Nevada Lithium

Nevada Sunrise began acquisitions of Nevada lithium brine exploration properties in September 2015 in the Clayton Valley area and the Lida Valley, located in Esmeralda County, Nevada.

Schematic Cross-section of Aquifers in the Clayton Valley (Zampirro, 2004)

Neptune Lithium Project

The Neptune property is located approximately 37 miles (55 kilometres) southwest of Tonopah, Nevada, near Silver Peak, in an active area of lithium exploration and mining. Neptune consists of a block of 93 unpatented placer claims totaling approximately 1,860 acres (753 hectares).

In 2015, Nevada Sunrise acquired historical geophysical data indicating Neptune has the potential to host lithium-bearing brines in subterranean aquifers beneath the Clayton Valley floor.

Neptune Lithium Brine Project_NI 43-101 Technical Report_29 February 2016

Neptune 2016-2017 Drilling Program

In January 2016, Nevada Sunrise announced the receipt of a drill permit from the U.S. Bureau of Land Management (the “BLM”) for Neptune. The BLM approved 10 exploration drill hole locations, and Nevada Sunrise plans boreholes each up to 380 to 480 metres deep into the interpreted sub-basin, with follow-up drilling if warranted.

On April 6, 2017, Nevada Sunrise announced the commencement of a regional drilling program at Neptune. One borehole to a depth of approximately 610 metres (2,000 feet) was planned to follow up on encouraging results from the 2016 lithium brine drilling program carried out by Nevada Sunrise. Hole N-2017-1 was drilled to a depth of approximately 1,500 feet, about 75% of the interpreted target depth, but the hole was lost due to unstable ground conditions. As a result, no brines were encountered in the borehole.

Nevada Sunrise had previously completed two exploration holes at Neptune in late March 2016. Borehole N-2016-1, drilled to 457.2 metres (1,500 feet) showed anomalous lithium in a grab sample of groundwater of 6.8 mg/l lithium at a depth of 438.9 metres (1,440 feet).

Drill targets at Neptune have been generated from the integration of the results of: (1) a detailed gravity survey by a previous operator that outlined a deep, fault-bounded sub-basin, (2) a controlled source audio magnetotellurics follow-up survey that detected conductive horizons within the sub-basin, and (3) a 2016 time-domain electromagnetic survey that provided additional detail about the conductive horizons. In each of the two holes completed in 2016, permeable sedimentary, lacustrine strata interbedded with volcanic ash and other ejecta was logged at various levels throughout the holes. This type of sedimentary strata is interpreted as a requisite host horizon for lithium-bearing brines as seen in the northern Clayton Valley.

Neptune 2016 Initial
l PlanNeptune-Drilling-April-2017
The southern Clayton Valley area demonstrates enrichment in lithium in the nearby mountain ranges, desert sediments and in local plants. Nevada Sunrise has carried out ASTER spectral analysis of satellite imagery over Neptune and surrounding areas of the Clayton Valley. Results indicate lithium-bearing clay is derived from bedrock in areas to the north, west and southeast of Neptune. Biogeochemical data collected by the Company in October 2015 confirmed anomalous lithium concentrations ranging from 11 ppm up to 35 ppm in a specific desert plant common to the Clayton Valley and sampled near the planned Neptune drill holes.

Neptune Property Agreements

Nevada Sunrise owns a 100% interest in Neptune following the issuance to an underlying vendor of 1,000,000 common shares of the Company.

Neptune is subject to a 3.0% gross overriding royalty (“GOR”). On the 3rd anniversary of the effective date of the definitive agreement, Nevada Sunrise has the right to purchase 1.0% of the GOR for US$1,000,000.

Recommended Drill Hole P-3 Site at Neptune

Aquarius Lithium Project

Aquarius consists of 90 unpatented placer claims totaling 1,800 acres (729 hectares) located in the Clayton Valley, approximately 3 miles (5 kilometres) southwest of the Silver Peak Mine. Nevada Sunrise owns a 100% interest in the property with no applicable royalties.

