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HiPOD: Spotted Dunes near Terra Cimmeria

Frost and sand are common occurrences on Mars. The bright carbon dioxide frost condenses out of the atmosphere during winter, marking a stark contrast with the dark sand dunes found here. This image reveals how the warming temperatures from the rising southern sun liberate the frost and expose the sand, initially in discrete spots. (Enhanced color image is less than 1 km across.)

uahirise.org/hipod/ESP_081492_
NASA/JPL-Caltech/UArizona

HiPOD: Lavas and Grabens

How far do the lavas from Arsia Mons invade the grabens here in Noctis Labyrinthus? Why is the contact so sharp? What marginal characteristics are present in the lava flows, particularly the details of the crenulations or lack thereof?

ID: ESP_075264_1630
date: 16 August 2022
altitude: 251 km

uahirise.org/hipod/ESP_075264_
NASA/JPL-Caltech/UArizona

HiRISE 3D: Like a Wound – This observation did not have much by way of its science rationale, but it’s weird-looking enough to warrant a 3D look.

uahirise.org/anaglyph/ESP_0828
NASA/JPL-Caltech/UArizona

HiPOD: Slope Monitoring in Layered Rocks

This deposit of sedimentary rocks has excellent examples of recurring slope lineae (RSL). This proposed region of interest was last imaged after the 2006 dust storm and shows numerous large RSL all over the steep slopes. Once this excellent candidate RSL site is confirmed, additional images can be acquired on the neighboring candidate RSL site to the east.

uahirise.org/hipod/ESP_075259_
NASA/JPL-Caltech/UArizona

HiPOD: A Layered Feature in a Crater in Nilosyrtis Mensae

The objective of this observation is to examine a layered feature in an impact crater. The layers may represent layers of mantle from when the climate changed and the shape may be due to the wind. The scene is also found in Context Camera data.

ID: ESP_075257_2155
date: 16 August 2022
altitude: 291 km

uahirise.org/hipod/ESP_075257_
NASA/JPL-Caltech/UArizona

HiPOD: Layers in a Crater

The objective of this observation is to examine light and dark layers in an impact crater in Cydonia Mensae. Our interest is in seeing if the layer boundaries are diffuse as suggested in CTX image data. Most of the layers seem to have definite boundaries.

ID: ESP_075247_2125
date: 15 August 2022
altitude: 292 km

uahirise.org/hipod/ESP_075247_
NASA/JPL-Caltech/UArizona

HiPOD: Textures of Amazonis

This observation was requested to look at some unusual surface textures in Amazonis Planitia. Some of the terrain grades into ridges that could possibly be invasive dikes or lava intruding into overlying ash. Despite the features in this image, Amazonis Planitia is one of the smoothest plains on Mars, and is located between the Tharsis and Elysium volcanic provinces, to the west of Olympus Mons.

uahirise.org/hipod/ESP_075239_
NASA/JPL-Caltech/UArizona

HiPOD: Slope and Gully Monitoring

Our science goal with this target is to monitor frost in active gullies in Moni Crater. Additionally, we want to observe lineae associated with sand dunes on the eastern rim of the crater and seen to be active in the Martian winter. Moni is an approximately 5-km diameter crater in the southern mid-latitude highlands of Noachis Terra, on the inner ring of the larger Kaiser Crater.

uahirise.org/hipod/ESP_075233_
NASA/JPL-Caltech/UArizona

HiRISE 3D: A Dark Spot, Revisited

Today’s HiPOD certainly warrants a look in 3D, as part of the rationale for the observation stated that stereo will be helpful for measuring the thickness of the banded terrain and layered material. (Give your eyes a few second to adjust with this one.)

uahirise.org/anaglyph/ESP_0822
NASA/JPL-Caltech/UArizona

HiPOD: A Great Dark Spot

This observation targets a pit partially filled with layered material and surrounded by banded terrain, as seen in Context Camera data . The relationship between the banded terrain and the layered material in the pit is unclear. HiRISE imaging may help to understand the contact between two. Stereo will be helpful for measuring the thickness of the banded terrain and layered material.

uahirise.org/hipod/ESP_082221_
NASA/JPL-Caltech/UArizona

HiPOD: Defrosting Dunes

This image shows a field a sand dunes in the Martian springtime while the seasonal carbon dioxide frost is sublimating into the air. This sublimation process is not at all uniform, instead creating a pattern of dark spots.

In addition, the inter-dune areas are also striking, with bright frost persisting in the troughs of polygons. Our enhanced-color cutout is centered on a brownish-colored inter-dune area.

uahirise.org/ESP_082672_1180
NASA/JPL-Caltech/UArizona

HiPOD: Gullies in the Depths of Hellas

Gullies are commonly found in the Martian mid-latitudes, particularly in the Southern Hemisphere. However, they are rare in the deepest parts of the massive Hellas impact basin.

For this image, HiRISE targeted a relatively fresh crater where previous images from the MRO Context Camera appeared to show gullies. This high-resolution look confirms their presence.

More: uahirise.org/ESP_082273_1360

NASA/JPL-Caltech/UArizona

HiPOD: Sediment Ponds in Tithonium Chasma

This survey of the canyon floor of Tithonium Chasma in Valles Marineris reveals terrain of two distinct ages. The slopes and hilltops here are made up of rough rocky outcrop that was sculpted by impact craters of all sizes. In contrast, the valley floors are filled with light toned, smooth materials with far fewer large craters.

uahirise.org/hipod/ESP_082582_
NASA/JPL-Caltech/UArizona

HiRISE 3D: Topographic Interactions in Athabasca Valles

The request for this image was to retarget for an observation centered on the interactions between lava, topography, and a fissure.

uahirise.org/anaglyph/ESP_0822
NASA/JPL-Caltech/UArizona

HiPOD: Hydrated Sulfates in Melas Chasma

This image was acquired to get more information about a site where the CRISM instrument detected hydrated sulfates. The bright materials are likely to be sediments rich in the hydrated sulfates, and this image shows that most of the material is covered by a thin deposit of dark material, perhaps sand.

More: uahirise.org/hipod/ESP_082700_

NASA/JPL-Caltech/UArizona

HiPOD: A Channel in Huygens

The objective of this observation is to examine small, eroded channels. In this spot are many branched channels that have dark material on their floors. This image is located on what is left of the eroded southwest crater rim of Huygens, which is 467 km (290 mi) in diameter. The scene is also available in Context Camera data.

uahirise.org/hipod/ESP_075192_
NASA/JPL-Caltech/UArizona

HiRISE 3D: Ridges West of Vernal Crater

These may be large mineralized fracture zones, so our image will help us to investigate further.

uahirise.org/anaglyph/ESP_0821
NASA/JPL-Caltech/UArizona

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HiRISE (NASA)

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