stretches the bits to fit the desired size of the new image. Creates a new image (icon, cursor, or bitmap) and copies the attributes of the specified image to the new one.
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