Mercury and Me: An Intimate Memoir by the Man Freddie Loved

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Schaefer, Bradley E. (2007). "The Latitude and Epoch for the Origin of the Astronomical Lore in MUL.APIN". American Astronomical Society Meeting 210, #42.05. 38: 157. Bibcode: 2007AAS...210.4205S. Christensen, Ulrich R. (2006). "A deep dynamo generating Mercury's magnetic field". Nature. 444 (7122): 1056–1058. Bibcode: 2006Natur.444.1056C. doi: 10.1038/nature05342. PMID 17183319. S2CID 4342216.

Their presence were everywhere,they strive to deliver high standards,and to ensure that all guests are having a wonderful time and to resolve any issues that may arise.Alyona,entertainment manager who is in charge of the aqua aerobics,sunset yoga on the beach,the nightly entertainment ,karoke etc is excellent at her job. Kaler, James B. (2016). From The Sun To The Stars. World Scientific Publishing Company. p.56. ISBN 9789813143265. Finley, Dave (May 3, 2007). "Mercury's Core Molten, Radar Study Shows". National Radio Astronomy Observatory . Retrieved May 12, 2008.

Wall, Mike (March 29, 2015). "NASA Mercury Probe Trying to Survive for Another Month". Space.com . Retrieved April 4, 2015. The planet's mantle is chemically heterogeneous, suggesting the planet went through a magma ocean phase early in its history. Crystallization of minerals and convective overturn resulted in a layered, chemically heterogeneous crust with large-scale variations in chemical composition observed on the surface. The crust is low in iron but high in sulfur, resulting from the stronger early chemically reducing conditions than is found on other terrestrial planets. The surface is dominated by iron-poor pyroxene and olivine, as represented by enstatite and forsterite, respectively, along with sodium-rich plagioclase and minerals of mixed magnesium, calcium, and iron-sulfide. The less reflective regions of the crust are high in carbon, most likely in the form of graphite. [54] [55]The observed perihelion precession of Mercury is 5,600 arcseconds (1.5556°) per century relative to Earth, or 574.10 ±0.65arcseconds per century [138] relative to the inertial ICRF. Newtonian mechanics, taking into account all the effects from the other planets and including 0.0254 arcsecond per century due to the oblateness of the Sun, predicts a precession of 5,557 arcseconds (1.5436°) per century relative to Earth, or 531.63 ±0.69arcseconds per century relative to ICRF. [138] In the early 20th century, Albert Einstein's general theory of relativity provided the explanation for the observed precession, by formalizing gravitation as being mediated by the curvature of spacetime. The effect is small: just 42.980 ±0.001arcseconds per century (or 0.43 arcsecond per year, or 0.1035 arcsecond per orbital period) for Mercury; it therefore requires a little over 12.5 million orbits, or 3 million years, for a full excess turn. Similar, but much smaller, effects exist for other Solar System bodies: 8.6247 arcseconds per century for Venus, 3.8387 for Earth, 1.351 for Mars, and 10.05 for 1566 Icarus. [139] [140] Observation Image mosaic by Mariner 10, 1974 Warren, Haygen (October 24, 2021). "BepiColombo completes first Mercury flyby, science provides insight into planet's unique environment". NASA Spaceflight . Retrieved October 8, 2022. Van Hoolst, Tim; Jacobs, Carla (2003). "Mercury's tides and interior structure". Journal of Geophysical Research. 108 (E11): 7. Bibcode: 2003JGRE..108.5121V. doi: 10.1029/2003JE002126. Mercury". US Geological Survey. May 8, 2003. Archived from the original on September 29, 2006 . Retrieved November 26, 2006. Zurbuchen TH, Raines JM, etal. (2008). "MESSENGER Observations of the Composition of Mercury's Ionized Exosphere and Plasma Environment". Science. 321 (5885): 90–92. Bibcode: 2008Sci...321...90Z. doi: 10.1126/science.1159314. PMID 18599777. S2CID 206513512.