File:Glacially-striated granite (Cadillac Mountain Granite, Silurian-Devonian boundary times, ~419 Ma; summit of South Bubble, Acadia National Park, Maine, USA) 4.jpg
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Summary[edit]
DescriptionGlacially-striated granite (Cadillac Mountain Granite, Silurian-Devonian boundary times, ~419 Ma; summit of South Bubble, Acadia National Park, Maine, USA) 4.jpg |
English: Glaciers are rivers of ice. Ice is a mineral (H2O) and glacial ice is a rock. Despite being solid, ice does flow under certain conditions at the Earth’s surface. Occasionally, Earth experiences Ice Ages, during which extensive ice sheets cover and move over significant portions of the Earth’s surface. As ice moves over landmasses, it erodes underlying rocks and picks up small to large pieces of debris. This debris accumulates at the base of the ice sheet and scrapes bedrock as the glacier moves, resulting in glacial scratches (glacial striations) (= thin scratch lines on rock) and glacial grooves (= large channels incised in rock).
The Late Pleistocene glacial striations seen here are developed on a granite surface atop a roche moutonnée in coastal Maine. The rock itself is part of the Cadillac Mountain Granite, a large pluton dating to about 419 million years ago. Locality: summit of South Bubble (a roche moutonnée), Acadia National Park, Mt. Desert Island, southern-coastal Maine, USA |
Date | |
Source | https://www.flickr.com/photos/47445767@N05/50603374713/ |
Author | James St. John |
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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/50603374713. It was reviewed on 18 November 2020 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0. |
18 November 2020
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Date/Time | Thumbnail | Dimensions | User | Comment | |
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current | 00:59, 18 November 2020 | 3,008 × 2,000 (5.53 MB) | Ser Amantio di Nicolao (talk | contribs) | Uploaded a work by James St. John from https://www.flickr.com/photos/47445767@N05/50603374713/ with UploadWizard |
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Metadata
This file contains additional information such as Exif metadata which may have been added by the digital camera, scanner, or software program used to create or digitize it. If the file has been modified from its original state, some details such as the timestamp may not fully reflect those of the original file. The timestamp is only as accurate as the clock in the camera, and it may be completely wrong.
Camera manufacturer | NIKON CORPORATION |
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Camera model | NIKON D70s |
Exposure time | 1/200 sec (0.005) |
F-number | f/7.1 |
ISO speed rating | 200 |
Date and time of data generation | 17:33, 11 September 2006 |
Lens focal length | 18 mm |
Width | 3,008 px |
Height | 2,000 px |
Bits per component |
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Pixel composition | RGB |
Orientation | Normal |
Number of components | 3 |
Horizontal resolution | 300 dpi |
Vertical resolution | 300 dpi |
Software used | Adobe Photoshop Elements 18.0 (Macintosh) |
File change date and time | 03:21, 15 November 2020 |
Y and C positioning | Co-sited |
Exposure Program | Not defined |
Exif version | 2.21 |
Date and time of digitizing | 17:33, 11 September 2006 |
Meaning of each component |
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Image compression mode | 4 |
APEX shutter speed | 7.643856 |
APEX aperture | 5.655638 |
APEX exposure bias | 0 |
Maximum land aperture | 3.6 APEX (f/3.48) |
Metering mode | Pattern |
Light source | Unknown |
Flash | Flash did not fire |
DateTime subseconds | 10 |
DateTimeOriginal subseconds | 10 |
DateTimeDigitized subseconds | 10 |
Supported Flashpix version | 1 |
Color space | sRGB |
Sensing method | One-chip color area sensor |
File source | Digital still camera |
Scene type | A directly photographed image |
Custom image processing | Normal process |
Exposure mode | Auto exposure |
White balance | Auto white balance |
Digital zoom ratio | 1 |
Focal length in 35 mm film | 27 mm |
Scene capture type | Standard |
Scene control | None |
Contrast | Normal |
Saturation | Normal |
Sharpness | Normal |
Subject distance range | Unknown |
Serial number of camera | 1004a0cc |
Lens used | 18.0-70.0 mm f/3.5-4.5 |
Date metadata was last modified | 22:21, 14 November 2020 |
Unique ID of original document | 6CAF7DB1DE85F29279428F3896A6040E |