Hottah (Mars)

Last updated
Hottah
PIA17062-MarsCuriosityRover-HottahRockOutcrop-20120915.jpg
"Hottah" rock outcrop on Mars - an ancient streambed [1] [2] [3] viewed by the Curiosity rover (September 12, 2012, white balanced) (close-up) (3-D version).
Feature type Rock outcrop
Coordinates 4°35′S137°26′E / 4.59°S 137.44°E / -4.59; 137.44

Hottah is a rock outcrop on the surface of Aeolis Palus, between Peace Vallis and Aeolis Mons ("Mount Sharp"), in Gale crater on the planet Mars. [1] [2] [3]

Contents

"Goulburn", "Link" and "Hottah" rock outcrop - suggest "vigorously" flowing water in an ancient streambed (September 27, 2012). PIA16157-MarsCuriosityRover-GoulburnLinkHottah-20120927.jpg
"Goulburn", "Link" and "Hottah" rock outcrop - suggest "vigorously" flowing water in an ancient streambed (September 27, 2012).

The outcrop was encountered by the Curiosity rover on the way from Bradbury Landing to Glenelg Intrigue on September 14, 2012 (the 39th sol of the mission), and was named after Hottah Lake, the sixth largest lake in the Northwest Territories, Canada. The "approximate" site coordinates are: 4°35′S137°26′E / 4.59°S 137.44°E / -4.59; 137.44 .

The outcrop is a well-sorted gravel conglomerate, containing well-rounded, smooth, abraded pebbles. Occasional pebbles up to a few centimeters across are embedded in amongst a matrix of finer rounded particles, up to a centimeter across. It has been interpreted as a fluvial sediment, deposited by a vigorously flowing stream, probably between ankle and waist deep. This stream is part of an ancient alluvial fan, which descends from the steep terrain at the rim of Gale crater across its floor. [2]

Remnant of ancient streambed on Mars (white-balanced) (September 14, 2012). (close-up) (3-D version). PIA16156-Mars Curiosity Rover-Water-AncientStreambed.jpg
Remnant of ancient streambed on Mars (white-balanced) (September 14, 2012). (close-up) (3-D version).

See also

Related Research Articles

<span class="mw-page-title-main">Gale (crater)</span> Martian crater

Gale is a crater, and probable dry lake, at 5.4°S 137.8°E in the northwestern part of the Aeolis quadrangle on Mars. It is 154 km (96 mi) in diameter and estimated to be about 3.5–3.8 billion years old. The crater was named after Walter Frederick Gale, an amateur astronomer from Sydney, Australia, who observed Mars in the late 19th century. Mount Sharp is a mountain in the center of Gale and rises 5.5 km (18,000 ft) high. Aeolis Palus is the plain between the northern wall of Gale and the northern foothills of Aeolis Mons. Peace Vallis, a nearby outflow channel, 'flows' down from the hills to the Aeolis Palus below and seems to have been carved by flowing water. Several lines of evidence suggest that a lake existed inside Gale shortly after the formation of the crater.

<span class="mw-page-title-main">Aeolis quadrangle</span> One of a series of 30 quadrangle maps of Mars

The Aeolis quadrangle is one of a series of 30 quadrangle maps of Mars used by the United States Geological Survey (USGS) Astrogeology Research Program. The Aeolis quadrangle is also referred to as MC-23 . The Aeolis quadrangle covers 180° to 225° W and 0° to 30° south on Mars, and contains parts of the regions Elysium Planitia and Terra Cimmeria. A small part of the Medusae Fossae Formation lies in this quadrangle.

<span class="mw-page-title-main">Hottah Lake</span>

Hottah Lake is the sixth largest lake in the Northwest Territories, Canada.

<span class="mw-page-title-main">Composition of Mars</span> Branch of the geology of Mars

The composition of Mars covers the branch of the geology of Mars that describes the make-up of the planet Mars.

<span class="mw-page-title-main">Mount Sharp</span> Martian mountain

Mount Sharp, officially Aeolis Mons, is a mountain on Mars. It forms the central peak within Gale crater and is located around 5.08°S 137.85°E, rising 5.5 km (18,000 ft) high from the valley floor. Its ID in the United States Geological Survey's Gazetteer of Planetary Nomenclature is 15000.

<span class="mw-page-title-main">Aeolis Palus</span> Palus on Mars

Aeolis Palus is a plain between the northern wall of Gale crater and the northern foothills of Aeolis Mons on Mars. It is located at 4.47°S 137.42°E.

<span class="mw-page-title-main">Timeline of Mars Science Laboratory</span> Event timeline of the NASA Mars Science Laboratory mission

The Mars Science Laboratory and its rover, Curiosity, were launched from Earth on 26 November 2011. As of August 17, 2024, Curiosity has been on the planet Mars for 4277 sols since landing on 6 August 2012. (See Current status.)

<span class="mw-page-title-main">N165</span> Rock on Mars

N165 is a rock on the surface of Aeolis Palus in Gale Crater on the planet Mars near the landing site of the Curiosity rover. The "approximate" site coordinates are: 4.59°S 137.44°E. On August 19, 2012, the rock was the first target of the rover's laser instrument, ChemCam, which can analyze targets at a distance using a laser and spectrometer. A Twitter feed for the rock was created, featuring an anthropomorphized account of its experiences. Its posts include a humor themed mix of social interaction and Mars content such as "Did you know I was born in a volcano? Basalts like me come from lava. That's why we call it Olympus Mom".