Aquarius was staked in early 2016 following a review of the results of proprietary gravity surveys carried out by a geological team led by Dr. John Oldow of the University of Texas, Dallas, which outlined a strong gravity low indicative of a deep, faulted sub-basin. A follow-up time domain electromagnetic (“TDEM”) survey carried out by Nevada Sunrise in March 2016 detected conductive horizons at depths ranging between 250 and 450 metres.

Nevada Sunrise has received a permit from the BLM for a drill program to test for lithium brines at Aquarius.

About the Clayton Valley

The Clayton Valley playa is characterized as an immature clastic salar, or salt flat. Other than work carried out in the last 5 years by junior exploration companies, including Nevada Sunrise since 2016, historical exploration for lithium brines outside of production well drilling at Albemarle’s Silver Peak mine is sparse. A large scale ground gravity survey by the United States Geological Service (“USGS”) in 1980 outlined two gravity lows in the south end of the Clayton Valley – the “South Central Low” underlies land controlled by Pure Energy, and the “Southwest Low” underlies Neptune. (Source: from R. M. Allender, Jr., “Technical Report on the Neptune Lithium Brine Project, Clayton Valley, Esmeralda County, Nevada, USA”, 2016).

In 2013, the USGS released a paper describing the Clayton Valley’s potential to host lithium deposits based on the hypothesis that lithium is liberated by weathering of host rocks or derived from hydrothermal fluids from a variety of rock sources within a closed basin. The floor of Clayton Valley has an area of about 100 square kilometers and a catchment of about 1,400 square kilometres, and is the topographically lowest of at least five adjacent basins that are hydrologically linked by groundwater flow (Zampirro, 2004). It is the combined area of all five linked catchments that is significant, making the effective area of the Clayton Valley lithium-brine system much larger than the footprint of the Clayton Valley proper (Source: from USGS Open File 13-1006, 2013).

Clayton Valley Water Rights

On January 28, 2016, Nevada Sunrise announced an agreement for an option to purchase water rights in the Clayton Valley. The pre-existing, certificated water right allows for 1,770 acre/feet of water use for mining and milling per year (the “Permit”). Nevada Sunrise believes that the acquisition of water rights is an important step toward development of its Clayton Valley lithium properties should lithium brines be intersected in future drilling programs.

In December 2015, Nevada Sunrise received a written appraisal from an independent appraiser certified in the State of Nevada, which valued the Permit at US$1.42 million. According to the appraisal report, the Clayton Valley basin is currently “over-appropriated”, and stated that any new application for water use in an over-appropriated basin would be carefully reviewed by the Nevada Division of Water Resources (the “NDWR”), and that it is uncertain if any new applications for water rights would be granted.

On April 22, 2016, Nevada Sunrise, through its Nevada subsidiary Intor Resources Corporation, filed an application to transfer the Permit from its current location in the adjacent mountain range to a location due east on the desert floor within the boundaries of the Company’s Aquarius Project. The proposed Place of Use and Point of Diversion lies directly between a road and a powerline, located approximately 5 kilometres (3 miles) from the town of Silver Peak, Nevada and Albemarle’s Silver Peak lithium mine and 8 kilometers (5 miles) from its nearest lithium brine production well. Albemarle is one of the world’s largest producers of lithium chemical products.

On May 16, 2016, Nevada Sunrise announced that Albemarle had filed an official protest with the NDWR against the Company’s application to transfer the Place of Use and Point of Diversion of the Permit.

In June 2016, Albemarle filed a petition of forfeiture to the NDWR against the Permit, citing lack of beneficial use for a period of five years, and made the argument to the NDWR that the Company should not have a hearing with NDWR to assess the validity of the Permit. Albemarle is one of the world’s largest producers of lithium chemical products and currently operates the only producing lithium mine in the United States in the Clayton Valley at Silver Peak, Nevada. Due to its use of the evaporative pond method for lithium extraction from subterranean brines, Albemarle is the largest consumer of groundwater in the Clayton Valley. The Company’s existing Permit, senior to many of Albemarle’s own water permits, is the only remaining appropriation of groundwater in the Clayton Valley that is potentially available for a lithium brine extraction operation using a modern, efficient method that consumes low amounts of water.

