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HiClip mini 4K: Along the Path of Mr. K

This image covers a small section of Hebes Chasma. (This is a non-narrated clip with ambient sound.)

youtu.be/6mmmc5_aK-Q

HiRISE 3D: Diverse Bedrock Exposures

This anaglyph shows a well-exposed massif with diverse bedrock exposures north of Hellas region.

Full image: uahirise.org/anaglyph/ESP_0819
NASA/JPL-Caltech/UArizona

HiPOD: Delta or Fan?

Delta or fan deposits indicate past water activity. HiRISE can resolve sedimentary characteristics such as layering, stratigraphic relationship to the surrounding geologic setting or distributary channels that cannot be resolved by other camera experiments.

ID: ESP_074848_2040
date: 15 July 2022
altitude: 284 km

uahirise.org/hipod/ESP_074848_
NASA/JPL-Caltech/UArizona

HiRISE 3D: Hillslope Shapes near Holden Crater

What was the source of the runoff that helped shape these hills and their slopes?

Full image: uahirise.org/anaglyph/ESP_0820
NASA/JPL-Caltech/UArizona

HiPOD: Gully Study

The gullies and their small fans in this impact crater are suggestive of recurring slope lineae. Are there fresh deposits here? The crater is less than 5 kilometers in diameter and the scene is located in Terra Cimmeria, to east of the massive Hellas impact basin.

ID: ESP_074833_1460
date: 14 July 2022
altitude: 254 km

uahirise.org/hipod/ESP_074833_
NASA/JPL-Caltech/UArizona

HiRISE 10K: A Simple Crater

Sometimes, the nicest pictures we acquire don’t need a long explanation, so we are parking this image of the northern part of large, less than 5-km diameter crater for your visual enjoyment.

Full cutout on Flickr: flic.kr/p/2pAWk46

HiPOD: Layered Features in Northern Mid-Latitudes

The objective of this observation is to examine several sets of layered features. Some are dipping and others are horizontal. Some are in craters, and another within a depression. The scene can be found in Context Camera image data.

uahirise.org/hipod/ESP_074824_
NASA/JPL-Caltech/UArizona

HiRISE 8K: In Tyrrhena Terra

Tyrrhena Terra is located in the cratered highlands of the Southern Hemisphere of Mars. It is one of the regions where instruments like OMEGA and CRISM (the latter also on the Mars Reconnaissance Orbiter) have identified numerous detections of hydrated silicates.

Full cutout on Flickr: flic.kr/p/2pAMjrM
NASA/JPL-Caltech/UArizona

HiRISE 3D: An Eye on You

From the rationale: “This feature has been suggested to have formed after Athabasca Valles was first carved and thus is evidence for multiple floods. The idea is hooey, but CTX is not sufficient to prove that.”

uahirise.org/anaglyph/ESP_0401
NASA/JPL-Caltech/UArizona

HiPOD: Fossae East of Arsia Mons

Our science goal with this observation is to examine a vent-like structure in the floor of a graben that is part of a larger fossae system partially buried by numerous flows. We want to determine the relationship of the possible vent to the graben and adjacent flow units, and look for any deposits related to the vent.

ID: ESP_074829_1720
date: 14 July 2022
altitude: 254 km

uahirise.org/hipod/ESP_074829_
NASA/JPL-Caltech/UArizona

HiIRSE 4K Possible Olivine on the Floor of a Crater in Northern Hellas Planitia

Olivine is a common silicate mineral that comes from magma generated in the mantle of Mars (this same process occurs on Earth as well).

Full cutout on Flickr:
flic.kr/p/2pACDRG

NASA/JPL-Caltech/UArizona

HiRISE 3D: The Skin of Smaug

Well, really just a stunning exposure of the South Polar layered deposits on Mars.

uahirise.org/anaglyph/ESP_0401
NASA/JPL-Caltech/UArizona

HiPOD: Fed by Fans But from Where?

With this observation, we see some candidate lake deposits possibly fed by alluvial fans in the distant past. At high resolution, we can check for layers and layer tilts to test a lacustrine hypothesis. Tilts more than 2 degrees suggest the origin is *not* lacustrine, but rather from a distal alluvial source.

uahirise.org/hipod/ESP_074827_
NASA/JPL-Caltech/UArizona

HiRISE 3D: Light-Toned Stratified Materials in Hebes Chasma

Hebes Chasma is an isolated chasma just north of the Valles Marineris canyon system of Mars. This image is northwest of the central mound located there.

uahirise.org/anaglyph/ESP_0402
NASA/JPL-Caltech/UArizona

HiPOD: Near the Deepest Point

We acquired this image to study layered materials in a low albedo (light-reflective) region near deepest point of an unnamed impact crater north of the Becquerel Crater. There might be possible embedded craters here, which is interesting because the host crater is relatively young, and the layers could be lake sediments.

ID: ESP_074825_2065
date: 13 July 2022
altitude: 290 km

uahirise.org/hipod/ESP_074825_
NASA/JPL-Caltech/UArizona

HiRISE 3D: A Candidate Landing Site in Mclaughlin Crater

This was a leading candidate site for the Mars 2020 rover and other future missions. The floor of McLaughlin Crater contains layered carbonates and clay minerals suggesting of an ancient lacustrine setting.

uahirise.org/anaglyph/ESP_0402
NASA/JPL-Caltech/UArizona

HiPOD: Among Hale Crater’s Central Peaks

This image is part of a new slope monitoring sequence as we try to observe any activity after a dust storm to compare with a previous Mars year sequence. Are any recurring slope lineae longer or more dense? Hale is about 150 km in diameter and located north of the Argyre basin.

ID: ESP_074813_1440
date: 12 July 2022
altitude: 258 km

uahirise.org/hipod/ESP_074813_
NASA/JPL-Caltech/UArizona

HiRISE 3D: A Candidate Landing Site in Hadriacus Palus

Now *this* would prove to be a tricky landing area!

uahirise.org/anaglyph/ESP_0403
NASA/JPL-Caltech/UArizona

HiPOD: Steep and Stunning

Even after so many years in orbit, there are still plenty of places on Mars that need the HiRISE treatment. This image was requested because there is little coverage along this portion of Coprates’ south wall. With this observation, we can fill in the gaps and get unique coverage. We can also look for colorful slopes of mafic materials.

ID: ESP_074814_1655
date: 12 July 2022
altitude: 257 km

uahirise.org/hipod/ESP_074814_
NASA/JPL-Caltech/UArizona

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HiRISE (NASA)

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