<span class="mw-page-title-main">Glenelg, Mars</span> Location on Mars

Glenelg, Mars is a location on Mars near the Mars Science Laboratory landing site in Gale Crater marked by a natural intersection of three kinds of terrain.

<span class="mw-page-title-main">Bradbury Landing</span> Landing site of Curiosity rover

Bradbury Landing is the August 6, 2012, landing site within Gale crater on planet Mars of the Mars Science Laboratory (MSL) Curiosity rover. On August 22, 2012, on what would have been his 92nd birthday, NASA named the site for author Ray Bradbury, who had died on June 5, 2012. The coordinates of the landing site on Mars are: 4.5895°S 137.4417°E.

<span class="mw-page-title-main">Jake Matijevic (rock)</span> Rock on Mars

Jake Matijevic is a pyramidal rock on the surface of Aeolis Palus, between Peace Vallis and Aeolis Mons, in Gale crater on the planet Mars. The approximate site coordinates are: 4.59°S 137.44°E.

<span class="mw-page-title-main">Peace Vallis</span> Martian valley

Peace Vallis is an ancient stream valley on the northern rim of Gale Crater on the planet Mars. It is notable for its associated alluvial fan which lies near the Mars Science Laboratory Curiosity landing site. The valley and alluvial fan provide evidence for geologically recent (Amazonian-aged) fluvial activity and sustained water flow on Mars. Recent high-resolution orbital images of Peace Vallis and its watershed also suggest that at least one glacial episode affected Gale crater. All of this evidence has implications for the history of water on Mars and the planet's long-term habitability. Understanding Peace Vallis and its fan also provides geologic context for the rocks observed on the ground by the Curiosity rover.

<span class="mw-page-title-main">Bathurst Inlet (rock)</span> Rock on the surface of Aeolis Palus on Mars

Bathurst Inlet is a rock on the surface of Aeolis Palus, between Peace Vallis and Aeolis Mons, in Gale crater on the planet Mars. The rock was encountered by the Curiosity rover on the way from Bradbury Landing to Glenelg Intrigue on September 30, 2012 and was named after Bathurst Inlet, a deep inlet located along the northern coast of the Canadian mainland. The "approximate" site coordinates are: 4.59°S 137.44°E.

<span class="mw-page-title-main">Rocknest (Mars)</span> Sandpatch

Rocknest is a sand patch on the surface of Aeolis Palus, between Peace Vallis and Aeolis Mons, in Gale crater on the planet Mars. The patch was encountered by the Curiosity rover on the way from Bradbury Landing to Glenelg Intrigue on September 28, 2012. The approximate site coordinates are: 4.59°S 137.44°E.

<span class="mw-page-title-main">Link (Mars)</span> Rock outcrop on Mars

Link is a rock outcrop on the surface of Aeolis Palus, between Peace Vallis and Aeolis Mons, in Gale crater on the planet Mars. The outcrop was encountered by the Curiosity rover on the way from Bradbury Landing to Glenelg Intrigue on September 2, 2012, and was named after a significant rock formation in the Northwest Territories of Canada. The "approximate" site coordinates are: 4.59°S 137.44°E.

<span class="mw-page-title-main">Goulburn (Mars)</span> Outcrop on Mars

Goulburn, also known as Goulburn Scour, is a rock outcrop on the surface of Aeolis Palus, between Peace Vallis and Aeolis Mons, in Gale crater on the planet Mars. The outcrop was encountered by the Curiosity rover on landing at the Bradbury Landing on August 6, 2012 and is named after a two-billion year-old sequence of rocks in Northern Canada. The "approximate" site coordinates are: 4.59°S 137.44°E.

<span class="mw-page-title-main">Rocknest 3</span> Martian rock

Rocknest 3 is a rock on the surface of Aeolis Palus, between Peace Vallis and Aeolis Mons, in Gale crater on the planet Mars. The approximate site coordinates are: 4.59°S 137.44°E.

<span class="mw-page-title-main">Tintina (rock)</span> Rock on the surface of Mars

Tintina is a rock on the surface of Aeolis Palus, between Peace Vallis and Aeolis Mons, in Gale crater on the planet Mars. The approximate site coordinates are: 4.59°S 137.44°E.

<span class="mw-page-title-main">Yellowknife Bay, Mars</span>

Yellowknife Bay is a geologic formation in Gale Crater on the planet Mars. NASA's Mars Science Laboratory rover, named Curiosity, arrived at the low lying depression on December 17, 2012, 125 sols, or Martian days, into its 668-sol planned mission on the planet. Primary mission goals of the Mars Science Laboratory were to assess the potential habitability of the planet and whether or not the Martian environment is, or has ever been, capable of supporting life.

<span class="mw-page-title-main">Mud cracks on Mars</span>

In January 2017, scientists announced the possible discovery of mud cracks in Gale Crater on Mars. The Curiosity Rover imaged what may be the first mud cracks ever found on Mars. They may have been formed from drying mud. The site, called “Old Soaker,” was within an exposure of Murray formation mudstone on lower Mount Sharp.

References

  1. 1 2 Brown, Dwayne; Cole, Steve; Webster, Guy; Agle, D.C. (September 27, 2012). "NASA Rover Finds Old Streambed On Martian Surface". NASA. Archived from the original on May 13, 2020. Retrieved September 28, 2012.
  2. 1 2 3 NASA's Curiosity Rover Finds Old Streambed on Mars. NASA. September 27, 2012. Retrieved September 28, 2012 via YouTube.
  3. 1 2 Chang, Alicia (September 27, 2012). "Mars rover Curiosity finds signs of ancient stream". AP News . Retrieved September 27, 2012.