On December 1, 2016, Nevada Sunrise learned that the State Engineer’s office of the NDWR had issued a ruling of forfeiture (the “Ruling”) against the Company’s water right in the Clayton Valley of Nevada. The Company has filed an appeal to the Ruling, and is currently engaged in litigation to restore the Permit.

The Company was surprised to receive the Ruling without the benefit of a hearing that it had requested with NDWR. Nevada Sunrise intends to vigorously defend the Permit, has filed evidence of water use that the NDWR requires, and awaits the outcome of its appeal.

Other Lithium Projects in Esmeralda County

Nevada Sunrise has adopted an exploration strategy targeting desert basins, or playas, that exhibit similar geological and geophysical characteristics to the Clayton Valley basin where lithium brines are known to accumulate in faulted sub-basins, or “traps”. Nevada Sunrise believes that interpreted gravity lows indicate the presence of deep, sub-basins that could host lithium-bearing brines.

Jackson Wash Lithium Project

Jackson Wash consists of 92 unpatented placer claims totaling approximately 1,840 acres (745 hectares) and is located in the Lida Valley on the east side of the Montezuma Range approximately 20 miles (30 kilometers) southeast of Silver Peak and 13 miles (21 kilometers) southwest of Goldfield. The Lida Valley is a flat, desert basin with a similar geological setting to the better-known Clayton Valley basin.

Prospecting at Jackson Wash in 2011 discovered widespread deposits of obsidian fragments on the valley floor, possibly derived from Tertiary felsic rhyolite and tuff volcanic rock units present in the Montezuma Range to the north and west of Jackson Wash. Fragments at six locations were sampled and returned lithium values ranging from 97.3 parts per million (“ppm”) lithium to 117.0 ppm lithium (R. M. Allender, Jr., 2016). Weathering of the felsic volcanic rocks containing lithium is believed to be a source of lithium contained in subterranean brines.

The results of a detailed gravity survey and two CSAMT lines surveyed in 2011 by a previous operator were interpreted as a layered sequence of unconsolidated, saturated alluvial sediments filling a deep basin beneath the valley floor. The Jackson Wash basin is believed to be related to north-south basin and range fault systems. Drilling and sampling of the sediments and groundwater in the interpreted basin are the next steps in the exploration process for Jackson Wash. Nevada Sunrise plans to test the Jackson Wash basin with a 3 to 4-hole drill program of boreholes up to 400 metres deep to test specific structural and stratigraphic targets believed prospective for lithium brine deposits.

Jackson Nash Gravity Survey

A drill permit for up to 10 holes over a 2-year period was granted by the BLM in February 2016. In June 2017, a borehole was drilled at Jackson Wash to a depth of 826 metres (2,710 feet) through interbedded sequences of sand, gravel, and clay. Hot fresh water was encountered in the borehole reaching a temperature of approximately 41 degrees C. (106 degrees F.) but no brines were detected.

Nevada Sunrise owns a 100% interest in Jackson Wash following the payment of 500,000 common shares of the Company to the underlying vendor since 2015.

A 1.5 mile (2.25 kilometer) area of interest applies to Jackson Wash and the property is subject to a 3.0% GOR. On the 3rdanniversary of the signing of the definitive agreement for Jackson Wash, Nevada Sunrise would have the right to purchase 1.0% of the GOR for US$1,000,000.

Atlantis Lithium Project

In February 2016, Nevada Sunrise announced the signing of a definitive agreement for an option to purchase a 100% interest in the Atlantis lithium property (“Atlantis”) located in the Fish Lake Valley in Esmeralda County, Nevada. Atlantis is comprised of unpatented placer claims and placer association claims totaling 2,900 acres (1,174 hectares) located approximately 25 miles (38 kilometres) northwest of the Silver Peak lithium brine mine.

