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HiClip mini 4K: Ridges of Times Past

Also visible in Context Camera data, objective of this observation is to determine the nature of a field of ridges near Apollinaris Sulci. (This is a non-narrated clip with ambient sound.)

youtu.be/0lVUzihouv8

HiPOD: Dunes of an Unnamed Crater

This scene is located within an unnamed impact crater to the northwest of the larger Antoniadi Crater in the Northern Hemisphere of Mars. We obtained this image to observe possible changes in dune position, and for more coverage of star dunes, which are dunes with arms radiating from a central peak. Star dunes are more common on Mars than on Earth.

uahirise.org/hipod/ESP_074717_
NASA/JPL-Caltech/UArizona

HiRISE 3D: Nili Patera Dunes

We acquired this observation to provide further high resolution images of the Nili Patera dune field.

uahirise.org/anaglyph/ESP_0406
NASA/JPL-Caltech/UArizona

HiPOD: Dunes on the Floor of Huggins Crater

Dunes are particularly suited to comprehensive planetary studies because they are abundant over a wide range of elevations and terrain types. A global scale study of Martian dunes serves a dual purpose in furthering understanding of both climatic and sedimentary processes, two fundamental topics currently driving Martian science.

uahirise.org/hipod/ESP_074727_
NASA/JPL-Caltech/UArizona

HiPOD: The Hills in Ganges Chasma

Ganges Chasma is in the northeast portion of Valles Marineris, and opens into outflow channels that flowed to the north.

Scattered hills on the canyon floor may be remnants of chaos terrain that formed from collapse of the canyon. Some of the bedrock has diverse colors as we see in the enhanced-color cutout.

uahirise.org/hipod/ESP_054609_
NASA/JPL-Caltech/UArizona

HiRISE 3D: Light-Toned Layered Deposits Exposed along Coprates Chasma Floor

Context Camera data shows exposure of light-toned layered deposits at this location. Our resolution can take a closer look at the details in the layering.

Full image: uahirise.org/anaglyph/ESP_0329

NASA/JPL-Caltech/UArizona

Channels near Huygens Crater

The objective of this observation is to examine channels on the outside of an impact crater. They lead away from the rim, and perhaps they were formed by the heat of the impact melting ground ice. There are many additional channels located in this general area, and much ice may have been present in the ground. This scene is also covered in Context Camera data.

uahirise.org/hipod/ESP_074717_
NASA/JPL-Caltech/UArizona

HiRISE 3D: Dune Monitoring in a Northern Mid-Latitude Crater

This was part of a seasonal series to track changes over time. This image had less frost than previous observations.

uahirise.org/anaglyph/ESP_0805
NASA/JPL-Caltech/UArizona

Megaripple Stripes on Mars

Among the undulating topography of this dune field in Rabe Crater, one notable feature is the presence of distinct megaripple stripes. Intermediate in size relative to larger dunes and smaller ripples, these megaripples gather in parallel rows, their formation guided by wind patterns and the distribution of grain sizes.

ID: ESP_058009_1355
date: 11 December 2018
altitude: 250 km

uahirise.org/hipod/ESP_058009_
NASA/JPL-Caltech/UArizona

HiRISE 3D: Volcanoes and Collapses

This image of Hephaestus Fossae shows a volcanic area where collapses like this happen. Chains of large elliptical pits mark the path that underground molten rock took.

uahirise.org/anaglyph/ESP_0802
NASA/JPL-Caltech/UArizona

Hematite in Capri Chasma

The Thermal Emission Spectrometer on the Mars Global Surveyor detected hematite along the chasma floor and edges of these mesas in Capi Chasma. Hematite on Earth is typically formed in aqueous environments or by aqueous alteration, so its presence warranted investigation by the two Mars Exploration Rovers, Spirit and Opportunity, that found a significant amount of the mineral.

uahirise.org/hipod/ESP_022698_
NASA/JPL-Caltech/UArizona

HiRISE 3D: Light-Toned Exposures near Voeykov Crater

Our goal here is a comparison with CaSSIS DTM and stratigraphy. CaSSIS also identified peculiar color variation here.

uahirise.org/anaglyph/ESP_0803
NASA/JPL-Caltech/UArizona

The Floor of Mawrth Vallis

CRISM data shows a localized, unique spectral phase consistent with poly-hydrated sulfate or zeolite here on the Mawrth Vallis channel floor, with implications for the regional history. This target provides both color coverage and stereo over the outcrop. We can also look for textual differences between new hydrated mineral and adjacent clays.

date: 21 May 2011
altitude: 285 km

uahirise.org/hipod/ESP_022578_
NASA/JPL-Caltech/UArizona

Noachian Bedrock Diversity

In an adjacent image we acquired in 2008, there was terrific color and texture diversity, so this observation was acquired to extend coverage. There are clays mixed with unaltered mafics in this area as well. “Noachian” refers to the early geologic period after Mars formed, 3 to 4 billion years ago.

ID: ESP_022601_1975
date: 23 May 2011
altitude: 279 km

uahirise.org/hipod/ESP_022601_
NASA/JPL-Caltech/UArizona

HiRISE 3D: Terracing Inside and Outside a Degraded Crater Rim

This image shows multiple bands on the inside and outside of a crater rim that may be terraces. Are they paired topographically?

Full image: uahirise.org/anaglyph/ESP_0407

NASA/JPL-Caltech/UArizona

HiRISE 3D: A Buffet of Secondary Craters

This observation is part of a study that aims to characterize how secondary crater shape depends on distance from source craters and hence impact velocity.

Full image: uahirise.org/anaglyph/ESP_0409

NASA/JPL-Caltech/UArizona

HiRISE 3D: A Possible Fresh, Small Crater in Arcadia Planitia

With this anaglyph, we can look for rocks, textures and excavated stratigraphy.

Full image: uahirise.org/anaglyph/ESP_0413

NASA/JPL-Caltech/UArizona

HiPOD: Colorful Impact

Our enhanced image reveals colors ranging from red to green to blue. These are infra-red shifted colors (infrared-red-blue) so it’s different than what we would see with our eyes.

More: uahirise.org/hipod/ESP_055541_

NASA/JPL-Caltech/UArizona

HiPOD: Seasonal Flows in the Central Mountains of Hale Crater

The recurring slope lineae (RSL) in Hale have an unusually “reddish” color compared to most RSL, perhaps due to oxidized iron compounds, like rust. Since HiRISE color is shifted to infra-red wavelengths, they are actually especially bright the near-infrared just beyond the range of human vision.

More: uahirise.org/hipod/ESP_040170_

NASA/JPL-Caltech/UArizona

HiPOD: Layering in Spallanzani Crater

In this image, we can see quite a spectacular layering pattern inside an impact crater called Spallanzani. Seeing layering is always exciting to geologists because it implies that the region has experienced multiple climatic conditions or geologic processes through time.

More: uahirise.org/hipod/ESP_040258_

NASA/JPL-Caltech/UArizona

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HiRISE (NASA)

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