For an option to purchase a 100% interest in Atlantis, Nevada Sunrise has agreed to pay a total of 500,000 common shares of the Company to the vendor upon signing the definitive agreement for Atlantis, and on subsequent anniversaries of the definitive agreement, as follows:

• On signing the definitive agreement: 100,000 common shares (paid)
• 1st Anniversary: 150,000 common shares (paid)
• 2nd Anniversary: 250,000 common shares (due in 2018)

A 1.5 mile (2.25 kilometer) area of interest applies to the Property. Atlantis is subject to a 3.0% GOR. On the 3rd anniversary of the signing of the definitive agreement for Atlantis, Nevada Sunrise would have the right to purchase 1.0% of the GOR for US$1.0 million.

On March 16, 2016, Nevada Sunrise announced an agreement with 1065604 BC Ltd., a private British Columbia company (“1065604”), for an option to earn an undivided 80% interest in Atlantis, by making cash and share payments to the Company and incurring exploration expenditures as follows:

• US$48,000 cash on the closing date of the transaction (paid);
• CDN$100,000 cash on or before the date which is the later of 30 days from the closing date and the date on which the 1065604 receives satisfactory evidence of the recording of claims newly-staked by Nevada Sunrise (paid);
• Incurring exploration expenditures of not less than US$1,000,000, consisting of US$100,000 on or before the 1st anniversary of the closing date, an additional US$250,000 on or before the 2 year anniversary of the closing date, and an additional US$650,000 on or before the 3rd anniversary of the closing. Any shortfalls in exploration expenditures in any year may be paid to Nevada Sunrise in cash to keep the option in good standing. Any excess amounts of exploration expenditures incurred in a year shall be applied to future years;
• Completion of a “going public” transaction resulting in a listing of 1065604 on a recognized Canadian stock exchange (the “Resulting Issuer”);
• Issuance of 1,250,000 common shares of the Resulting Issuer, with 250,000 common shares issuable on or before the date that is 60 days following the completion of a “going public” transaction, 500,000 common shares issuable on or before the 2nd anniversary of a the closing date for the transaction, and 500,000 common shares issuable on or before the 3rd anniversary of the closing date of the transaction. It is a condition of the option agreement that the common shares of the Resulting Issuer be subject to no more than a four month hold period in Canada from their date of issue.

On May 9, 2016, American Lithium Corp. (TSXV: LI) announced the acquisition of 1065604, and on May 17, 2016 announced completion of the acquisition, thereby meeting the obligation for 1065604 to achieve a “going public” transaction. American Lithium Corp. subsequently issued 250,000 of its common shares due to the Company according to the terms of the option agreement with 1065604 and assumes the obligation for the remaining share payments due to Nevada Sunrise. American Lithium Corp. will operate exploration at Atlantis.

Nevada Sunrise made the decision to acquire Atlantis after a review of geological mapping that shows the presence of lithium-bearing rocks in the ranges draining into Atlantis, anomalous to economic contents of lithium reported in surface and historical drill hole brines in the Fish Lake Valley within 3 miles of the Property, and historical ground gravity data that shows a distinct gravity low in the heart of the Atlantis claims. Dr. John Oldow’s detailed gravity survey work in Esmeralda County has better defined the historical gravity low at the Property as a deep, sub-basin, which led Nevada Sunrise to staking additional claims at Atlantis in January 2016.

As part of a regional lithium exploration program, the USGS reported in Open-File Report 81-962 (1981) that historical drill hole FL-11a is located outside the eastern boundary of Atlantis, approximately 3 miles (4.5 kilometres) east of the centre of the interpreted sub-basin. Hole FL-11a was drilled to a depth of 450 feet (147 metres) and encountered lithium values in sediments ranging from 10 ppm to 115 ppm and averaging 61.7 ppm for 67 samples analyzed. Lithium in sampled ground water ranged from trace at the end of the hole to 21 ppm at a depth of 55 feet (18 metres). Nevada Sunrise believes that drilling deeper holes at Atlantis within the area of the interpreted sub-basin could intersect aquifers potentially hosting trapped brines with higher contents of lithium than were encountered in the relatively shallow USGS hole drilled to the east of the gravity low anomaly. Also reported in USGS Open File Report 77-54 (1977) were the collection of 10 surface brine samples with lithium contents ranging 37 – 350 mg/l (ppm), and averaging 159 mg/l (ppm) to the north of the sub-basin.

Gemini Lithium Project

Gemini is located approximately 6 miles (10 kilometres) east of the town of Lida, Nevada, and consists of 134 placer claims totaling 2,680 acres (1,085 hectares). Gemini is adjacent to the Gold Point Solar Energy Zone, a BLM land reserve for solar power generation. Nevada Sunrise acquired Gemini by claimstaking in November and December 2015 with no applicable royalties.

On January 21, 2016, Nevada Sunrise announced that it had entered into a letter agreement to grant a 50% working interest in Gemini to Eureka Resources Inc. (“Eureka”, TSXV: EUK).

Nevada Sunrise made the decision to acquire claims covering the available land after reviewing the results of a recent gravity survey in conjunction with favourable local geology, namely late Miocene felsic volcanic tuffs adjacent to Gemini. These rocks provide the source of lithium for trapped, lithium-rich saline ground-waters (brine) within the sub-basins.

Previous ground gravity surveys in the Lida Valley area were widely-spaced and limited in scope, however in 2012 and 2013 a geological research team led by Dr. John Oldow of the University of Texas, Dallas collected approximately 500 gravity measurements along 7 transects crossing the Lida Valley. The detailed gravity survey results indicate strong gravity lows within two, faulted sub-basins approximately 7 kilometres (4.5 miles) apart, each interpreted to be hundreds of metres deep.

In February and March 2016, Nevada Sunrise received results from two TDEM surveys carried out at Gemini. The moving-loop TDEM surveys over Gemini West and Gemini East detected conductive zones within the sub-basins defined by Dr. Oldow’s gravity surveys. The results gained from the TDEM survey are interpreted to be conductive brines at depth located well below the non-conductive alluvium (sediments) at surface.

A conductive layer 150-250 metres deep appears to cover most of Gemini West and Gemini East, and several isolated strong conductive zones were interpreted at depths from 400 to 600 metres. The conductive layers and zones are indicative of brine solutions in porous aquifers and traps within each sub-basin.

Gemini Project Geophysical Interpretation July 2016.PDF

Drilling into the conductive zones within the sub-basins for lithium-bearing brines is recommended as the next step of exploration. There are no known drill holes at Gemini.

In June 2016, Nevada Sunrise submitted a permit application to the BLM for a 10-hole drill program to test for lithium brines at Gemini. A drilling permit, good for two years, was granted by the BLM in July 2016.

Gemini Transaction With Eureka

Eureka has the right to acquire a 50% interest in Gemini by reimbursing Nevada Sunrise for 50% of Gemini’s acquisition costs, and issuing Nevada Sunrise an aggregate of 500,000 common shares. The reimbursable acquisition costs include staking costs, data acquisition and processing, and claims registration fees payable to Esmeralda County and BLM. Eureka will issue to Nevada Sunrise 500,000 of its common shares as a prospect fee, with 300,000 shares to be issued on receipt of acceptance of the transaction by the TSXV and a further 200,000 shares to be issued on the first anniversary of such acceptance. Eureka and Nevada Sunrise will also enter into a joint venture with respect to Gemini, with Nevada Sunrise acting as operator of exploration in exchange for a 10% management fee to be charged to the joint venture.

In May 2016, Eureka and Nevada Sunrise entered into an addendum to the Agreement in which they agreed that Eureka had completed its due diligence review on Gemini and that Nevada Sunrise had confirmed receipt of approximately CAD$97,000 from Eureka representing 50% of the acquisition and evaluation costs on Gemini as provided for in the Agreement. All approvals of the independent directors of each company were obtained, and the letter agreement and its addendum were accepted by the TSXV. In June 2016, Eureka subsequently issued 300,000 common shares to Nevada Sunrise and became the owner of a 50% interest in Gemini. The companies subsequently entered into a definitive joint venture agreement.

John R. Kerr, P. Eng., and Robert M. Allender, Jr., CPG, RG, SME, are the Company’s designated Qualified Persons within the meaning of NI 43-101 and each have reviewed and approved the technical information contained herein.